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CHAPTERS IN THE PREHISTORY
OF EASTERN ARIZONA, I

PAUL S. MARTIN
JOHN B. RINALDO
WILLIAM A. LONGACRE
CONSTANCE CRONIN
LESLIE G, FREEMAN, JR.
JAMES SCHOENWETTER

FIELDIANA: ANTHROPOLOGY
VOLUME 53

Published by
CHICAGO NATURAL HISTORY MUSEUM

SEPTEMBER 19, 1962

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FIELDIANA: ANTHROPOLOGY

A Continuation of the
ANTHROPOLOGICAL SERIES
of

FIELD MUSEUM OF NATURAL HISTORY

VOLUME 53

IB Te EDUCATION

CHICAGO NATURAL HISTORY MUSEUM
CHICAGO, U.S.A.
1962

Digitized by the Internet Archive
in 2011 with funding from
Biodiversity Heritage Library

http://www. archive.org/details/fieldiana531962fiel

CHAPTERS IN THE PREHISTORY
OF EASTERN ARIZONA, I

COLORADO

@ACKMEN

CORTEZ
J

CHIN LEE@ \

we
ARIZONA

@ GALLUP

eFLAGBTAFF

NEW
MEXICO

WINSLOW®

TABLE ROCK PUEBLO

s
CONCHO
CHILCOTT SITES— =f coesins SITE

1957 gi ae @ QUEMADO
SHOW Low's ea TUMBLEWEED CANYON

MINERAL CREEK SITE ee a HOOPER RANCH PUEBLO
THODE SITE |

@CASA GRANDE

@SILVER CiTy

MEXICO

MAP SHOWING EASTERN ARIZONA AND WESTERN NEW MEXICO

CHAPTERS IN THE PREHISTORY
OF EASTERN ARIZONA, I

PAUL S. MARTIN
JOHN B. RINALDO
WILLIAM A. LONGACRE
CONSTANCE CRONIN
LESLIE G. FREEMAN, JR.
JAMES SCHOENWETTER

FIELDIANA: ANTHROPOLOGY
VOLUME 53
Published by
CHICAGO NATURAL HISTORY MUSEUM
SEPTEMBER 19, 1962

Edited by Lrtu1an A. Ross

Library of Congress Catalog Card Number: 62-21153

PRINTED IN THE UNITED STATES OF AMERICA
BY CHICAGO NATURAL HISTORY MUSEUM PRESS

Preface
Field Season of 1960

The field research of the 1960 season was remarkably interesting.
Several projects were undertaken, the results of which are described in
this report.

The National Science Foundation extended financial aid (Grant
No. G-13039) to the expedition and this permitted us to carry on an
archaeological] reconnaissance; to embark on a palaeo-ecological inquiry
by means of pollen analysis; and to dig a pre-ceramic site (Tumbleweed
Canyon Site) of pithouses. These ventures could not have been under-
taken without this aid.

In addition, with Museum funds, five other sites were excavated,
making, with the pre-pottery village, a total of six. These are (in alpha-
betical order):

1. Chilcott Sites (3), near Mesa Redondo and about seven miles
southwest of Concho, Arizona (Sec. 5, Twp. 11 N., R. 25 E., G. and
S.R.M.).

2. Goesling Site, located about two miles east of St. Johns, Arizona,
and overlooking the valley of the Little Colorado River (NE 4, Sec. 2,
Twp. 12 N., R. 28 E., G. and S.R.M.).

3. The Great Kiva, Hooper Ranch Pueblo (see Martin, Rinaldo
and Longacre, 1961), near Springerville, Arizona, on the banks of the
present channel of the Little Colorado River (NE 14, SW 4, Sec. 8,
Twp. 9 N., R. 29 E., G. and S.R.M.).

4. Rim Valley Pueblo, on the Hooper Ranch, situated high up
on the edge of a mesa overlooking the valley of the Little Colorado
River and the Hooper Ranch Pueblo (SE 144, NE 4, Sec. 18, Twp.
9N., R. 29 E., G. and S.R.M.).

5. Thode Site, on the west bank of the east fork of Mineral Creek,
near Highway 60 (SW \%4, NE \, Sec. 13, Twp. 10 N., R. 25 E., G.
and S.R.M.).

6. Tumbleweed Canyon Site, on the west bank of the Little Colorado
River, about halfway between St. Johns and Springerville, Arizona,
far from a highway; high up on an “island”? mesa of lava, overlooking

4 PREFACE

Lyman Dam Reservoir (NE 14, SE 4, Sec. 17, Twp. 11 N., R. 28 E.,
G. and S.R.M.). Financial aid supplied by funds from the National
Science Foundation.

The sites are on ranches owned by:

1. Mr. D. Chilcott, managed by Mr. Frank Stradling, Concho,
Arizona.

2. Mr. Al. H. Goesling, St. Johns, Arizona.

3 and 4. Mr. Rob Hooper, Springerville, Arizona.

5. Mr. Earl Thode, Vernon, Arizona.

6. Mr. Pacer Wiltbank, Eagar, Arizona.

I have listed these public-spirited gentlemen separately so that their
names will stand forth prominently and everyone will recognize their
contribution to archaeological research. I hope more will follow their
example. It is a pleasure to record here the thanks of the Museum
and of the members of the expedition and to state that our goals have
been greatly advanced by their unselfish help. We were permitted to
dig without hindrance and to bring back to the Museum, for research and
exhibition purposes, all of the specimens recovered. Many thousands
of people will benefit directly and indirectly from this arrangement
and will derive educational and cultural stimulation as well as satis-
faction of a common curiosity about man’s past.

In addition, I want especially to thank the members of the expedition
for the aid that they rendered in digging, in processing and cataloging
artifacts, in mending and restoring pottery, in housekeeping and in
maintaining an enviable record of spontaneity, of good will and co-
operation, of cheerfulness, of harmony, and of zest for all phases of the
work, whether glamorous or dull: Mr. William Alschuler, Miss Ellen
Chase, Mr. David Herod, Mr. Gardner Lane, Mr. William A. Longacre,
Mrs. Martha Perry, Mr. Pat Romane, Mrs. John B. Rinaldo, Mr. John
Saul, Mr. Roland Strassburger, and Mr. John Wells. Assisting also were
several neighbors and helpers of other seasons: Mr. Wilfred Barreras,
Mr. Joe Goodman, Mr. Genaro Nuarez, Mr. Gilbert Padilla and Mr.
Kenneth Penrod.

The palynological project was a new venture for us and was financed
entirely by the grant from the National Science Foundation. Mr. James
Schoenwetter was in charge of this project and has written an excellent
- report that appears in this volume. I find it suggestive and informative.
Without the advice of and the frequent consultations with Terah L.
Smiley and Paul S. Martin of the Geochronology Laboratories of the
University of Arizona, Schoenwetter’s objectives could not have been
attained.

PREFACE 5

The archaeological reconnaissance, made possible by a grant from
the National Science Foundation, was undertaken by Mr. Longacre.
It was successfully accomplished because of Mr. Longacre’s skill in estab-
lishing cordial rapport with neighboring ranchers, some of whom were
hostile due to past actions of prospectors. In the preliminary work,
Mr. Longacre was given admirable assistance by Mr. Leigh Richey of
St. Johns, Arizona.

I also take pleasure in thanking for their assistance: Mrs. Elizabeth
Brawley, St. Johns; Mr. and Mrs. Wayne Brinkerhoff, Snowflake; Mr.
and Mrs. J. R. Carter, Snowflake; Mr. Vernon Frazier, Snowflake;
Mr. and Mrs. Jake Kittle, Show Low; Mr. and Mrs. John D. Leverton,
Concho; Mrs. Leola Mineer, St. Johns; Mr. Verl Rhoton, Lakeside;
Mrs. Merle Thomas, Concho; Mr. and Mrs. Harvey Wilhelm, Snowflake;
Mr. and Mrs. Ira Willis and Mr. Kelley Willis, Snowflake; Mr. Ozie
Wilson, Pinetop; and Mr. and Mrs. Richard Wilson, Pinetop.

Our work is slowly becoming known in the Vernon area and more
and more people are beginning to respect archaeology as opposed to
pot-hunting. Last summer we held an open house one Sunday afternoon
to show our friends how we wash and classify pottery; how we restore
smashed and incomplete pottery (and demonstrate that we recover
mostly sherds and broken pots—rarely a whole one); what we recover
in the way of artifacts and how we catalogue them; how we record
architectural details; and what we ‘“‘do”’ with these data. More than a
hundred people came, in spite of one of the heaviest rainfalls of the
summer.

Analyzing and preparing our data for publication are large tasks
that have to be wedged into a crowded Museum schedule. Realizing
that I alone could not do full justice to the analysis of the pottery that
we recovered, I enlisted the help of Mr. Walter Boyer, sometime artist
in the Department of Anthropology, and of two advanced student-
assistants from the Department of Anthropology of the University of
Chicago, Miss Constance Cronin and Mr. Leslie Freeman.

The possible origin of a pottery type called Snowflake Black-on-
White—as yet really not too well known and not described—has been
examined by Miss Cronin and Mr. Boyer. The examination pursued two
trails: one admittedly subjective; and the other (hopefully) ‘‘objective.”
I placed approximately 2500 black-on-white painted (decorated) sherds
from five sites at the disposal of Miss Cronin. These sherds represented
several pottery types ranging in time from about a.p. 750 to about 1200.
Miss Cronin (assisted in the preliminary stages of the study by Mr.
Boyer) grouped the sherds into lots bearing identical or similar elements

6 PREFACE

of designs, but without regard to type, site, or chronology; for example,
all sherds bearing squiggly hatch, or ticked lines or pendent triangles
were put into separate piles and then counted. Then she re-sorted the
same sherds by site, by type, and by chronology and then separated these
groups into lots bearing similar or identical elements of design. These
were counted, percentages derived, and graphs drawn. Thus the study
was “‘quantified.”” Miss Cronin’s report is included in this volume.

The following civic-minded and generous persons have thought well
enough of our work to contribute financially to the expedition: Mr. C. E.
Gurley, Gallup, New Mexico; Mr. and Mrs. Maxwell Hahn, Scars-
dale, New York; Dr. Charles W. Keney, Gallup, New Mexico; and
Mr. Judd Sackheim, Chicago. The gifts of these thoughtful people
reach far beyond the materialistic side of things; they reach into our
hearts and cheer us. I hope the results of the expedition, embodied in
this report, will bring them pleasure.

Our immediate neighbors in Vernon continued to help us in manifold
ways and to be enthusiastic about our work. I am happy to thank Mr.
and Mrs. Tom Cox, Mr. and Mrs. Donald Goodman, Mr. and Mrs.
Charles Gillespie, Mr. and Mrs. Leon Gillespie, Mr. and Mrs. Milton
Gillespie, Mr. and Mrs. Cecil Naegle, Mr. and Mrs. Leonard Penrod,
Kenneth Penrod, Mr. and Mrs. Floyd Penrod, Mr. and Mrs. Claude
Phipps, and Mr. and Mrs. Eben Whiting for all favors, large and small.

Miss Lillian Ross, Associate Editor of Scientific Publications, has
earned our gratitude for help in seeing this report through the press and
for catching errors of omission and commission.

Mr. Bertram J. Woodland, Associate Curator, Petrology, identified
the materials from which the stone artifacts were made; Dr. Albert
Forslev, sometime Associate Curator, Mineralogy, and now on the staff
of the College of William and Mary in Norfolk, Virginia, made mineral-
ogical analyses of two samples of clay; and Dr. Fritz Haas, Curator
Emeritus, Lower Invertebrates, checked the shell specimens. We are
grateful to these gentlemen for their help.

Dr. Frederick J. Dockstader, Dr. Fred Eggan, Mr. Byron Harvey III,
and Mrs. Marjorie F. Lambert were kind enough to examine photographs
and data of our sacred stone image and to aid us in our attempts to
identify it. We appreciate their assistance.

Mrs. Agnes McNary Fennell, my secretary, and Miss Lillian Novak
typed the manuscript and tables and deserve great thanks for their
work. Mrs. Fennell also made the index.

Again it is my pleasure and privilege to thank the administration for
its support of the Vernon project. President Stanley Field, Dr. Clifford C.

PREFACE i

Gregg, Director, and our Board of Trustees once more provided us with
funds for the expedition. I hope they will derive as much pleasure
and satisfaction from the results of our work as I do in expressing my
appreciation and indebtedness to them for their sustained interest and
assistance.

PAUL S. MARTIN
January 1, 1961

List of ILLUSTRATIONS . .

Contents

I. ARCHITECTURAL DETAILS. .

Tumbleweed Canyon Site
House A .
Shape .
Walls
Floor
Firepit. .
Lei aaeak ty ae
Postholes .
Roof re:
Milling Area . .
General Comments
House B .
Shape .
Walls
Floor
Firepit .
Pits =
Postholes. .
Roof :
General Comments

House D. .
Shape. .
Walls
Floor
Firepit .
Postholes .
Roof :
Milling Area .
General Comments

Storage Pits(?)

Goesling Site .

Shape .

Walls

Floors .

Firepits

Entrance .

Pit ay

Postholes .

PAGE
15

11)
19
19
19
19
19
19
ils
20
20
20
20

20
20
20
22
22
22
22
22
22

22
22
23
23
25
25
25
25
25
25
26
26
26
28
28
28
29
29

10 CONTENTS

Roof :
General Comments
Chilcott Sites .

Chilcott Site 1
Number of Rooms
Dimensions of Rooms
Walls
Floors .

Firepits

Postholes
Ventilator

Roof

General epacde

Chilcott Sites 2 and 3
Number of Structures
Walls
Floors .

Firepit
Postholes
Roof
Shape .

Thode Site . ;
Number of Rooms
Walls
Floor
Firepit .

Entrances

Pitse.

Postholes .

Roof

General Gonieieare

Rim Valley Pueblo :
Arrangement of Pueblo Bare ;
Number of Rooms
Dimensions of Rooms
Walls :
Ventilators and Niches:

Floors .

Firepits f
Ladder pits(?)
Vault

Bin

Ceiling

General Catimnenta

The Great Kiva, Hooper Ranch Pueblo

Shape .
Dimensions .
Walls

Pictographs

PAGE
29
29

32
32
a2
32
33
34
34
36
37
37
aii
ai
ai
37
ai
By,
37
iyi

40
40
40
40
40
40
40
40
40
40

40
43
43
43
43
46
48
48
48
48
48
50
50

53
53
53
53
54

CONTENTS

Niche .

Recessed Posts

Floor

Bint a)

Firepit .

Deflector .

Vaults .

Crypt

Pits:

Ramp Pniyway

Posts and Postholes

Roof

Comparisons ;
Summary of Secular Aicuitestine

II. Some CONVERGENCES AND CONTINUITIES
The Great Kiva . ‘ee:
The Sacred Stone Image .

III. Porrery. eae
General Remarks . ans
Whole or Restorable Pots ee eer

Relative Popularity of Several of the Significant Pane Boden ie -

IV. SrarTisTIcCAL ANALYSIS OF PAINTED POTTERY TyPEsS FROM UPPER LITTLE

CoLoRADO DRAINAGE
Introduction :
Choice of Materials :
Some Methodological anedecenone :
Basic Procedure .
Inter-Site Seriation

Interpretation
Intra-Site Seriations .

Goesling Site . ‘

Rhoton and Thode Sites ;

Chilcott Site

Rim Valley Pueblo

Hooper Ranch Pueblo .
Conclusions

V. ANALYsIs OF PoTTERY DeEsIGN ELEMENTS
Sorting. .
Analysis .
Conclusions. ; :
Kiatuthlanna ee -on- -White 3
Red Mesa Black-on-White
Snowflake Black-on-White

VI. ARTIFACTS
Introduction .

Tools Used in Preparation and Storaze of Food .

Manos .
Rubbing Saas’

102

oP RLOS
. 106

107
107
109
109
110
115
115

115

116

119

12 CONTENTS
PAGE

Pestles.. g. $c a % es ee Gat eae Re, Sg Se ge
Mietates’ <> = sug Fal com oe OE RIS ie nS
Small Metate- like Grindine tones fea x sae
Mortars <3 of nee car ee Ca et
Pot Covers. she qh - 8 So ee ee
Plaimmerstonés: =. 500s 1s) fee ee 8 eS we cece Soe
jeter IESE gg Rr es se Ay HS
Tools Used in pone: elias eerie ec
Tools Used-in Construction of Houses . =... 5 <*. . 5% =) eee
We ee ee he a ee ee een
Rid se ets as bac tey ed) Te NS oc
Axe-Grinding Slabs 5 ea te od Ah ca Me Ag Ste oly Ge Roe
Choppers . . Nad 24 Caan Oh
‘Tools and ice mene aed in iaasie — Warts ok eae
Projectile, Points” «©... <te shee Sores ehh ee eld
Arrow=Shatt Wools: cg) ses es eR Ss
Household Utility Tools). . 0... 8% 2s 3 2 ae
Flake Knives » . ¢. 2 ss + 48) 3 ve awn,
Sorapers-. sn 2 & 66s Les BER. 2 8” he er
SAWS os gn ceordl a Shae) oe eget Goce SNe acm peel Me et en
Drills . , 7. wees? hw &) Rw a ae ce a
Weaving Tools: ¢ 660d DS. ces hy ee ey
Bore Awl soe ey ce san ey Se eee coe ee ec pet ce ec
Spindle Whorls: 4, 2 ots 2 20 2% @ a 02 ee
Ormamients’..< e s0 ew 8 le eee, ee et es ges eh
Pendants: .. ce se yee ce) eee eee cg eee ee
Beads. -<: sg 208 &« soepaleoa ates) Sp tet ace
Bracelets... .6 4% <-« 3. 6 @ ch Je) ca ccs 5,
RITE Soy vest: err, Se ks es fs 8 GI!
Bone Ring Meiesal errr ee
2b a a Eee eo GG 6 cS ANS
Cut Slrell 9.566. a ae ee ea le lee oo oe
Geremonial: Objects” =... fj... eG s ee ce ee
Gylindeér-Stones).1 os, 2 s,s 0d ots ech, ee et
Sacred(Stone:Image.- . . 3, 2° 5% 12) ec oe cee LG
Worked ‘Sherds: °°... > ke. 46> Sy ee oO
Summary 2060 is ge Oe lo da pcg ee ey ee ag

VII. ARCHAEOLOGICAL RECONNAISSANCE IN EASTERN ARIZONA ..... . . 148
Introdwetion! (0 oe. Mn eh a et ee Le
Organizations 25 ve. ce, veh of wee stoi sO, den, Pema ah) -v got
Field Procedure. .. . of eA go eo
Temporal-Spatial Gbaipation of Surveyed Resion 5 hs it ee eee
Site*Liocations: =. 3s. maw “eas 6) bora Oe eee Le
GeneraliSummary:. ¢.. 7... % ace Ge ee
Gonelusions#...)6 ss Be sy ee a, ee ed ee CO

VIII. Potten ANAtysis or EIGHTEEN ARCHAEOLOGICAL SITES IN ARIZONA AND
INE W, MEEXIGO?.:) cue! te dan Os Pek. aes a eee
Acknowledgments 2.) 6: a. 0k: oh We acl Ee aces
Untroduchion *.21 45) s¢- a; Ao Sowers, oa: ee ee LS

CONTENTS 13

PAGE
Methodscand Eechmiques® Ur e.4 met sos ere se ss Ss ae oe LO
fSLZuaahoubUOV=E® outa” Go wes Oya & a0) SB Sey ine sa Lon ace Dama eDeMetesae ame piarseemane! (27/0)
Pea COM ge area sere ye eRe We wy St Ug At, wal as ie ne a ea ee LL
JAWALVSISN st) cue ee on arnt Pome Mees Gy
Common Names of Pollen Te A Beales aes? Baha cay hee LS
Resulister erties Vics ee RY eee te oh casi aukents! cae et aoULeE
AGEOVONSLLES Ee cman ee +: EPC anny Te Pee MeRB ae, co tia Aaah ay vey SINE
Reach sitesien siecs ss Sy ths GM tay eerste) Be tlwe eites woe wion Seth. ey ay eenkehe
Pithouse Village Sites PoE RA. aetna. Pet tt =, ome eAlT8
IRUGDIOUSIEES Ia ps gales hips ES gon meet ieo) ue nies sy weed a oe me SL
Surface Samples: gs. by eeee acts) sip eee. cared cl Sere ee tee lB
Conclusions .. . Re WORN ses, Somen se fa, he oente es BIA
Interpretations and Tnferendes Me eG eee eh tet lity a os ee Ol
Climatic Change .. . eee er LOM
The Nature of Pre- Being Ragteoteeoral Gacdiiens Pet oporme se lols:
Relationship of Prehistoric Environments to Prehistory . . .. . . 198
Appendix A: sample Collection’ Technique .< . : s+). « «+ = » 206
Appendix B: Pollen Extraction Technique ........... . 207
IX. SumMAaRyY .. . Set Ok Oe ca Re RES ES ser, ees 210
Tumbleweed Cau ait Site eae aA to ot hein ao ey elo
Goeslincssitera me re) oe te ee een Oe be ad BAG 212
OMI COTASILCS ie en NRO, a Re Peete AP alee 5) ens ak Gh we eke a ea penile
MORE Sic at pens Se Pe he Pee Ie Rr. See eT a eh 2
Rim Valley Pueblo ... . CEE eet ee Gor ao, oe Sheet eh “alae Pa
Great Kiva, Hooper Ranch Pueblo Ss Rae eke Ec RCRA en, Stes ge ae I)
Settlement Patterns .. . Eat On Geese, tte ee ey Sake os ee ReaD
Tumbleweed Canyon Site SPP Ser iets ee os hugh Pay eae ke
Pa etee se eat tian i but is) su any, de Sekar Giese
COHMGGEE SULCS ar ohare cue cna ale cad opel botanic! ct aeeeuees LO
Sihodewitesravien me) em rn Che) i565) 4, oe Sim Uetaes er ms ae we CULE,
Rim Valley Pueblo ... . Ne aC oe Lee cin Ie ON ae Cee al ss
Great Kiva, Hooper Ranch Puchla, eS a ees Oke 220
Ainalystsior blements Of cottery WOGSIPMe sos) a se we ee eee
Arcuaeclesical Meroumdisgance . + <b 6 a we OR a oe eee
en RR eC ikag call ai hth eit asle ces Sok HOE ee ek 8 oe BBO
LUMO SIN, UR i, ANE sigh) pha RN ine AM Geen. GM ke Ae

ISPD TEES CALLE rod wep a be Aa Be An ee, oo el ae eae Aiea Paes i mn te 7

er a<wie, “ed
#4 re > ;
bed eK
hed ou Peo ee
7 =e 5S ae . ae
mete i 7
a =" ad eS 7 my
Aeateis’. eae tge Wei rE
=), eee aes i -
hcl

List of Illustrations

Map showing eastern Arizona and western New Mexico Frontispiece
Text Figures
PAGE
1. Panoramic view of Tumbleweed Canyon Site and mesa from across the canyon 20
2. Sketch map of Tumbleweed Canyon Site and environs oe 21
House A, Tumbleweed Canyon aks aca manos, broken metates, and
roof beam fragments . : i Bact sine sole ote es Pare ; 22
4. Plans and sections of houses and pits, Tumbleweed Canyon Site 23
5. Milling area, House A, Tumbleweed Canyon Site, showing manos and broken
metates CORP inas Akrcen hepa ts PT Rahat for cteake bra, | LLY a 24
6. House B, Tumbleweed Canyon se see curb around edge of house and
firepit ; use Su rons States a, oe : 24
7. House D, Tumbleweed Canyon Site, showing broken metate fragments near
center of house and rocks piled up as walls around edge of house . se 25
8. Pithouse A, Goesling Site, showing postholes, firepit in center and southern
recess in background . SOE a, ETRE BO RPA het NSS 26
9. Plans and sections of Pithouses A and B, Goesling Site Ai,
10. Veneer masonry which reinforced north wall of Pithouse A, Goesling Site . 28
11. Pithouse B, Goesling Site, showing shallow pit in northeast corner and quad-
rangular arrangement of postholes . Sat RN ie eae Petes. 20
12. Rooms 1 and 5 in foreground and Structure 2 in background, Chilcott Site 1,
showing alignment of postholes in rooms, and relationship of rooms with
masonry walls to larger structure 30
13. Plans and sections of Chilcott Site 1 31
14. Rooms 3 and 4, Chilcott Site 1, showing reduction in entryway . 32
15. Detail of firepit, deflector, ventilator opening and damper slab, Room 4,
Chilcott Site 1 “A tae eo eins tar Pe ak pe er meer Fe a sao
16. View of Room 1, Chilcott Site 2, showing uneven floor and area of burned
post and rocks near center of structure ; : 34
17. Plans and sections of Chilcott Site 2 (left) and Site 3 3 (right) : ck ah.
18. Room 1, Chilcott Site 3, SORE: basalt boulder walls and general se i of
structure . ‘ i Eee a ist rate Rees tepl oko Se aS |
19. Room 2, Chilcott Site 3, oie rectangular firepit 38
20. Thode Site . ah Tad 38
21. Plan and sections of Thode Site . 39
22. Rim Valley Pueblo, looking south . 41
23. Plan and sections of Rim Valley Pueblo 42
24. Outer wall of Room I, Rim Valley Pueblo 43

LIST OF ILLUSTRATIONS

PAGE
Rectangular doorway in north wall of Room G, Rim Valley Pueblo 44
Oval ventilator in south wall of Room C, Rim Valley Pueblo 45
Niche in north wall of Room A, Rim Valley Pueblo Ae 46
Ring slab from Room C, Rim Valley Pueblo, possibly frame for vent 47
Flour receptacles and corner bin in southeast corner of Room B, Rim Valley
Pueblo . 47
Firepit, ladder-pit, ventilator, and ane slab, Room A, Rim sie Pueblo 49
Room C, Rim Valley Pueblo, with Room B at left and Room H at right . 50
Hooper Ranch Pueblo, showing Great Kiva in foreground and dwelling
rooms in background Pre)
Plan and sections of Great Kiva and adjacent rooms at Hooper Ranch Pueblo 52
Great Kiva, Hooper Ranch Pueblo, from the west. Ramp entryway and
deflector in background; postholes and vaults in foreground . te
Detail of masonry in face of bench on north side of Great Kiva, Hooper
Ranch Pueblo 54
Detail of niche in face of bench on south side of Great Kiva, Hooper Ranch
Pueblo . me hanks 55
Deflector, Great Kiva, Hooper Ranch Pueblo, viewed from ramp entryway . 56
South vault, Great Kiva, Hooper Ranch Pueblo . 56
Ramp entryway, Great Kiva, Hooper Ranch Pueblo, showing ‘‘vestibule”’
area and narrower portion beyond; deflector slab in foreground 57
View through ring slab cover of crypt, Great Kiva, monet Ranch Pueblo,
showing stone image and miniature jar . : os hg ie) ee OS
Crypt in Great Kiva, Hooper Ranch Pueblo, with covers removed, showing
construction detail of interior and objects in position . aye)
Painted sacred stone image, Great Kiva, Hooper Ranch Pueblo 70
Snowflake Black-on-White pottery . 78
Brown indented corrugated pottery . 7)
McDonald Corrugated bowl wf.
Schematic illustration of relative similarity between samples of pottery.
(a) Chilcott Sites; (6) Rim anes Pueblo; ) See Ranch Pueblo; and
(d) site totals . = 91
Percentages of three pottery types by I levels at Goesling Site . 92
‘Trends in oe a er a oS eo from Chilcott Sites and Rim Valley
Pueblo . . er ho eye a dee cl AM A cs BOT
Trends in painted pottery types: — from sae Ranch Pueblo . 101
One-hand manos, Tumbleweed Canyon Site : Bali
Intermediate and late ees of manos, Rim ue Pucblo, Thode Site, Chil-
cott Site 1 ; : See = ks
Rubbing stones, miscellaneous types, Gosling Site, Thode Site, Rim Valley
Pueblo, Hooper Ranch Pueblo Seb: ride 120
Pestles, miscellaneous types, and pee re Tumbleweed ee Site,
Rim Valley Pueblo : : 121
Metates: left specimen basin type, center specimen with trough open at one
end only, right specimen with through trough . 123
Mortar, Thode Site . 2 a5

Pe PNanaAYN =

LIST OF ILLUSTRATIONS 17

PAGE
Maul, axe and pot cover, Rim Valley Pueblo, Hooper Ranch Pueblo . . . 127
Medicine cylinders and pot polishing stones, Hooper Ranch Pueblo, Rim
Walleye OG OeS Ie IEC ie saad eek yt crete RS, beg ecek. ce ce dar pcan) Wee
Axe-grinding slab, Hooper Ranch Pueblo... . . Nee <1
Choppers and large scraper, Tumbleweed eanarine Site, Rim Valley Pueblo,
Chilcott Site 1, Goesling Site . ... 131
Projectile points, miscellaneous types. . . . De eR ey 1hS)>.
Blades, Tumbleweed Canyon Site, Hooper Ranch Pueblo. ...... . 134

Abrading stones, arrow-shaft tool and smooth saw, Hooper Ranch Pueblo . 135

Flake knives and small scrapers, Tumbleweed chiles iaig Chilcott Site 1,

Goesling Site, Hooper Ranch Pueblo... . . = ay,
Drills, punches, saws and blades, Soe Ranch Pueblo, Goesting site, Chil-

cott Site 1, Rim Valley Pachle k! , 138
Bone awls, incised bone fragment, bodkin tip and ring Pitesay eeutnag

Site, Rim Valley Pueblo, Hooper Ranch Pueblo, Thode Site .... . 141
Spindle whorls, worked sherds and miniature jar, Chilcott Site 1, Goesling

Site, looper mance buebloy ese 04 4: = Bee al ce ieee Me ae
Pendants, bracelet fragments, and ring fragment, Goesling Site, Hooper

ReeaeTE LE pee een Ye ees eG, ae Ge inet a hgedeeey ey eka
Map showing area of archaeological survey, east-central Arizona. . . . . 149
Projectiio pomits fromopre-potiery sites 2405. 2s ee kd ee TS
Misceliadcous tools from pre-pottery sites’... . 2 i.) ee Se TB
Scrapers and utilized flakes from pre-pottery sites . . ........ . 159
Gerapen Wore peepatrrmutes oor. a ee eS eee ye TOO

Large bifacially percussion-flaked scrapers/choppers from pre-pottery sites . 161
Choppers and manos from pre-pottery sites .........:. «4+ + 162
Pollen diagrams of archaeological sites in Vernon, Arizona, area . facing page 168

Analyses of three samples of pollen from modern surface and pollen diagrams
of two archaeological sites in Pine Lawn, New Mexico, area. . facing page 172

Important palynological features of samples of pollen from occupation levels
at archaeological sites in Vernon, Arizona, area. .......... 175

Samples of pollen from modern surface at various elevations in Vernon, Ari-
ilig Hine Roce ty Es Gy Be See Su oy Mata plik tee haan Oe me A Ser ane en BPs LY f°

List of Tables

iin Ge eer seocrearer mee Pe FSW. Say eRe ate eee hs at ST
aE OLSEN Cat Cat COT a ECR ine bec eh,. eee te ia Skog) Ole ei ie ebay Re
Cm Or MURR CCIE MRE ee aes we ee A tm ee Se
Totals of sherds, Rim Valley Pueblo... . . daca We Eig et olay Are
Totals of sherds, Great Kiva, Hooper Ranch Pueblo ....... . . 85, 8%
Sample size of sherds and final matrix for inter-site seriation. . . . . . . 93
Sample size of sherds from Goesling Site ..... 5 .+ +s «se «+ +) OF
Sample size of sherds and final matrix, Chilcott Site .......... 95

Sample size of sherds and final matrix, Rim Valley Pueblo... . . . . 98

LIST OF TABLES

PAGE
Sample size of sherds and final matrix, Hooper Ranch Pueblo . . . . . . 100
Percentages of given types by design elements at given sites . . . . . 112,113
Brainerd-Robinson ratios, showing similarity in single types at sites of

different horizons) 4.4. 2. = Seale “A ee) ae i

Brainerd-Robinson ratios, showing similarity in pottery types at single sites . 114

Site locations; pre=-pottery.| Groupee 2a) en sree ret
Sitewocations) Plain Ware, Group) lilies se eee ci eee
Site locations, early black-on-whites, Group EIT = = 32. =] 2. 2) see
Site locations, Reserve-Snowflake Black-on-White, Group IV... . . . 153
Site locations, Tularosa Black-on-White, Group V .......... .. 154
Sitelocations,;ZuniGlazes Group) Vilee. 5) s es eee een
Summary of locational preferences for entire surveyed area . .... . . 154

Comparison of pollen chronologies from southern Arizona and from eastern
Arizona andswesterns News VlexiGOl smn o) ule Ai nen enn ae

I. Architectural Details

By Joun B. Rinatpo

Associate Curator, Department of Anthropology
Chicago Natural History Museum

TUMBLEWEED CANYON SITE

The Tumbleweed Canyon site is located in east-central Arizona ten
or eleven miles southeast of St. Johns and sixteen miles northwest of
Springerville (Sec. 17, Twp. 11 N., R. 28 E., G. and S.R.M.). It is
situated on a small mesa just below the west rim of the Little Colorado
River valley (figs. 1, 2) and overlooks Lyman Reservoir. The sides of the
mesa are precipitous cliffs and the entire mass of rock which forms the
tableland appears to have split off from the higher rim rock to the west.
This geological fault forms a small canyon about 90 feet deep and 150 feet
wide. The canyon received its name from the masses of tumbleweed that
drift up the slope of the west wall.

On top of the mesa were several depressions, some, in a centrally
located group, outlined with basalt boulders. At either end of the oval-
shaped mesa double lines of basalt boulders are piled up in what were
probably walls, and other wall-like structures appear along the edge of
the mesa wherever the rock talus affords a possible means of access.
Numerous stone tools were found on the surface but not a single potsherd.

House A
(Figures 3 and 4)

Shape.—Roughly circular; greatest diameter, 5.4 meters.
Walls.—Basalt boulders and gravelly light gray earth.

Floor.—Gravelly light gray earth; uneven, with rocks protruding
through the surface; depth below present ground level, 20 to 45 cm.

Firepit.—Roughly circular; sides and floor were of gravelly earth;
diameter, 30 cm.; depth, 10 cm.

Pit.—Shallow, oval; sides and floor were of light-colored clay; con-
tents, rocks; length, 42 cm.; width, 27 cm.

20 PREHISTORY OF EASTERN ARIZONA, I

Fic. 1. Panoramic view of Tumbleweed Canyon Site and mesa from across the
canyon; looking north.

Postholes—Were spaced at irregular intervals around the edge of the
house; 18 in number; average diameter, 20 cm.; average depth, 17 cm.

Roof.—Heavy roof timbers radiated from a point near the center of
the house toward the edge of the house and toward the burned butts of
posts; a layer of brush was built up on top of the rafters (thick charcoal
layer), then a layer of clay.

Milling Area (fig. 5).—A cluster of metate fragments and manos was
found near the firepit.

General Comments.——This house burned. An area on the south side
between some of the wall rocks appears to have been an entrance.

House B
(Figures 4 and 6)

Shape-—Roughly “‘D” shape with flat side of ‘‘D”’ on south; greatest
inside diameter, 2.1 meters.

Walls.—Light gray gravelly earth for three walls; basalt boulders were
piled up on the north side; the earthen walls sloped steeply, the north wall
was Closer to vertical; a lip or curb was situated at the top of the wall, 25
to 30 cm. wide, 10 cm. high.

‘suOIIAUS pue 931g UOAURT) podMoyquIny jo deur yI}9049

SY31L3W

juiod wnjoqg VT
Sjid pud sasnoujiq 4-V

S|J]OM Japjnog apnin p-|

‘Oly

in)
bo

PREHISTORY OF EASTERN ARIZONA, I

Fic. 3. House A, Tumbleweed Canyon Site, showing manos and broken metates
zn situ and roof beam fragments radiating toward the center of the house from the edge.

Floor.—Of gravelly earth like walls but brown in color; the surface
was uneven; depth below present ground level, 32 to 65 cm.

Firepit.—Quadrant-shaped; lined with rocks and with a rim consisting
of a row of rocks; diameter, 80 cm.; depth, 8 cm.

Pits —None found.
Postholes—None found.

Roof.—Height and exact character unknown; charcoal was in the fill
and some burned mud but there were no impressions of roofing on the
lumps of mud.

General Comments.—House B was partly burned. Malpais rocks piled
up on the north side may indicate that this house was partly excavated
into the bed-rock of the mesa.

House D!
(Figures 4 and 7)

Shape.—Roughly circular; greatest diameter, 3.6 meters.

1 Symbol “C”’ used for storage pit (fig. 2).

ARCHITECTURAL DETAILS 23

HOUSE A

HOUSE D

d Firepit
met Metate

ma Mono

E43 Roofing poles or timbers
UM, \sndisturded clay

2
HOUSE B
METERS

Fic. 4. Plans and sections of houses and pits, 'umbleweed Canyon Site.

Walls.—Large and small basalt cobbles and boulders were piled up
around the edge of the floor; a narrow shelf of light-colored gravelly earth
was located on the south side of the house. Height of rock wall, 67 cm.

Floor.—Light gray gravelly earth and rocks; surface very uneven;
depth below present ground level, 40 cm.

Suo] “Wd IG MOI

“yqiou oneuseu s}utod
*soUO}S YIM pouTpNO (MOLL MOT

-0q) doazy pue ssnoy jo aspo punoje qano Surmoys

‘au1G uoAURT) PooM

27quiny, ‘gq e8snoFT “9 “SIy

u2 soye}ouWI U
peemeyquin

“a

tou sjyurod

Suoy “Ud YG MOLY

“npis

ayoiq pue sourw Surmoys ‘931g uOAURr)
aie BSUTTTIPY °S “OL

ie ry.

osnoyy ‘e

ARCHITECTURAL DETAILS 25

Fic. 7. House D, Tumbleweed Canyon Site, showing broken metate fragments
near center of house and rocks piled up as walls around edge of house. Arrow 50 cm.
long points north; meter stick in background.

Firepit.—Roughly oval; the floor was of burned gravelly earth; rocks
on the north and east sides formed a rim; length, 44 cm.; width, 33 cm.;
depth, 7 cm.

Postholes—None found.

Roof.—Poles and branches crossed the angles between the larger rocks
of the wall. The roof framework was covered with a layer of brush.

Milling Area.—Fragments of a metate and one mano were found by
the firepit.

General Comments.—This house burned. The entrance may be indi-
cated in the southeast quadrant by a gradual upward slope of the floor
and a lower wall in this area.

STORAGE Pirs(?)

Three roughly circular pits with vertical walls and basin-shaped bot-
toms were trenched, but we did not discover any definite indication as
to how they were used. ‘Two were partly excavated and one was com-
pletely excavated. All contained flint chippings, flint artifacts, and a
small amount of charcoal. They were more than 190 cm. in greatest

26 PREHISTORY OF EASTERN ARIZONA, I

diameter and from 47 cm. to 70 cm. in depth. ‘Two were with the cen-

tral group of houses and within 5 meters of Pithouse A, but the third was

ci ee

io at ge

Fic. 8. Pithouse A, Goesling Site, showing postholes, firepit in center and southern
recess in background. Arrow 50 cm. long points north; meter stick in background.

more than 20 meters to the north. We have called them storage pits
but this designation is simply a guess.

GOESLING SITE
(Figures 8-11)

The Goesling Site is situated on a bluff above the valley of the Little

Colorado River about one mile east of the river and south of the St. Johns—
Salt Lake Highway.

Shape.—The pithouses were roughly ‘“‘D’’-shaped, with the flat side to
the south. Greatest inside diameter: Pithouse A, 5.2 meters; Pithouse B,
3.2 meters.

Walls.—Excavated into gravelly earth. A veneer of slabs laid in abun-
dant mortar reinforced the north and east walls of Pithouse A (fig. 10)
and pebble veneer may have strengthened the north wall of Pithouse B.
A single coat of plaster 0.5 cm. thick was laid on the north wall of Pit-
house A.

PITHOUSE A

a
'
a
=
=
-E
oO
uw
<p)

Firepit
Recess

Posthole

——-—— Wall of earlier
house

—.—.— Wall of later house

Ulli, Undisturbed clay

PITHOUSE SECTION A-A

Fic. 9. Plans and sections of Pithouses A and B, Goesling Site.

28 PREHISTORY OF EASTERN ARIZONA, I

Floors.—A very thin coating of grayish adobe was spread over the
compacted fill in Pithouse A. It was smooth but sloping. No floor coat-
ing was found in Pithouse B, where the floor was gravelly earth.

Buses ree fe ROME as ts Sak lil

Fic. 10. Veneer masonry which reinforced north wall of Pithouse A, Goesling
Site. Meter stick for scale at left.

Firepits—One was excavated in Pithouse A. It is rectangular in shape.
Length, 50 cm.; width, 40 cm. The sides were compacted gravel mixed
with a little clay. It had no definite bottom. The firepit in Pithouse B,
located in the northwest corner, was a small, shallow depression which
contained ashes.

Entrance.—None was located. Entrance was possibly through a hatch-
way in the roof of Pithouse A. No entrance was found for Pithouse B.

ARCHITECTURAL DETAILS 29

Fic. 11. Pithouse B, Goesling Site, showing shallow pit in northeast corner and
quadrangular arrangement of postholes. Arrow 50 cm. long points magnetic north;
meter stick in background.

Pit.—A shallow rectangular pit was located in the northeast corner of
Pithouse B. Length, 80 cm.; width, 60 cm.; depth, 10 cm. The walls
and floor were of gravelly earth. The walls were vertical.

Postholes—Four shallow postholes were found in Pithouse B. Diam-
eters, 20-25 cm.; depths, 8-15 cm. Four postholes were found in Pit-
house A. Diameters, 20-30 cm.

Roof.—Exact character unknown. Made of beams and branches cov-
ered with adobe; evidence obtained from charcoal and burned clay.

Pottery and Artifacts—See Chapters III and VI.

General Comments.—These houses burned and Pithouse A was used for
a pottery dump after it had been abandoned.

CHILCOTT SITES
(Figures 12-19)

The three Chilcott sites were located on the slopes of broad juniper-
covered hills overlooking a valley to the north. ‘They are situated about
a mile north of the highway between Concho and Show Low, Arizona
(Sec. 5, Twp. 11 N., R. 25 E., G. and S.R.M.).

Pa ne ¢ row
* ‘¢ .
Sat = *

Fic. 12. Rooms 1 and 5 in foreground and Structure 2 in background, Chilcott
Site 1, showing alignment of postholes in rooms and relationship of rooms with masonry
walls to larger structure.

Metate

Burial

Ventilator

Pit

Firepit

Post

Posthole
Undisturbed clay
Earlier floor

Loter fill

Unexcavated
Rooms

SECTION B-B’

SECTION A- A’

Fic. 13. Plans and sections of Chilcott Site 1.

SECTION C-C’

32. PREHISTORY OF EASTERN ARIZONA, I

Fic. 14. Chilcott Site 1, Rooms 4 and 3, showing reduction in entryway. Arrow
50 cm. long points magnetic north; meter stick stands against south wall of Room 4.

CuILcoTT SITE 1
(Figures 12-15)

Number of Rooms.—Five rooms and one structure of unknown function
were excavated at Site 1. Some of these were adjacent but only two were
contiguous. Most of the rooms were approximately rectangular in shape.

Dimensions of Rooms.—Rooms range in length from 2.6 to 4.4 meters and
in width from 1.8 to 4.1 meters. The portions of the walls that remain
standing are 35 to 100 cm. high (including excavation into native soil).

Walls.—Floors were excavated into white soil or red clay 5 cm. to
170 cm. below the surface. Masonry was based on the old ground sur-
face above the floor; there were no prepared foundations. The upper
walls were constructed of crude random rubble type masonry made of
assorted unshaped basalt boulders and smaller stones. Some through

ARCHITECTURAL DETAILS 33

Fic. 15. Detail of firepit, deflector, ventilator opening and damper slab, Room 4,
Chilcott Site 1.

stones appeared in the thinner partition wall between Rooms 1 and 5;
also, short lengths of wall were of composite construction, with two facings.
These portions were built with two rows of stones and were 30 cm. thick;
others had only a single row of stones and were 20 cm. thick. The large
number of fallen wall stones indicates that the walls extended a few feet
above their present height.

Mortar: A brown adobe or mud mixture which had dried medium-

hard.

Plaster: A single coat of undecorated mud plaster up to 2.0 cm. thick
had been applied to the walls.

Floors.—Tan native soil or white rock was covered with a layer of gray
to brown adobe clay; the surface is generally uneven, some sections are
smooth. The earlier floor in Room 4 had been partly removed and the
postholes in it covered by a later floor.

34 PREHISTORY OF EASTERN ARIZONA, I

Firepits —Three were found, in Rooms 1, 4, and 5. The one in Room 1
was round, was lined with adobe and was 60 cm. in diameter and 20 cm.

Fic. 16. View of Room 1, Chilcott Site 2, showing uneven floor and area of
burned post and rocks near center of structure. Arrow 50 cm. long points magnetic
north; meter stick in background near test trench.

deep. The one in Room 4 was rectangular, with floor and walls of white
rock except on the south side, where the wall was lined with adobe clay.
A large stone formed the rim on the north, a masonry deflector on the
south (fig. 15); this pit was 65 cm. long, 60 cm. wide, and 22 cm. deep.
The one in Room 5 was rectangular and was lined with adobe plaster;
it was 60 cm. long, 50 cm. wide, and 12 cm. deep. All these firepits con-
tained white ash. Those in Rooms 1 and 4 were near the center of the
room; that in Room 5 was in an angle of the north wall.

Pit.—One in the east end of Room 5 was roughly bell-shaped, and
the bottom was lined with stone slabs. Diameter at mouth, 35 cm., at
floor level, 45 cm.; depth, 35 cm.

Postholes.—Two postholes were aligned down the long axis of Room 5;
another in Room 1 may possibly be an extension of this row. Diameters,
10, 11, 13 em.; depths, 10, 13, 15 cm. Four postholes in the north half
of Room 3 near the walls were 18-30 cm. in diameter and 10 cm. deep.
Four postholes were also found in Room 4; the two later ones were 15 and

@ Posthole

SECTION A-A

ma. Mano

Yi, Undisturbed clay

— \ SECTION B-B’
METERS \

d_ Firepit
COD Masonry
Yl, ndisturded cloy

SECTION A-A’

| 2

METERS

Fic. 17. Plans and sections of Chilcott Site 2 (left) and Site 3 (right).

36 PREHISTORY OF EASTERN ARIZONA, I

31 cm. in diameter, 25 and 33 cm. deep; one was recessed in the east wall,
the other was next to the west wall. The two earlier ones were 28 and
35 cm. in diameter, 48 and 50 cm. deep.

Ventilator (fig. 15).—In the center of the southeast wall; crude rubble
masonry based at floor level reduced the width of a former passage to an
‘‘antechamber”’ (Room 3) from 55 cm. down to 20 cm., and in height
down to 30 cm. It had a stone slab lintel and masonry sides. It was

closed with a stone slab ‘‘damper.’

Fic. 18. Room 1, Chilcott Site 3, showing basalt boulder walls and general shape
of structure. Arrow 50 cm. long points magnetic north; meter stick in background.

ARCHITECTURAL DETAILS 37

Roof.—Evidence from burned clay impressions and charred fragments.
Made of beams and split poles or splints covered with clay. The main
beams or girders were supported by posts.

General Comment.—Rooms 3 and 4 appear to have been the ante-
chamber and main room of a single pithouse (fig. 14) which had been
remodeled into two rooms. A new floor had been added in both sections
covering the postholes in Room 4, and the passageway between the two
rooms had been converted into a ventilator. The butts of wood posts in
these rooms were charred. Apparently these posts were obtained from
trees that were felled by burning them at the base.

CuHILcoTT SITEs 2 AND 3
(Figures 16-19)

Number of Structures—Two structures were excavated at each of these
sites. Trenching and testing in the general sherd area failed to reveal
additional structures.

Walls——Only one structure (Room 1, Site 3) had masonry walls.
These were of random rubble of boulders laid with the flat side to the
interior of the room. Dimensions of stones: length, 22-30 cm., average,
26 cm.; thickness, 15-25 cm., average, 19 cm.; width, 3-4 cm. less than
length. They were laid in abundant mud mortar. No plaster was found.
Dimensions of walls: present height (including earth base), 45-50 cm.;
width, 27—30 cm.

Floors.—Excavated below the old ground level. This soil was com-
pacted and formed the floors which sloped toward the center of the room
and were uneven.

Firepit.—One firepit, located in the south end of Room 2, Site 3, was
rectangular in shape and lined with rough stone slabs. Length, 63 cm.;
width, 54 cm.; depth, 10 cm.

Postholes—One posthole, at the north end of Room 2, Site 3, was 15cm.
in diameter; it contained rotten wood. One near the center of Room 1,
Site 2, was 30 cm. in diameter; it contained a charred post.

Roof.—Exact character unknown. Approximate limits of rooms at
Sites 2 and 3 were determined by dark soil containing minute charcoal
fragments; it is assumed these dwellings were shelters roofed with brush.

Shape.—The three shelters were approximately oval in shape, 4.0 by
3.7 meters, 2.2 by 2.1 meters, 5.75 by 4.75 meters. ‘The room with
masonry walls was roughly rectangular in shape, 2 meters long by 1.75
meters wide.

Fic. 19. Room 2, Chilcott Site 3, showing rectangular firepit in background near
meter stick. Arrow 50 cm. long points magnetic north.

best, tor ;

Pa SEs z

2 > Pn ey ‘e7 S
Pu heey:

Fic. 20. Thode Site. Arrow 50 cm. long points magnetic north and to firepit in
Room E; meter stick at left.

Asuosow
paysabins

Anjo
pequnjsipun

Asuosow

sjolung

jideut4

yw WooYy | Ys

79-9 NOILD3S

‘AUG 2Bpoy,y, JO

4 wooy

N-¥ NOILD3S

y wooy

SWOOY Pa}DADOXauU/)

HHA.

4-8 NOILD3S

40 PREHISTORY OF EASTERN ARIZONA, I

THODE SITE
(Figures 20 and 21)

This small site is situated on the west bank of the east fork of Mineral
Creek about 24% miles east of Vernon, Arizona, on U. S. Highway 60
(Sec. 13, Twp. 10 N., R. 25 E., G. and S.R.M.). Before excavation the
site appeared as a low mound of rocks about 200 yards south of the high-
way and west of a grove of oaks that grow in the creek bottom.

Number of Rooms.—Eleven rooms were excavated. ‘Two or three more
may be present in the north end of the ruin. Several of the rooms are
adjacent but not contiguous (see fig. 21).

Walls.—Crude masonry composed of assorted sizes of unshaped cobbles
and boulders all of igneous rock and ranging in length from 8 cm. to
20 cm. The thinner walls contain some through stones. The greatest
height of the standing wall, including the earthen base, was 67 cm.; the
base of the masonry was on the old ground surface, 25 to 55 cm. above
the floor. The mortar was mud; some stone-to-stone contact was observed
in the bedding planes; no plaster was found.

Floor —Generally dark red clay native to the locality; light-colored
soil in some areas; the surface was fairly even but sloping. The floor
levels were semi-subterranean.

Firepit—One in Room E. ‘“‘D”-shaped with flat (east) side made of a
stone slab set on edge; length, 45 cm.; width, 40 cm.; depth, 35 cm. It was
lined with native clay. Small areas of burned floor and light gray ashes
(not contained in pits) were found in two other rooms (Rooms C and F).
These may have been hearth areas.

Entrances.—None found.

Pits—None found.

Postholes—None found.

Roof.—Exact character unknown. Charred pole fragments were found.
The roofing poles may have been supported by the walls.

General Comments.—This site has the appearance of a series of shallow
pithouses or deep sub-surface rooms clustered about a nucleus (Room E).

RIM VALLEY PUEBLO
(Figure 22)

Situated on a mesa above the west bank of the Little Colorado River
about four miles north of Springerville, Arizona. Rim Valley Pueblo
was built on a little flat about four-fifths of the distance from the rim-rock

Room A contains arrow 50 cm. long

north and meter stick standing against the south wall.

lley Pueblo, looking south.

Rim V

IG. 22.
pointing magnetic

SECTION A-A’

i RmG
a

o
E

a
Bf

Room K fi RmH & Room C
Up a wy 5 fl
MV

SECTION B-B’

Y Yj YY

Firepit

Ladder pit

Vault

Ventilator

Flour receptacles
Bin

Niche

Doorway

Wall abutment
Wall bond
Suggested masonry
Undisturbed clay
Datum point

METERS

Fic. 23. Plan and sections of Rim Valley Pueblo.

ARCHITECTURAL DETAILS 43

Fic. 24. Outer wall of Room I, Rim Valley Pueblo. Meter stick in foreground.

of the cliff to the top of the mesa (NE 4, SW 4, Sec. 8, Twp. 9 N.,
R. 29 E., G. and S.R.M.). The Hooper Ranch Pueblo (see p. 53) lies a
few hundred yards below to the northeast on the opposite bank of the river.

Arrangement of Pueblo Parts—Rooms are grouped in two units of one
story each, on opposite sides of a plaza (fig. 23). The unit on the east side
is small, has only four rooms, is roughly L-shaped and only one room wide.
A larger unit on the west side is rectangular in form and two or three
rooms wide.

Number of Rooms.—Eleven rooms were excavated and fourteen more
were indicated by the outlines of fallen walls; an estimated twenty-one
rooms are in the larger unit.

Dimensions of Rooms.—Roughly rectangular in shape; length, 2.40-
5.65 meters, average, 3.83 meters; width, 1.50-4.50 meters, average,
2.74 meters.

Walls.—No prepared foundations; walls were based on bedrock, on
native soil a few centimeters above bedrock, or, in one instance, on trashy
fill. Masonry started a few centimeters below floor level.

Types of Masonry: Some through stones were used, but most walls
were a product of two facings, each of a different type of masonry built
up one against the other and with some stones interlocking inside the wall.

44 PREHISTORY OF EASTERN ARIZONA, I

Type 1 was similar to vertical slab masonry. A course of large stones
(average 36 cm. long, 24 cm. wide, 2 or 3 cm. less thick than wide) alter-
yw Rae a. q3 . Tun
7 ae Se

‘ va

sen

Fic. 25. Rectangular doorway in north wall of Room G, Rim Valley Pueblo.
Meter stick at right.

nated with several courses of smaller stones including some small slabs
(average 10 cm. long, 8 cm. wide, 6 cm. thick). Small slabs and stones
were used as chinking in the vertical joints between the larger stones.
The outer surface of the exterior walls was generally of this type (fig. 24).

Type 2 was random rubble masonry of cobble-sized stones laid up in
abundant mud mortar. ‘The courses sloped, the stones used were only

ARCHITECTURAL DETAILS 45

Fic. 26. Oval ventilator in south wall of Room C, Rim Valley Pueblo. Meter
stick at right.

roughly matched for size, and the general product was crude in appear-
ance. ‘This type of masonry was generally used for the surfaces of walls
visible from the interior of the room; usually they were covered by plaster.
With the exception of one smaller room (Room G), each room had two
walls with each type of masonry. Generally the south and west walls
were of Type 1, the north and east walls of Type 2.

Dimensions: Walls ranged in thickness from 25 to 38 cm. (average,
31 cm.); present wall heights ranged from 30 to 110 cm. (average, 75 cm.).

Most often basalt boulders and cobbles from local outcroppings were
used as stones in the wall. Many were angular in shape, some rounded.
Less often walls were constructed of laminated sandstone slabs and angu-
Jar chunks of sandstone probably quarried from nearby cliffs.

Small flat or angular pebbles were infrequently inserted in the mud
mortar of the walls to fill voids.

The mortar was soft gray mud of fine texture, occasionally containing
larger particles.

The plaster was gray or brown in color, undecorated, quite thick. It
was applied in a single coat and smoothed over irregularities in the sur-
face of the masonry.

46 PREHISTORY OF EASTERN ARIZONA, I

Fic. 27. Niche in north wall of Room A, Rim Valley Pueblo. Meter stick at left.

Doorways (fig. 25): Both doorways were rectangular: neither had
been sealed and both were through interior (partition) walls. Width,
36 and 45 cm.; probable height (lintel fallen in), 59 and 60 cm.; sills were
adobe plaster or stone slabs; the sides were masonry and the lintel (one
lost) was a stone slab.

Ventilators and Niches (figs. 26, 27).—Six ventilator openings were found,
all in the centers of walls and opposite firepits. Five were rectangular
in shape and with their sills near floor level and one was oval in shape
and with its sill 20 cm. above the floor. Four had lintels of stone slabs
set on end. The others had sides of Type 1 masonry on one side of the
wall with large boulders forming the sides of the opening. The sill of the
oval opening between Rooms H and C was formed by a semicircular arc
carved(?) in a thick slab-like boulder (fig. 28). The sills of the rectangular
openings were adobe clay or slabs covered with adobe. The openings
ranged in width from 20 to 35 cm. (average, 29 cm.), in height from
20 to 33 cm. (average, 29 cm.).

"you 1)0U
-Seur s}urod Suoy “uid QE MOLY “OTgong AaT[eEA Wry ‘gq WooY jo
I9UIOD JSB9YINOS UI UIG I9UIOD Pu sazdR}Jd9991 NOT “67 ‘OY

“JUOA 1oj eure ly ATqISs
-sod ‘ojqeng AaTeA wry ‘D WoOOY wos qeis Suny “gz

48 PREHISTORY OF EASTERN ARIZONA, I

One niche was found in the west wall of Room A, 50 cm. above the
floor near the southwest corner. The height of the opening was 22 cm.;
the width, 24 cm.; the depth, 24 cm. ‘The lining was stone slabs except
the back, which is adobe plaster.

Floors.—Material: A layer of smooth adobe clay was laid 2.0 to 6.0 cm.
thick over gray basalt bedrock or gravelly earth. The adobe curved up
to meet the wall plaster.

Alterations: The vault in Room C was covered with plaster matching
the floor. Part of the floor in Room A was refinished with a thin layer
of adobe.

Flour receptacles: Three flour receptacles (fig. 29) were found in the
southeast quadrant of Room B near the bin. Lengths, 34, 30, 40 cm.;
widths, 28, 30, 33 cm.; depths, 12, 10,6 cm. ‘They have bottoms made of
stone slabs, one of which was smooth and was used as a metate; they were
separated by walls of slabs or manos set on edge or by rows of stones.
Manos and hammerstones were found nearby.

Firepits (fig. 30).—Rectangular in shape, with stone-slab-lined sides
and bottoms; the slabs on the sides projected above the floor level. The
slab on the side toward the ventilator was slightly higher (example,
Room F) than the others. The firepits have gravel or bedrock bottoms
(examples, Rooms B and C). The firepit in Room C was made of rough
slabs; in Room B the slabs were finished more smoothly. Firepits were
generally located in line with the ventilators near the centers of the rooms.
Length, 42-75 cm. (average, 49 cm.); width, 33-62 cm. (average, 40 cm.);
depth, 20-25 cm. (average, 20 cm.). Some firepits have notches in their
sides and gaps at their corners. All the firepits contained fine white ash
and a small amount of charcoal. ‘The one in Room B held a pot rest
stone standing at the center of the south side.

Ladder-pits(?).—Rectangular ladder pits(?) (fig. 30) lined with adobe
plaster and in one instance rimmed with slabs adjoined the firepits in
Rooms A, C, F and J. They are on the side toward the ventilator (east
side). Lengths, 69, 45, 40, 45 cm.; widths, 45, 44, 40, 35 cm.; depths
all 20 cm;

Vault—A vault (fig. 31) was found near the west wall of Room C in
line with the firepit, the ventilator and the door; it had been excavated
into bedrock and lined with two courses of masonry on the west side, one
slab at each end, and one at the east side below floor level. Rectangular
in shape. Length, 75 cm.; width, 36.0 cm.; depth, 25cm. It had been
covered with a later floor. It contained an awl-sharpening stone.

Bin.—A large slab set on edge projected from the south wall of Room
B, making a bin (fig. 29) with three sides in the southeast corner.

Fic. 30. Firepit, ladder-pit, ventilator, and damper slab, Room A, Rim Valley
Pueblo. Arrow 30 cm. long points magnetic north.

50 PREHISTORY OF EASTERN ARIZONA, I

Fic. 31. Room C, Rim Valley Pueblo, with Room B at left and Room H at right.
Arrow 50 cm. long points north; meter stick in background.

Ceiling —Height not known. On the basis of maximum height of walls
yet standing, and fallen wall stones it is estimated to have been about
2 meters high. The method of construction is unknown except by infer-
ence. Fragments of wooden roof members (beams, poles) cross the shorter
dimension of the room.

General Comments.—Rim Valley Pueblo was a small pueblo village con-
sisting of two units both of one story and totaling perhaps twenty-five
rooms. The majority of the larger rooms were equipped with firepits,
ventilators and other features usually associated with dwelling rooms. A
few smaller rooms lacked these features and were probably storage rooms.

The masonry in general seems quite comparable to that of other pueb-
los of roughly the same period and culture (late Reserve Phase, early
Tularosa Phase) both in the upper Little Colorado drainage and farther
to the south and east. Although the particular type of masonry in which
rows of large rocks alternate with several courses of smaller rocks is less
neat here than it appears in later ruins, it is consistent enough in con-
struction so that its position seems definitely to be in that tradition of
banded masonry which may have been remotely inspired by a style origi-
nating in the area of Chaco Canyon.

ARCHITECTURAL DETAILS 51

Some of the features of Room C seem to indicate that it was used for
ceremonial as well as secular functions. ‘The association of ventilator,
firepit and vault, the elaboration of the ladder-pit(?) with arm-like stone

Fic. 32. Hooper Ranch Pueblo, showing Great Kiva in foreground and dwelling
rooms in background. Meter stick stands against north wall of Great Kiva.

slabs on each side, and the position of the vault in the normal location in
a kiva for a foot-drum type of vault or sipapu seem particularly suggestive.
There is also the possibility that the secondary wall through which the
ventilator opening passes could have been the face of a platform or bench.
However, because it seems a little high for this purpose and was filled be-
hind with very large boulders it seems more probable that this boulder-
filled area served as a buttress to strengthen the earlier primary east wall.
These features of Room C when coupled with those from other rooms—
a possible ‘‘kachina’”’ niche in the wall across from the firepit, a ladder-pit
and ventilator in Room A (the southwest corner), and evidence for con-
siderable (ritual?) red paint grinding in the southwest corner of Room B
across from the firepit and ventilator in that room—seem to hint that at
least these rooms were more than ordinary dwelling rooms, ‘Throughout
much of the upper Little Colorado drainage and in the Reserve area up
to the end of the Tularosa Phase small kivas of the Anasazi type seem to

(

Unexcavoted Area

Unexcavated Area

SECTION B-B

//, Y WIIS44

Crypt ;
SECTION 4-4’

Bench

Firepit ‘ Posthole oss Flagstones
Post Vault fr Bin
Platform Deflector ¢

YU, Undisturbed clay
Sealed doorway Upper habitation level

Pit Lower habitation level
Wall abutment w Step
Wall bond T Ventilator tunnel

Bedrock meee Niche

Fic. 33. Plan and sections of Great Kiva and adjacent rooms at Hooper Ranch
Pueblo.

wn
ho

ARCHITECTURAL DETAILS 53

Fic. 34. Great Kiva, Hooper Ranch Pueblo, from the west. Ramp entryway
and deflector in background; postholes and vaults in foreground. Access road runs
diagonally through kiva. Arrow 50 cm. long at left; meter stick in background.

be lacking. These dwelling rooms with more than the common features
possibly could have been used for small group ceremonies as well as for
normal dwelling purposes.

THE GREAT KIVA, HOOPER RANCH PUEBLO
(Figures 32—41)

Hooper Ranch Pueblo is located on the east bank of the Little Colorado
River approximately four miles below Springerville (Sec. 8, Twp. 9 N.,
R. 29 E., G. and S.R.M.).

The kiva itself is situated on the south end of this ruin, which con-
tained perhaps sixty rooms along with two small kivas of the more conven-
tional Western Pueblo type. It is, moreover, a much larger kiva and is
not surrounded by rooms as the others are.

Shape.—Rectangular and fairly symmetrical except that the north wall
was constructed to follow the orientation of the rooms adjoining the kiva
on the north rather than being parallel to the south wall.

Dimensions.—15.5 meters east to west and 14.5 meters north to south.

Walls (fig. 35).—Of masonry. Sandstone slabs, some laminated,
mostly as quarried or rough hewn, were laid up as a veneer against the

54 PREHISTORY OF EASTERN ARIZONA, I

Fic. 35. Detail of masonry in face of bench on north side of Great Kiva, Hooper
Ranch Pueblo. Meter stick at right.

wall of the excavation into the native clay or trash. The north wall is
composed of two facings, and the stones interlock in the interior; the west
wall was built of random rubble; the other walls had large slabs set on
edge or end at the base and regularly coursed rubble walls above. The
vertical joints between the large vertical slabs were filled with a chinking
of stone laid either horizontally or vertically. ‘Thickness: Face of bench,
18 cm.; upper north wall, 45 cm.; other walls, 20 cm. A single layer of
undecorated, dark gray mud plaster was noted but only on the lower walls.

Pictographs.—Pecked areas were uncovered: (1) on a large vertical
slab set in the face of the bench near the middle of the south wall and
west of the niche; (2) on a stone at the corner of the ramp entrance.

Niche (fig. 36).—Near the middle of the face of the bench, in the south
wall. Rectangular in shape and lined with slabs. Width, 50 cm.; height,
28 cm.; depth, 28 cm.

Recessed Posts—One near each of three corners, northwest, southwest
and northeast; these were roof support posts. Their lower sections were
covered by masonry in the face of the bench.

Floor.—Dark gray adobe clay was applied as a single layer; it was
smooth and fairly level. A pit near the northwest corner had been
floored over.

ARCHITECTURAL DETAILS 55

i ~
at. oi

Fic. 36. Detail of niche in face of bench on south side of Great Kiva, Hooper
Ranch Pueblo. Meter stick at right.

Bin.—Five large slabs set on edge crossed the northeast corner diag-
onally on a level with the floor of the bench.

Firepit.—Circular shape, flat bottom; diameter, 50 cm.; depth, 30 em.
It was lined with adobe clay burned red and contained much charcoal
in the form of small fragments, including those of charred corncobs and
walnuts. ‘The surrounding floor west of the deflector was burned.

Fic. 37. Deflector, Great Kiva, Hooper Ranch Pueblo, viewed from ramp entry-
way. Masonry base and masonry-rimmed trough to east. Arrow 30 cm. long points
magnetic north.

Fic. 38. South vault, Great Kiva, Hooper Ranch Pueblo. Arrow 30 cm. long
points magnetic north.

ARCHITECTURAL DETAILS 57

Fic. 39. Ramp entryway, Great Kiva, Hooper Ranch Pueblo, showing wider
‘vestibule’ area and narrower portion beyond; huge deflector slab in foreground.
Meter stick at right.

Deflector (fig. 37).—A large slab had been set on edge between the
firepit and the ramp entryway; it is partially supported by masonry on
the east side and at the ends. Length, 240 cm.; height, 72 cm.; thick-
ness, 15 cm.

Vaults (fig. 38).—Rectangular in shape. One is located on each side
of the floor area. The south vault was lined with stone masonry and par-
titioned into two sections; the north vault was lined with adobe clay and
had a floor of stone slabs. Length: south vault, 133 cm. (total); north
vault, 85 cm. Depth: south vault, 40 cm.; north vault, 30 cm.

Crypt (figs. 40, 41).—A square box, with floor and walls of stone slabs,
has a roof of a ring slab and a rectangular stone slab for a cover. Length,
38 cm.; width, 36 cm.; depth, 28cm. It contained a painted sacred stone

58 PREHISTORY OF EASTERN ARIZONA, I

image (see pp. 69-74), a decorated miniature jar, and black and white
beads. Some of the beads were found inside the jar, others on the floor
of the crypt.

Fic. 40. View through ring slab cover of crypt, Great Kiva, Hooper Ranch
Pueblo, showing stone image and miniature jar in situ. Arrow 30 cm. long points
magnetic north.

Pits —One is oblong, wider at one end, and another is circular, with
walls and floor of native clay; these walls curve to a basin-shaped bottom.
Length of oblong pit, 110 cm.; diameter of circular pit, 38 cm.; depths,
50 cm. and 28 cm. Both pits contained many rocks.

Ramp Entryway (fig. 39).—Oriented to the east, and lined with stone
masonry. Its floor slopes up gradually. A low adobe step is in line with
the upper east wall of the kiva proper. The entrance widens from 110 to
250 cm. at this point, forming a vestibule between the ends of the bench
and the deflector. Width, 100 cm. at outer end; length (outside Kiva
proper), 285 cm.

ARCHITECTURAL DETAILS 59

Posts and Postholes—Nine principal ones, two of them double. The
diameters range from 35 to 100 cm. The posts, 22—30 cm. in diameter,
decayed and/or charred, were wedged in with slabs set on edge around

nam nA Die

a“ ba!
Ay ho,
aharna

Fic. 41. Crypt in Great Kiva, Hooper Ranch Pueblo, with covers removed,
showing construction detail of interior and objects in position.

them. Depths of the postholes ranged from 60 to 100 cm. ‘Three were
located across the west end, two at the east end, and four in a quadri-
lateral arrangement in the main floor area east and west of the vaults.
Two of these postholes were double.

Roof.—Top layers were clay over brush; the exact character of the
lower layers is unknown. The alignment of the principal posts and holes
suggests that four large beams crossed the shorter dimension of the kiva.
The maximum height of the standing upper wall (130 cm.) added to the
maximum height of the veneer masonry for the bench (85 cm.) indicates
a vertical distance from the main floor to the roof of over 2 meters.

60 PREHISTORY OF EASTERN ARIZONA, I

Comparisons—The rectangular shape of the Great Kiva seems to be
most like that of Mogollon Great Kivas such as those described by Hough
(1907, pp. 53, 55-57) on the Blue River, and three kivas closer to Reserve,
New Mexico: that at the Sawmill Site (Bluhm, 1957, pp. 15-27), another
at Higgins Flat Pueblo (Martin, Rinaldo, and Barter, 1957, pp. 13-22),
and one at Casa Malpais near Springerville (Danson, 1957, pp. 82-83).
In this feature, if the ramp entryway is left off it also has obvious relation-
ships to earlier Mogollon small and big kivas (Bluhm, 1957, p. 26) as
well as to contemporary and later western pueblo kivas (Smiley, 1952,
p. 20).

In size it compares with the Nantack Village Great Kiva (Breternitz,
1959, p. 16) and the other larger kivas mentioned above although it is
smaller than the courtyard Great Kiva at Kinishba. On the basis of size
—the paramount criterion—it can certainly be classified as a Great Kiva.

The vertical slab masonry is unlike that of any of the other Mogollon
Great Kivas. It is more nearly comparable to that of Kiva I, Arizona
W :10:52, at Point of Pines (Smiley, 1952, p. 40), or Kiva I at Table Rock
Pueblo (Martin and Rinaldo, 1960b, p. 158). In this feature it appar-
ently reflects the current style of wall construction rather than a tradi-
tional style, although the early Anasazi Great Kivas on Basket Maker III
and Pueblo I sites contain somewhat similar masonry; for example, the
face of the bench in Kiva I of the Cahone Canyon sites (Martin, 1939,
p.230e

The arrangement of the sub-floor vaults on either side of the Great
Kiva has its parallels both in the Mineral Creek Pueblo Great Kiva
(Martin, Rinaldo, and Longacre, 1961, p. 26) and in Anasazi Great Kivas
on Pueblo III sites (Martin, P. S., 1936, pp. 48-49; Morris, E. H., 1921,
p. 119; Roberts, F. H. H., Jr., 1932, pp. 88-89). The use of a small sub-
floor circular firepit rather than a raised hearth or a large rectangular
masonry fireplace has its closest parallels in Anasazi small kivas.

The vaults on the south side of the Great Kivas at the Hooper Ranch
Pueblo and Mineral Creek Pueblo were lined with masonry, whereas the
north vaults were less elaborate. An analogous situation was observed
by Roberts (1932, p. 88) at the Village of the Great Kivas, where the
west vault of the Great Kiva was more complex.

SUMMARY OF SECULAR ARCHITECTURE

The secular structures excavated during the 1960 season present a
hypothetical sequence of architectural development which is complete in
itself and yet roughly parallels that of other areas. The first step in this

ARCHITECTURAL DETAILS 61

sequence is highly conjectural. It is compounded of bits of evidence en-
countered at Laguna Salada, in some of the pit structures at Tumbleweed
Canyon, and from the floor areas at the Chilcott Sites. This postulated
earliest type of structure may have been a light brush shelter erected over
a compacted floor area, or, on occasion, over a shallow excavation. This
stage has its parallel in the Wet Leggett Cochise dwelling area (Martin
and Rinaldo, 1950b, p. 430).

Sometimes (as at Tumbleweed Canyon) the nature of the building site
necessitated the excavation of rocks to secure a smooth floor and a deeper
area more sheltered from the wind. In these instances the rocks were
simply piled up around the edge of the excavation. In at least one in-
stance these piles of rocks appear to have been used for the base of a crib-
like roof structure. This stage has a rough parallel in some of the Pine
Lawn Phase sites in the Reserve area such as the Promontory Site (Mar-
tin, Rinaldo, and Antevs, 1949) where in some rare instances rocks re-
moved in the process of digging a pithouse floor had been piled up around
the perimeter. A more definite parallel is evident at the Bluff Site in
Houses 6 and 15 of the Hilltop Phase (Haury and Sayles, 1947, pp. 24, 38),
which had walls of rubble piled up to hold back the trash out of which
they were excavated.

It is conjectural whether these piled-up rocks formed walls that might
be typologically and sequentially related to the next development (repre-
sented in the Chilcott and Thode sites), which is actual masonry of a
crude rubble type. These walls in the Thode and Chilcott sites were built
up between adjacent rooms of a series of dwellings clustered together.
Although pueblos begin to take form at this stage, there is as yet no pre-
conceived plan. Villages have the form of a series of pithouses or sub-
surface rooms clustered together in an amorphous group, with only an
occasional room tacked on.

Floors were excavated below ground level to various depths and the
walls were continued upward above the ground surface of the excavation
by means of crude rubble masonry of unshaped field stones and cobbles.
In some instances, particularly in the later sites such as Site 31, at Vernon,
the earthen wall of the excavation was faced with a veneer of rubble
masonry of a single thickness, and continued upward above the ground
surface with larger through stones or masonry of a double thickness of
stones (Martin and Rinaldo, 1960a, p. 56). Similar developments in-
volving rooms transitional between pithouses and surface houses with
crude masonry walls have been noted in the Reserve Phase both in the
Reserve area and in the Point of Pines area (Martin, Rinaldo, and Antevs,

62 PREHISTORY OF EASTERN ARIZONA, I

1949, p. 126; Martin and Rinaldo, 1950b, pp. 416-417; Peckham, 1958,
pp. 91-93; Breternitz, 1959, pp: 56-57).

The possibility that these crude masonry walls had extensions of jacal
construction has been suggested. The quantities of wall stones excavated
from these structures in the Vernon area favor the conjecture that the
masonry walls built there were sufficiently high without a jacal extension
for a person to stand upright. No remains of posts have been found
inside the walls to suggest more than a minimum of roof support—nothing
like the rows of postholes indicating jacal walls that were found at Three
Pines Pueblo (Martin and Rinaldo, 1950b, p. 432), and have been postu-
lated for Ruin B at the Nantack Village (Breternitz, 1959, p. 55). This
does not mean that jacal walls were not used in the Vernon area, but
rather that evidence for their existence has not yet been found.

Although the rooms are spaced separately for the most part, at this
stage they tend to approach a rectangular shape, with the exception of
those at the Thode Site. There are apparently very few contiguous rooms
at sites contemporary with this site (Martin, Rinaldo, and Longacre,
1961). However, in the next phase both Mineral Creek Site and Rim
Valley Pueblo are composed of rooms that are contiguous and for the
most part rectangular in shape.

The interior furnishings of the earlier houses are very simple and even
the later rooms have few. In the earlier houses the milling stones and
firepits constitute virtually the only interior furnishings. The firepit is
located near one wall or, less often, in a corner. Ordinarily these fire-
pits are simple shallow depressions excavated into the native soil and are
not lined with plaster. They are more frequently oval or circular in
shape than rectangular. One was outlined with rough stones. Typo-
logically more developed and occurring in later sites are circular firepits
which are located near the centers of the pithouses. These are usually
somewhat deeper and are lined with adobe plaster.

The later houses, such as those at Site 30 (Martin and Rinaldo, 1960a),
are sometimes furnished with storage pits in addition to the milling cen-
ters and firepits. A still later development was the construction of rec-
tangular firepits; some of these are plaster-lined, and others are lined on
the side with rough stone slabs. These occur in the earlier pueblos such
as Chilcott Sites 1 and 3, the Thode Site, and occasionally in the later
pueblos such as the Mineral Creek Site and Rim Valley Pueblo. These
crude stone fireboxes are frequently associated with ventilators and in at
least one instance with a ladder-pit.

The next stage in this development of interior architectural features
is found only at the latest sites excavated in the area. It occurs at Table

ARCHITECTURAL DETAILS 63

Rock Pueblo (Martin and Rinaldo, 1960b), Hooper Ranch Pueblo, and
Rim Valley Pueblo, but not at the Mineral Creek Site. This develop-
ment is represented by centrally located fireboxes with sides and bottoms
lined with nicely worked stone slabs. ‘These fireboxes are often associ-
ated directly with ashpits or ladder-pits and are set so as to be furnished
with fresh air through some form of ventilator. They are also occasion-
ally found in the same rooms with furnishings such as bins and flour re-
ceptacles, which have walls made of stone slabs. This trend toward the
construction of somewhat more elaborate interior furnishings has its par-
allels in the later phases, such as the Tularosa Phase, both in the Reserve
area (Martin et al., 1956; Martin, Rinaldo and Barter, 1957; Rinaldo,
1959) and at Point of Pines (Wendorf, 1950; Breternitz, 1959; Olson,
1960).

In short, the developments in architecture throughout the upper Little
Colorado drainage appear to parallel a similar evolution in the neighbor-
ing areas to the south such as the Reserve area and the Point of Pines
area. Inasmuch as most of these developments involve some form of
stone or masonry construction it seems likely that they had their ultimate
source in the Chaco tradition of the Anasazi culture to the north, where
these arts reached such a high point.

Il. Some Convergences and Continuities

By Joun B. RinALpo

Associate Curator, Department of Anthropology
Chicago Natural History Museum

THE GREAT KIVA

The Great Kiva at the Hooper Ranch Pueblo contains a number of
elements of construction that appear to be modifications of features found
in earlier Great Kivas both in the Mogollon and the Anasazi traditions.
So many of the principal features of this kiva, such as shape of floor plan,
type of entrance, arrangement of roof supports, and primary orientation,
are Mogollon in derivation that the character of the entire structure is of
a distinctly Mogollon cast. Yet some of its furnishings, such as a deflector,
a particular type of vault, a masonry-faced bench, and a wall niche, seem
to indicate that the builders must have been at least influenced in their
planning by the Anasazi tradition. Finally, it contains a few features—
a type of bench, a form of crypt, and an arrangement of roof beams—
which strongly suggest parallel features in historic Western Pueblo kivas.

The rectangular shape of the floor plan (fig. 33) is almost certainly
of Mogollon derivation. Many of the earlier Mogollon ceremonial struc-
tures from the Circle Prairie Phase on up through the Three Circle and
Nantack Phases are rectangular (Wheat, 1954, p. 62; Haury, 1936a, p. 62;
Martin and Rinaldo, 1950a, p. 284; Breternitz, 1959, p. 18; Bluhm, 1957,
p. 15). Moreover, almost all of the later Mogollon Great Kivas are rec-
tangular (Bluhm, loc. cit.; Olson, 1960, p. 199; Martin, Rinaldo, and
Barter, 1957, p. 13). Some of the exceptions, such as the earlier structure
at Higgins Flat Pueblo (Martin, Rinaldo, and Barter, loc. cit.) and the
Mineral Creek Site (Martin, Rinaldo, and Longacre, 1961, p. 23), may
represent examples of either cultural lag or stronger Anasazi influence.

The entrance (fig. 39) was of the ramp type with a short step as one
entered the ‘‘vestibule.’ This type of entrance is considered typical of
Mogollon Great Kivas. It is generally similar to those excavated in the
Reserve area (Martin, Rinaldo, and Barter, 1957, p. 18; Bluhm, loc. cit.;
Rowe, 1947) and to those described for the Blue River area (Hough, 1907,
pp. 53, 55-57) and for Point of Pines (Breternitz, 1959, p. 17; Olson, 1960,

SOME CONVERGENCES AND CONTINUITIES 65

p. 192). Itis both shorter and narrower than most of these, although it is
almost as wide where it widens out into the “‘vestibule.” In common
with the entrance of the Great Kiva at the Dry Prong Site it has a step,
as do the entrances of several other Great Kivas (Nantack Village, Saw-
mill Site, Higgins Flat Pueblo). Somewhat similar lateral entryways with
steps have been found in earlier Mogollon pithouses (Haury, 1936a, figs. 6,
21-23; Martin and Rinaldo, 1950a, p. 276), and the concept may be de-
rived from these or ultimately from the Hohokam (Gladwin, Haury, and
Sayles, 1937, p. 61).

The use of roof support posts in groups of three pillars in some rows
and two in others also seems to have parallels in the earlier Mogollon
Great Kivas. This arrangement is most clearly seen in the later Great
Kiva structure at the Sawmill Site (Bluhm, 1957, fig. 3). A similar group-
ing may be separated out at Higgins Flat Great Kiva (Early) if rows of
posts oriented parallel to the front and rear walls are selected from the
pattern (Martin, Rinaldo, and Barter, 1957, fig. 2; Olson, 1960, fig. 6).
Furthermore, the plaza at Foote Canyon Pueblo (which may have func-
tioned as a Great Kiva) presents a similar arrangement of large posts
(Rinaldo, 1959, fig. 66).

In this connection the positions of the posts and the distance between
them suggest that in the Hooper Ranch Great Kiva sets of beams or girders
crossed the kiva at right angles to the ramp entrance and across the shorter
dimension of the kiva, possibly with two beams side by side across the
middle section, where there are double postholes. However, we did not
find enough of the roof structure to know whether the main beams actually
followed this orientation and positioning—as was the usage in historic
lesser kivas such as that at Shipaulovi (Mindeleff, 1891, fig. 23) or at
Hawikuh (Hodge, 1939, fig. 3) and therefore was an innovation when this
Great Kiva was built—or instead followed some other arrangement in
continuation of the customs in earlier Great Kivas such as that at the
Dry Prong Site (Olson, 1960, p. 192).

The primary orientation of the entire Great Kiva, with its long axis
through the hearth and firepit area, the deflector, and the lateral entrance
running from west to east, is another Mogollon characteristic. This
general orientation is typical of Mogollon pithouses and Great Kivas as
contrasted with those of the Anasazi, which are generally oriented north
to south.

Deflectors (fig. 37), even of the most rudimentary sort, are relatively
rare in Mogollon structures, although they do occur at the Harris Village
(Haury, 1936a, fig. 22) and at Turkey Foot Ridge (Martin and Rinaldo,
1950a, p. 389). As they are a customary furnishing of Anasazi lesser kivas

66 PREHISTORY OF EASTERN ARIZONA, I

and pithouses and are found even in Chaco Great Kivas (Vivian and
Reiter, 1960, p. 90) it would appear that the huge slab set in a masonry
base between the entrance and the hearth area in the Hooper Ranch
Pueblo Great Kiva is a feature that probably was derived from the Ana-
sazi tradition.

The benches found in Anasazi Great Kivas have been discussed by
Vivian and Reiter (1960, p. 88). Like these, the bench (fig. 34) of the
Hooper Ranch Great Kiva is faced with masonry, is relatively level, and
surrounds a lower floor area. Although the concept of a bench, its loca-
tion (surrounding a main floor area), and its masonry facing seem to be
derived from the Anasazi tradition, in dimensions and certain details of
construction the bench in this latter Great Kiva is more like the bench in
the Great Kiva at the Dry Prong Site (Olson, 1960, p. 190), which this
Great Kiva resembles in other features as well. This bench is both
higher and wider than the benches in Anasazi Great Kivas (Morris, 1921,
p. 115; Martin, 1936, p. 50; Roberts, 1932, pp. 91-92; Vivian and Reiter,
1960, pp. 12, 29, 39, 44, 56, 63, 67), and the masonry veneer covers a
native gravelly clay rather than a rubble core.

The benches in these two Mogollon Great Kivas appear to have par-
allels in the banquettes of lesser Hopi kivas both at Awatovi (Smith, W.,
1952b, pp. 5-6) and at the other Hopi towns (Mindeleff, 1891, pp. 122-
129). In fact, the width and general arrangement of the bench in the
Hooper Ranch Great Kiva suggest that this area may have been used by
spectators and participants who sat or stood, as they do in the Hopi kivas,
on the banquette and the elevated portion or platform (Voth, 1901,
pp. 92-93).

The rectangular slab-lined niche (fig. 36) in the center of the face of
the south bench would seem to be another example of a feature in the
Anasazi tradition. Niches, or, as Vivian calls them, “‘wall crypts,” are
generally lacking in Mogollon pithouse-kivas and Great Kivas, but they
have been found relatively often in Anasazi lesser kivas and Great Kivas
(Vivian and Reiter, 1960, p. 84).

Also suggestive of Anasazi inspiration is the fact that the niche and
the north and south vaults form a southward oriented row or secondary
axis of features across the short dimension and through the center of the
Great Kiva. This ‘“‘axis’? seems to link up directly with the row of fea-
tures in Kiva I (ventilator, ashpit, firepit, vault and kachina-kihu) with
which it is roughly in line (fig. 33, section B—B’). The north to south
orientation of this row is the traditional arrangement found in the ma-
jority of kivas in the Zuni, Acoma and Hopi villages (Mindeleff, 1891,
pp. 115, 116) and in most Anasazi pithouses and kivas (Kidder, 1958,

SOME CONVERGENCES AND CONTINUITIES 67

p. 246), whereas generally in the earlier Mogollon culture an eastward
orientation prevails. The niche seems to constitute the focus for the sec-
ondary north to south axis in the same way that the lateral entrance does
for the primary eastward orientation.

The north vault, which was not lined with masonry, seems to be analo-
gous to the simple resonator pits found in some earlier Mogollon Great
Kivas (Bluhm, 1957, p. 18; Olson, 1960, p. 193; Martin, Rinaldo and
Longacre, 1961, pp. 29, 58,59). But the south vault (fig. 38), which had
masonry lining, division into two compartments, and general complexity,
and was also contiguous to a primary roof support posthole, resembles the
vaults in Anasazi Great Kivas to a considerable degree. The greater com-
plexity of the western vaults in Anasazi Great Kivas has been noted by
Roberts (1932, p. 88) and Vivian and Reiter (1960, p. 93). At Hooper
Ranch and at Mineral Creek Site the analogous southern vaults were the
more complex, and they included the use of stone masonry, a feature which
does not appear in the grooves and resonators of the earlier Mogollon
Great Kivas to the south, and which is probably derived from the Ana-
sazi. It is probably no mere coincidence that the crypt containing the
sacred stone image was in this area of the Great Kiva floor and was asso-
ciated with this vault.

It is interesting to observe that this crypt (fig. 40) had a double cover,
the lower part consisting of a perforated slab or ring slab, the upper, a
rectangular worked slab. This appears to be another instance in which
the perforated slab for a small structure such as a niche formed a frame
similar to that used for the doors or hatchways of dwellings, as at Kin-
tiel (Mindeleff, 1891, pp. 192-194), at Four Mile Ruin (Fewkes, 1904,
pp. 160-161), and at Table Rock Pueblo (Martin and Rinaldo, 1960b,
pp. 157, 174). Once again, as in the kachina-kihu at Table Rock Pueblo,
the concept seems to be that of a spirit’s entrance, but in this case the
idea is reinforced by the occurrence of the stone image within the crypt.

According to Stephen (Parsons, Editor, 1936, p. 261) there was a
niche-cache (his term) which contained an image in the Wikwalobi kiva
at Sichomovi. This he records as follows: ‘‘Tihkuyiki (Childbirth water
house) or Tuwabontumsiki, the phallic niche-cache in this kiva.. . is an
oblong rectangle, say six by eight inches. It contains one object, an
image. The cavity is about fifteen inches deep. Tuwabontumsi, Sand
altar woman, is the wife of Masauwu, and the sister of Muriyinwu. She
gave birth to all kachina. She is also called Muriyinmana, also called
Tihkuyi, Childbirth water.” Stephen does not say whether this ‘“‘niche-
cache” is in the floor, the bench or the wall, but there is an obvious re-
semblance in shape and function.

68 PREHISTORY OF EASTERN ARIZONA, I

There was no direct evidence as to the use of the vaults in the Hooper
Ranch Great Kiva. As neither of them showed signs of fire or contained
ashes, they were certainly not auxiliary firepits. Although they could
have been used as foot-drums there is no evidence for it other than the
parallels mentioned above, and they are too small for use as sudatories,
as Vivian and Reiter have suggested (1960, p. 93). The division of the
south vault into two compartments has its parallel in Great Kiva I at
Pueblo Bonito (op. cit., p. 67) and this seems to lend credence to another
suggestion Vivian and Reiter have made concerning their use as containers
for growing beans, corn or other plants as part of a hypothetical ceremony
possibly ancestral to Powamu. It is suggested that one compartment
could have been used for growing beans and the other for growing either
beans or corn.

However, if such were the case, the diminutive size of the firepit
(diameter, 50 cm.; depth, 30 cm.) relative to the air space to be heated
(estimated at over 500 cubic meters) within the Great Kiva presents a
problem, assuming of course that the postulated ancestral Powamu cere-
mony was much like the contemporary ceremony in which plants are
forced during the coldest month of the year. The huge size of the fire
screen provides a possible answer. When excavated, the firepit contained
mostly charcoal, but the area surrounding the firepit for some distance
was burned red. This suggests the possibility that the burned area was
used for a hearth, as in the earlier Great Kivas at the Dry Prong Site,
the Sawmill Site and Higgins Flat Pueblo, and that the small circular
firepit was used primarily for the storing of hot coals, as in the firepits at
Site 481 in the Quemado area (Smith, W., 1950, p. 396).

On the whole, the Hooper Ranch Great Kiva seems to constitute an
example of converging traditions, formed as it is of architectural features
stemming from both the Anasazi and the Mogollon ceremonial structures.
The deflector, the masonry lining and division into compartments of the
south vault, the masonry veneer, and the general concept of the bench
and the wall niche are parallel to features which have been found more
frequently in Anasazi lesser kivas and Great Kivas. But the rectangular
shape of the floor plan, the lateral stepped entrance, the general arrange-
ment of the roof supports, and the primary orientation of the structure
toward the east are elements represented more strongly in Mogollon pit-
houses and Great Kivas. Thus the Great Kiva contains within it the
elements of a convergence of the Chaco tradition of the Anasazi and the
Tularosa tradition of the Mogollon, a convergence which is more clearly
exemplified in the ceramics which the kivas contained.

SOME CONVERGENCES AND CONTINUITIES 69

THE SACRED STONE IMAGE

Before we discuss this stone figure a word of caution is perhaps needed.
In our attempt to probe the relationships of the stone image to possible
present-day counterparts we have tended to emphasize Hopi rather than
Zuni similarities. This is not because the culture at Hooper Ranch Pueblo
appears to be more closely related to Hopi culture. Quite to the con-
trary, we feel that the architectural and ceramic traditions, the settlement
patterns and other traits provide a more definite link with the Zuni cul-
ture. However, the literature on the Hopi is in general more complete,
particularly on those subjects with which we are concerned here, so that
it is much easier to draw parallels in the direction of Hopi culture. Of
course, there are also other traits, both in ceramics and architecture,
which might link this culture in that direction, but they tend to be repre-
sented to a lesser extent than the Zuni traits.

The sacred stone image (fig. 42) is sufficiently specialized in form and
decoration to enable us to examine it with more assurance than was possi-
ble with the similar figures that appear in the pictographs on the walls
of the pueblo rooms (Martin, Rinaldo and Longacre, 1961, pp. 55-56).
The posture of the arms and legs is similar to that of the pictographs, but
the sculpturing of the hands and feet of the image was done with greater
precision, and the features of the face and the decoration in colors which
are found on the effigy do not appear at all in the pictographs.

This is clearly an anthropomorphic figure. The left arm is upraised
and bent at the elbow. The right arm is missing, broken off in ancient
times. The legs are spread out and bent at the knees. The nose, chin,
hands and feet are carved in relief, and the mouth and possible vulva ap-
pear as small cavities. The hair and eyes are painted black, and the
left eye is lower than the right and roughly diamond-shaped rather than
oval. The front of the body, the face, and the limbs are painted yellow.
The hands are black, bordered by a red stripe at the wrist, and the feet
are bordered by red stripes and possibly by black stripes(?) at the ankles.
The body is decorated on the front by a series of vertical stripes in the
following sequence (proceeding from the figure’s left side): yellow, blue-
green, red, black, yellow, blue-green, black (center stripe), blue-green,
yellow, black, red.

Except for white (east), which is omitted, these are the directional
colors of both Hopi and Zuni (Parsons, 1939, pp. 186, 218, 172; Bunzel,
1932, pp. 670, 714; Voth, 1901, p. 75). It may be pure chance that the
first few color-directions of this series happen to be in the same sequence
that the Hopi use in their ritual circuit—yellow (north),' blue-green

! Actually northwest, southwest, southeast, etc.—points of sunrise and sunset at
the solstices.

Fic. 42. Painted sacred stone image, Great Kiva, Hooper Ranch Pueblo.

SOME CONVERGENCES AND CONTINUITIES 71

(west), red (south), black (zenith), but omitting white (east). The factor
which suggests that this particular sequence might be Hopi rather than
Zuni is that among the Hopi the color for zenith is black, whereas among
the Zuni it is “‘all colors” or ‘‘speckled’”’ (Parsons, op. cit., pp. 172, 365;
Voth, loc. cit.; Bunzel, loc. cit.). Zenith is always named after east and
before nadir by both Zuni and Hopi. Although the series in the direc-
tional circuit is the sequence followed in the colors of some ceremonial
objects and paintings (Voth, 1901, pls. 42, 47, 53; Stevenson, 1904, pls. 74,
108) it is not used on the majority; so this clue as to the cultural identity
of the image is weak.

However, there are some additional clues which seem to corroborate
this color-directional symbolism among the former occupants of Hooper
Ranch Pueblo. (1) The figure was accompanied in the crypt by a minia-
ture narrow-mouth jar containing six black beads, five white beads, one
blue-green bead, and a red chip of stone. These objects might be inter-
preted to represent the directions zenith (or nadir), east, west and south
respectively (omitting north). (2) Yellow pigment in quantity and yellow
bone beads were found in the north vault of Kiva I. (3) Painted stones on
which green was the dominant color were found near the center of the
west wall of the Great Kiva.

Aside from the obvious clues to its religious character provided by the
position of the stone image in a large ceremonial structure, the associated
sacred objects in the crypt and the lavish use of the directional colors sug-
gest that this represents a supernatural being. But the question arises as to
what kind of a supernatural being—a proto-kachina, a cult deity, or a clan
wuya? The wuya (a clan protector, clan symbol, or clan ancient) finds
so little expression in the literature (Titiev, 1944, p. 155) that we found
nothing specific to tie to and felt at a loss to pursue the matter further.

A search was made through the literature pertaining to kachinas and
through our museum collections for a figure closely resembling this image
but we were unable to find any. Except that one eye is lower than the
other and of different shape (cf. Smith, W., 1952b, p. 123, note 45) and
there is possibly a straight throat line with a black band underneath
(which creates the impression of a half-mask) there are no facial features
of the image suggestive of a mask. The nose and mouth are generally
naturalistic in form and there is no evidence of headdresses, horns, feath-
ers, beaks, tubular mouths, “‘beards,” special face painting, or other attri-
butes ordinarily found on kachina figures (Colton, 1959; Fewkes, 1903).
Furthermore, there were no kachinas in the same posture as the image—
arms raised and elbows bent, legs spread out and knees bent, etc. How-
ever, some were found which were similar in one or two details. For

72 PREHISTORY OF EASTERN ARIZONA, I

example, a few have yellow masks with black eyes (Citulilu, Fewkes, 1903,
pl. 44), but are unlike the image in other details. Vertical stripes on the
body are seen on Patun or Squash (op. cit., pl. 52, p. 116) and on Rainbow
(Stevenson, 1904, pl. 74). They also appear on a number of dolls of the
older flat type in our collections, but on these the stripes are almost always
in fewer colors.

There is a closer degree of likeness between the stone image and the
figurines of cult deities which appear on the altars in the Marau and
Wuwutcim ceremonies of the Hopi. ‘This seems to be particularly true
of versions of Talatumsi and Marau-mana (Parsons, Editor, 1936, pp. 883,
964, figs. 467, 484, pl. 23; Fewkes and Stephen, 1892, p. 196, pl. 1, fig. 2;
Fewkes, 1894, p. 69; Voth, 1912, pls. 5, 10, 13). These are usually repre-
sented with flat yellow faces, black hair and eyes, and yellow torsos of
roughly the same proportions as those of the image. On at least two of the
figurines the feet are rendered in some detail and have flat soles like those
of the figurine, so that they can be stood alone on the altar floor or tied
to the “rainbow” bar. Their feet are usually spread apart a small dis-
tance and they have their arms upraised in a pose similar to that of the
image. Talatumsi is clad in cotton garments on occasion and there is the
possibility that the stone image was similarly clothed at one time (Parsons,
Editor, 1936, p. 964), so that the vertical stripes or body-painting may be
irrelevant to identification.

The posture with arms upraised and feet spread apart with knees bent
is occasionally seen in depictions of other cult deities, Alosaka, for example
(Fewkes, 1903, pl. 59), and there is a striking resemblance in several attri-
butes to the figures of anthropomorphic supernatural beings seen in some
Navaho sand paintings. The somewhat elongated form of the torso, the
position of the arms and legs, the longitudinal multi-colored stripes on
the body and the yellow face are found on these figures in some instances
(Wyman, 1952, fig. 38, for example). Because these sand paintings are
thought to have retained some of the archaic features of the older Pueblo
dry paintings (from which they were derived) these Navaho figures may
indirectly corroborate our identification of the image as a representation
of a supernatural being, possibly a cult deity. It is therefore suggested
that in particular the posture is symbolic of cult deities as differentiated
from kachinas although it could equally well be a conventionalized atti-
tude representing childbirth, sexual intercourse (Cosgrove, 1932, pl. 225, f;
Smith, W., 1952b, figs. 53, b, 92, a) or any one of several other alternatives.

There is further evidence for the female character of the stone image
in its dominant yellow color, which among contemporary Pueblo Indians
is symbolic of females (Parsons, 1939, pp. 102, 275) and there is also some

SOME CONVERGENCES AND CONTINUITIES Fis

archaeological confirmation for yellow being a “‘female”’ color. Six fig-
ures in the Awatovi murals and one in a Mimbres Polychrome bowl—all
definitely female—are painted yellow (Smith, W., 1952b, figs. 51, c, 53, b,
67, d, 78, a, b, 81, b; Nesbitt, 1931, pl. 23, 6). Moreover, they are similar
in other attributes. Five of the Awatovi figures have upraised yellow arms
(Smith, W., 1952b, figs. 51, c, 53, 6, 78, 6, 81, 6) and two of them have
black hands like the stone figure (op. cit., figs. 53, b, 81, 6). There are
other archaeological parallels; the similarity in posture between that of
the stone image and those of the anthropomorphic figures in certain
Four Mile Polychrome bowls is inescapable (Martin and Willis, 1940,
pl. I; Fewkes, 1904, pl. 25, a); and, as mentioned above, the posture is
much like that of the anthropomorphic pictographs found on the walls
of the dwelling rooms at the Hooper Ranch Pueblo. A figure in this pos-
ture was also found painted on a stone slab at Kinishba (Cummings, 1940,
pl. 34).

Taken together, the data favor the identification of the image as a
female cult deity related to the underworld rather than as a proto-
kachina. The resemblances of the image to cult deity figurines of the
present-day Hopi are particularly important in this connection and have
been discussed in detail. The location of the image in a crypt in the
Great Kiva floor bears out the relationship to the underworld. The
crypt is analogous (on a small scale) to the kiva itself, with the aperture
apparently representing the kiva entrance. The aperture is also prob-
ably symbolic of the entrance to the underworld, and the crypt of the
underworld itself. As such it must have been a particularly sacred place.
The location of the image in this crypt seems to indicate that the deity
represented by the image was related to the underworld. In Stephen’s
time the figure of Tuwabontumsi (a cult deity) was kept in a “‘niche-
cache” in the kiva (see p. 67), and while today the figure of Talatumsi
(another female cult deity) is kept in a shrine on the cliffs (Titiev, 1944,
p. 131, pl. 3, 6), this may be a relatively recent custom.

More specifically, the image may be identified as representing a female
cult deity belonging to a group that is concerned with childbirth, repro-
duction and fertility (particularly fecundity in men and animals rather
than in vegetation). Included in this group are those female deities men-
tioned above: Talatumsi, Tuwapongtumsi and Marau-mana. These may
have been differentiated from a single ancestral deity.

There is a possibility that the image represented the ancestral deity
from which the three (or more) present-day deities (Talatumsi, Tuwa-
pongtumsi and Marau-mana) were differentiated long ago. ‘There is
also the possibility that it represented simply another deity, also of the

74 PREHISTORY OF EASTERN ARIZONA, I

same group, who has been forgotten; and no doubt there are other pos-
sibilities. Most of the data seem to support the theory that the image
represents a cult deity rather than a proto-kachina, although we cannot
rule out that possibility either, for the asymmetrical eyes and the lower
face have mask-like qualities, and the vertical striping resembles that of
some of the older kachina dolls. However, resemblances in hands, feet,
head, general torso form and posture are closer to those of both ancient
and modern representations of cult deities. Its position in the Great Kiva
crypt—a particularly sacred place—bears this out and also its relationship
to the underworld. Its sexual parts and dominant yellow color indicate
that it is a female. As might be expected, it is most like the older repre-
sentations of supernatural beings, particularly those yellow central figures
in the Awatovi murals who stand with their arms upraised as if bestow-
ing blessings.

Dr. Fred Eggan (verbal communication) has suggested that this dif-
ferentiation may have occurred through the addition of new population
groups with similar beliefs and rituals, with subsequent partial equating
of the deities involved, or through later development of parallel cults
consequent on population increase, and with different versions of cult
deities and rituals.

III. Pottery

By Paut S. MartTIN

Chief Curator, Department of Anthropology
Chicago Natural History Museum

GENERAL REMARKS

The study of prehistoric pottery from a given area is a vast under-
taking and one could devote an infinite amount of time to it. Not only
does one have the materials of manufacture—clays, tempering materials,
slip-clay and pigments—to comprehend but also the decoration on the
pottery, analysis of design-elements, temporal and spatial relationships of
types and “horizon styles’? to pursue and to grasp. Small wonder that
one can become involved and bogged down in minutiae and perhaps lose
his way in a maze of technological and esthetic problems. Thus, it is
difficult to persuade oneself not to make the study of pottery an end in
itself. One can avoid this danger by integrating the ceramic data with
all other available data and making interpretations from this combined
information.

In this brief section I shall present the data that might conceivably
be useful to other students who may wish to use this information for mak-
ing other and different interpretations.

To supplement my remarks, I persuaded Miss Cronin and Mr. Free-
man, graduate students in the Department cf Anthropology, the Univer-
sity of Chicago, to pursue two investigations and to report on their efforts.
Miss Cronin’s investigation dealt with possible derivation of Snowflake
Black-on-White pottery through the analysis of elements of designs. Mr.
Freeman’s study was concerned with statistical analysis of the painted
pottery types recovered from the excavations and an ordering of the sites
based on this analysis.

The reports of Miss Cronin and Mr. Freeman follow this chapter.

I have not discussed the method of manufacture—securing and pre-
paring clays, shaping, polishing or finishing—inasmuch as this problem
has been well ventilated several times. Also omitted are such items as
origins (except for the chapter on the lineage of Snowflake Black-on-

76 PREHISTORY OF EASTERN ARIZONA, I

White pottery), paste, tempering, paints, shapes, and decoration. A dis-
cussion of these would seem superfluous since all the types mentioned in
the alphabetically arranged lists at the end of this chapter have been
described and illustrated (see citations in Martin, Rinaldo, and Longacre,
1961, pp. 143-144). The exceptions are Gila Polychrome, for which I
cite Haury (1945, pp. 63-80), and Snowflake Black-on-White, a type that
we are not yet ready to describe.

The uses to which pottery was put may briefly be listed: in the prepa-
ration, cooking and serving of foods (the practice of providing separate
containers or plates for each individual was unknown to these people);
in the storage of water, foods, and seeds; and in ceremonial and mortu-
ary rituals.

In other reports, we have frequently mentioned “‘trade”’ or “‘intrusive”’
pottery; in this chapter there is no such subdivision. If I possessed data
derived from the technological methods of analysis (petrographic and
other laboratory results obtained from thin sections) and if I could com-
bine these with information regarding style and general appearances of
pottery derived from direct inspection, I should be happy to make lists
of possible intrusives. These data I do not have. Rare, unique or un-
familiar types may be possible intrusives, but I prefer to list them as
unknowns until such time as I can avail myself of analytical methods of
identifying ceramic materials. Such identification, however, may be
slow and costly and it requires special laboratory equipment and a trained
ceramist. These, unfortunately, are not always at hand.

In Freeman’s report (chapter IV) the author leaned heavily on pottery
for relative dating of sites. The pottery types chosen for this purpose had
already been dated elsewhere, for the most part by dendrochronology,
and have a relatively short time span. This inferential method was
chosen because (1) pottery possesses a variety of features and richness of
development; and (2) it was the only one open to us for creating a chrono-
logical frame of reference, since we lacked absolute dates for any of the
sites. The ordering of the sites is probably correct; assigning estimated
dates to them is a complex matter, depending as it does on intangible
factors, the prejudices of the authors, and unrecorded impressions gained
from the excavations. The assignment of dates will be deferred to the
last chapter.

Miss Cronin found herself involved in the question of ceramic change.
Did the changes in design elements come about gradually or suddenly?
Long experience in sorting and classifying sherds leads me to believe that
pottery represents a continuous stream of development and that changes
in design elements and style occurred gradually, for the most part, and

PODPTERY We

that the potters were not aware that they were taking place. The mech-
anisms for producing changes in pottery designs are not well understood.
It is often assumed that there is manipulation of designs resulting in fresh-
ness and variety of treatment (Bunzel, 1929, p. 57). Rands (1961, p. 333)
suggests that in some traditions stylistic changes are made up of small
innovations that are cumulative; or that minor changes are in the nature
of substitutions rather than accumulations.

Whatever may have been the mechanisms for changes in pottery de-
signs, one can sense a general drift throughout a larger area. Indeed,
even though I can not document it, I advance the speculation that the
trend in ceramic designs throughout much of the Southwest may have
been “‘drifting’’ along the same general path at roughly the same time
levels. In other words, we may have horizon styles (Willey, 1948, p. 8)
in the Southwest.

A total of 15,243 sherds of all types was recovered from six sites.
In chronological order, early to late, the frequencies are as follows:

(Coesiinpsoite (earliest) pterant or mrceos sta: soe ao ks ete 4,988
PPNOLOMMSILLE RT Ieee ee clk eee tates 2 FERAL Te cA vee 136
Gane CREATE SEA) ete tard eat Mey Mere RE ce sual hl ay lov Pn ol egal 2,602
Senet Aad cree. ee poe CIA I iss aN" ae acaranel WOM 765
ACTEM Wille vue DO ore erie ioe PES Lee fae cic x io tae y aces 2,188
Great Kiva, Hooper Ranch Pueblo (latest)............. 4,564

PGA eer tee eter ea ae rene ek tie ie-t dete pe ee 15,243

Tables showing total sherd tabulations and percentages for all sites
(except Rhoton Site) are presented at the end of this chapter. We have
not included any remarks on the pottery types or the architectural de-
tails of the Rhoton Site (a very small one) because one day’s digging
produced only a few sherds and not much else. Cronin and Freeman
wanted, however, to include the Rhoton sherds in their analyses because
the designs and types seemed pertinent.

Complete sherd counts for all rooms and levels have been published
(Martin, Rinaldo, Longacre, and Freeman, 1961).

Someone may observe that the total number of sherds for the Hooper
Ranch Pueblo (Great Kiva) as given here (4,564) does not agree with
the number (4,998) of sherds for the Hooper Ranch Pueblo as given by
Freeman in his chapter. Mr. Freeman used the sherd count from the
Great Kiva and also from some of the rooms of the Pueblo (dug in pre-
vious season, 1959; Martin, Rinaldo and Longacre, 1961).

78 PREHISTORY OF EASTERN ARIZONA, I

Fic. 43. Snowflake Black-on-White pottery.

WHOLE OR RESTORABLE POTS RECOVERED!

1. Red Mesa Black-on-White bowl (incipient Snowflake Black-on-
White?); cat. no. 280955; found in fill 2 of Pithouse A, Goesling Site
(fig. 43, right).

2. Snowflake Black-on-White bowl (cat. no. 280954); found on floor
of Room 1, Chilcott Site 1 (fig. 43, left).

3. Snowflake Black-on-White pitcher (cat. no. 280935); found near
House 2, Chilcott Site 1.

4. Snowflake Black-on-White(?) pitcher (cat. no. 280936); found with
burial no. 1, Room A, Thode Site (fig. 43, center).

5. Brown indented corrugated, smudged interior, bowl (cat. no.
280937); found with burial no. 1, Room A, Thode Site (fig. 44, right).

6. Brown indented corrugated, smudged interior, bowl (cat. no.
280938); found with burial no. 1, Room A, Thode Site.

7. Brown indented corrugated jar (cat. no. 280939); found with
burial no. 1, Room A, Thode Site (fig. 44, left).

8. McDonald Corrugated bowl (cat. no. 280940); found on floor of

Room B, Rim Valley Pueblo (fig. 45).
. 9. Woodruff Smudged bowl (cat. no. 280941); found on floor of
Room G, Rim Valley Pueblo.

1 Listed in approximate chronological order of sites; earliest sites given first and
latest, last.

‘DN

Fic. 44. Brown indented corrugated pottery.

#4h\ :
‘ie

Hialer,

}

McDonald Corrugated bowl.

45.

Fic.

80 PREHISTORY OF EASTERN ARIZONA, I

10. Heshota-uthla Polychrome(?) jar, miniature (cat. no. 280953);
found in floor crypt with sacred stone image; Great Kiva, Hooper Ranch
Pueblo.

RELATIVE POPULARITY OF SEVERAL OF THE
SIGNIFICANT PAINTED POTTERY TYPES

These sites are listed according to the seriation or ordering as worked
out by Freeman (Chapter IV).

1. Goesling Site; two pithouses dug:

oO
/ oO

Red Mesa Black-on-Wihiten. «5.4004 665. 6 eee DA aes

KiatuthlannayBlack-on-=\Wihites 7. ae ee eee ae 4.63

2. Chilcott Sites; pithouses, early type surface rooms, and brush
shelters:

%
Snowlakerblack-on=VVnites ae eee eee 19.39
Réserve Black-on=Wihite sito. cen ertion) ecient ie oe 4.11
dtularosasBlack-on-Whiterrs- eee eee eee 225
Kiatuthlanna Black-on-Wihites. .2e)) 45 see eee eee 1.61

Out of total of 2602 sherds, 6 were Wingate Black-on-Red.

3. Thode Site; ‘‘incipient pueblo”’; surface rooms with masonry walls
and sub-surface floors, each room close to another but not contiguous:

O7.

/0
Snowllake: Black-on=VWihiten. ce © ie ee eee 23.00
(TularosaBlack-on=Wihites).. 33), eee ee eee 4.18
Reserve Black-on=White.... 602s eee 2.61

Out of total of 765 sherds, 3 were Wingate Black-on-Red.

4. Rim Valley Pueblo; small pueblo consisting of two units, each of
one story, totaling about 25 rooms. No kiva was located. Built near
rim of canyon of Little Colorado River:

%
Red: Mesa: Black-on-Wihites S30 ee hte ee ee oe ee 7.59
Snowtlake/Black-on-=Wihiten eo fs fe ee 6.03
‘Tularosa: Black-on=Wihitee) 2.3..tes ae ee ee ee 4.62
Wingate Black-on=Nediianace ice cei serie rare 2:29

Out of total of 2,188 sherds, 3 were Houck Polychrome and 2 were
St. Johns Polychrome.

5. Great Kiva, Hooper Ranch Pueblo (for description of architec-
tural and ceramic details of pueblo, see Martin, Rinaldo and Long-
acre, 1961).

POTTERY

07
/O
iewlarosa: Black-on-WVinite roars cr > heats et. ct cl oe wis a shee 11.00
Mranipete IAB e OMG EG OU sac hsin akc eed pwd See pes 6.77
ips POlmirnea es 2)2 om aden Sa ts sss view oe os LORE 343
Heshota-utblavbolychrome = 4. 5 2:24 saewae ales oie « 2.08
Hours VitlesPolyehrame cin s. sex @ tei aay fe ene ata tee § 2.02
Kawakinasbolyenromen a din ayte Gis en a,3 OGIO an icc 1.88
Taste 1.—TOTALS OF SHERDS, GOESLING SITE
No. %
Decorated Wares
Kiatuthlanna Black-on-White........................... 231 4.63
Ween eda Idee OR-VV DINE: oo oe i i lm he ede ens 1364 27.35
Mite Mound Black-on-Whites.....- 9h sass ance ae 10 .20
Rami BidcR-ON- Wed o,f oh a eos be eee we eS ee 1 .02
Indeterminate Black-on-White.: 2.5.2... .222----c:s+ Bye) ilalteitl
Hotalfor Decorated Waressoe o.com uci oe ee eee 2185 43.81
Textured Wares
ree plats corrupted (52 oom ese os oon ood wei Pei ns, aad 2 04
Browusndented corvuvated: oa 66% «sca ndae ene ee eee 3 .06
Gray. plat COLL PALE” a oyepeconedsi 2.5 eve aie) 6 ap cele we aed Bre wih Bape 185 Shih
iSraveindented COnmupatedia ss) sreile csr c eet ee eee 110 PPA
Gray corrugated, wavy or exuberant..................... 61 E22
INTAG IRE CONC ALC wae cient ea eh Fe ah cee sashes a) ole sub Shh Goines 28 56
SAN A-ha Vs eee ree eer ene eke Ash onthe tee ro, dochaysinasleke 460 9.22
needs CORmMIp Ate Ge 1.6): cee SPp eisai edi terecicrs) 5 va Bie) ans Sec ah eee 11 ae
IRERSELVE COMMU P ALCO. Crete cic. s irae Ha. eeetbar teks TAB Re acaemE 2 04
Cray cormirdted: DOtLOMIS hia) oem asco entities kus Selous 155508 Sies
WotalitorelexturedVWViaKress in. vim fee ow adore nee wets 2417 48.46
Plain Wares
J AVPTE VAL Eo. otweiies WCRSRRNG sin Rich Oki ete aie eats ean Pe 120 2.41
UG Teta MELE se as a ie AOE 84 ens te Oat eat a ee eee eI eRe 43 .86
ONO MERI og 69 gc chan 5 Sheet ef Ee vie Soe De ee 145 2.91
San Francisco Red, Smudged Interior.................... 1 02
Titel) DA Ca Tap Soy aes cle c sr payee AY Ee RD Dea wT 1.54
NOtAMOlmeLAlteVVAUES ene i eit an heh ek adie ¢ ns tes 386 7.74

RAITT IRIE nen rye 515 iG ck kee AA pe Skee ee 4988 100.01

PREHISTORY OF EASTERN ARIZONA, I

Taste 2.—TOTALS OF SHERDS, CHILCOTT SITES

Decorated Wares

Kiatuthlanna Black-on-=VVibites se eee ere eerie:
Red¢Mesa Black-on-Whtter 2... = Sate ccs ee ee eee ee
Reserve Black-on=Wihite. . 2c sos oe ete ee een ee
Snowllake’ Black-on-White® << 2 ~ cine ee ees erste ete
‘iularosa, Black=-on=Whiter. .2oor Ge Lee ee Ca eee ee
Wingate Black-on-Redivu: 22% sja%s cee Wie ieee eee es oi
Indeterminate: black-on-red.%. co Gs os ares eee Gee OD sD
Indeterminate black-on-white: «.- - 2.5.40 +00 ee eee eee

‘Rotalsfor- Decorated uyViares soe. oe eee eee eee

Textured Wares

Brown plain corrupatede.... 5 25) ss)-.ce eo fee ee eee

Brown plain corruga

tec. smudpedsintenor ss) oe eee

Brown indentedicormipatede sc ee ase nel ete eee

Brown indented corr

ugated, smudged anterior. 2.12 2) 4a es

(Grayap lai corrupateder oy tans seas are See eee = ee ee
(Grayandented comusatede era te er eek ne
(Grayapatterned:coumpatede amin.) ers eee eee oe ere
MeDonaldi@ornmucated indenteda. a5 or 4-6 eee eee
Patterned vorcusated 239 oon b ay vin Ge, oe rie ingen 2 apie, Seen
Ailarosa ve aNet Welt Oe Soe idee kar foe igs eee eee ee

Indeterminate.....

Indented corrugated, red slip interior and exterior.........

Indented corrugated
Brown indented corr

exterior, black-on-white interior.......
ugated, fugitive red paint interior......

‘TotaliiorRextureduWianesianan since eee Cee eee

Plain Wares
Alma Plaine 2) 7.5 2.
Forestdale Smudged
Reserve Smudged. .

SansPrancwscor eda ois he oh Oe ee eee

Woodruff Smudged.
Indeterminate.....

1277

Oo
i)

|
PNANNYeR

POTTERY

Taste 3.—TOTALS OF SHERDS, THODE SITE

No.
Decorated Wares
miatuthianna, Black-on-VW bite, «mies: ids isean oe.4 6 ee ee 16
VES envy tol ACK Olt VW MICE fee ao tap taley orescence wr et a 20
PAPI id ieee AIO VV Che ace Ses 2a nn byte ace Goa ete, MRS 176
Pars a sae -Oiti WNC x. ons dc gost onan Sx paki bat RS a OR Goa 32
Vt ae ARETE cS sieve Wie Saya ey are Cavs Ole 3
indeterminate |plack-on-wiiten 5 crscti ass) citi). aia Be 230
SGV UP ECERG LEE VV AEES sx pwel ocx et 45! po) os + Bee Maek at hee 477
Textured Wares
PARES GINA POR UtA DUIALE O Me w '5. 4". se sisice a teks we se ee ee eee «Os 15
Brown plain corrugated, smudged interior................ 1
BVOWivitd enLeGkCORnUGated. a cui acer yes ok n oar ale © cleo ge)
Brown indented corrugated, smudged interior............. 2
rity MACE COIDMRATEC Sia iced Haan bg Kee 8 ee mim FD 2
ATEe REC GCOGIU PALE Cet mye a ctonoy-3 ys reReKeiene oat anche tee) < orl ne 8
MGLStErTOMM Atel os Nera ees ees A ceva me ee ae ett ore 3
MoaraliformbexturedaWiaresin nay ytares Sevens ae sie pom ate ae 210
Plain Wares
PRUE Mek tetrs eam Wei es ia Stee ce meg wa be ss 51
Smee EINER GEE cA tl Oe wed ten oe Meee ee oe nae es as ee 2 4
NV ERIE TER eT cm se cl te ee Sb Wie ec nese wien ne Oe Oe 4
MIGLERELIIM ALE rae ate See ain ley ye cee tee no RS 20

PREHISTORY OF EASTERN ARIZONA,

Taste 4.—TOTALS OF SHERDS, RIM VALLEY

Decorated Wares

FigucksPolyGhrome se mo oe cree eer eee ne eee
Kratuthlanna Black-on-VWibite- +e oe oe eee
Red Mesa: Black-oneWhites =<: cas oe ee cee
Reserve) Black-on-W Hite: & <2. ss tees ee ee
Sex) ohns7Polychrome. cu tecc terion ee ae
Snowflake Black-on-Whites > 2. 2... s+ +s ade eee ek
Wnlarosatblack=-on=VVibites ot. cee eee ae eee
‘TularosayWhite-on-Reds okie. 22 ee ee ee
Wingate Dlack-on-R edi 5. ieee eae ne Oe ete
Indeterminate black-on-red.- 2 2): os ee ee eee

Textured Wares

Brown plaimcorupated ey.) oh cree ee ree ee eee
Brown plain corrugated, smudged interior................
Brownvindentedscormicated crear 2 ery ees eee
Brown indented corrugated, smudged interior.............
Gray indented corrumated aoe ct oie. Ae ee ee eee
Imeisedicormuratedttne a> cuspueil oto. aren ae eee
McDonaldeCorcugated Plaine. 6 eo ion ee ae ee
McDonald Corrugated indented. = 3c. pee pees cee ee
McDonald! CorrmeatedsPatterned’ 1157. ae oe ee
Patternedcorrupated <2) cere ee ee oe eee ee
Bunchedtcornmugated arcu oy... sav a Ce A ee ee
Mularosavtallet Rim 3: 2 esi. tae. eee ee ee
AONnedi corrugated’. (8. ey. ceva r ee ee eo, eee Lee eee ee
indeterminate: )oe <i. shee ee oe ee ee

Plain Wares

Abra vP lasts 59. )2.ccts bite Sata a oie ale amie ahs oN eee
Reserve Smudpedin. i. «ste pier ate ee ee
SanKrancisco Rede ie ce ce eee at vines Se eee
San Francisco. Red, Smudged Yuterior: >. 2.005.202 22-4 4.
Woodrth Smudredi= cee melee eee ee ee eee
Sricleteqaaniate ss Jcis aioli hohe Go ee eee hee Oe ee

PUEBLO

No. %
3 .14
6 PPea |
11 50
166 (Pew
2 .09
132 6.03
101 4.62
2 .09
50 2.29
8 Bs if
169 Tat
650 329.71
76 3.47
107 4.89
528 24.13
506 25-02
1 .05
3 14
6 .27
19 .87
10 -46
58 2.65
4 .18
5 .23
> .14
35 1.60

33 125
2 09

2 09

1 05
1355 6.17
4 18
177 8.09

POTTERY

Taste 5.—TOTALS OF SHERDS, GREAT KIVA,
HOOPER RANCH PUEBLO

No.
Decorated Wares

Pause Nilev Poly chromers.eacncwre cy.ieore ok eee 92
KGila PP OlVEnrOMiG ris mete ne ee aes es en a 11
Eleshota-uthlask Oly Gorome ware treo. ora eee ee ce o5
PREVA ge VACUO INNES oA Se ce ee aa x ee 10
Rowaktnagbolychromern. cto ce eee een ae 86
Koyatuthianna: Black-on- White. 5.:,¢-62 cic ee ae ee 3
Pinos Black-on- Gray. tae nt Sete Seen) oe eee ce 3
inedale BlACk-GNeNedn oes eer ern ee Semis enh sien oe i)
PiMmedaleyEOlyGHLOMle wey rane see eens ee ee WS)
PinnawaLGlaze-on-VWhiteter: eyelget nnd ak ie eos eeu 7
Pintawarblack-on-Red 05 <2). -.as tae su tive, eee oe 6
Pinnawasl Oly CATOMe=). te soyd ei cess es Ae See eee 1
Binnawarked-Ou=VViOitee a cic ere eoce ace ie A atte atten a 3
rerio sholvehronie se aata.s ioe. cca is ae aan ess ek Se ake 5
edi Mesa Black-on-W.initen ser cs. Geoscns ae ise a ee iS
RESeLve; DlaGCk=On=V VINE: cp eaec evar ht autiey Rees & eee oe = 12
Be ORs NITRATE Fie ok cas A a ee ee ee ae i we 143
puGwelowsblack-au=Ied ici. ace aa ten oats eas oe oe oe 3
snowllakevblaek-on-VWiiite: cys. 4 se tudes nei ee ee ee 15
BPUMeeeVine A GLYCHIGEME : sic cc fcc w Ycin RR ee oe els wed Be 11
luslarosa Black-Gn-VWilitel. 26.) nee One nae oe ae Lh ee 502
Winn aie rie OiReN otis: Sats adie ane nee es Las 309
indeterminate: black-on-red)..c aa ee ee 288
indeterminate bDlack-ou-whites..)r-as te a eee nee 178
PcErerminate wiite-On-Led yet ea err ie ee oe 6
Indeterminate polycnnomen na. ashes ay eee) ai ee a 31
Motal torDecorated Wares: 9 ciao es Geese 1925

Textured Wares

UTS Ae GT Ga ile gpa Be Beal eb Delo eet ly See GN Eee 2
Ort M Ah COTEMEALE rc ices eee as we ok 676
Brown plain corrugated, smudged interior................ 172
BLOWHIMOENLCCCOLUMP ALEK a aie enter sone cians ote cies ora ied es 786
Brown indented corrugated, smudged interior............. 408
RUC ISE COLIN PALER itt a isteach a Aarons une ols 22
McDonald Corrugated Madented . 0... 66g. os sc cee des 13
RMeDaraid Comugated Patterned oie dc ee eee eee ee 1
AT eLMeC COLUM Aten: Wie aie Mei tery ide Ours oes ala epee 91
PETES BS he ge 2 RR Poe oy a ee a ge ile
Pee E AI REE RING 5 oe Sn oo vin auth eck Cle nad <8 or ea eR me 4
PEO COVE MALEK a Steere aiken La eR ie 2 ees 4
Be ENN a iti Pye tus ie ok aa Bae ee eicaie Cae 4 xn nish yall 153

PREHISTORY OF EASTERN ARIZONA, I

TaBLE 5.—TOTALS OF SHERDS, GREAT KIVA,
HOOPER RANCH PUEBLO (continued)

Plain Wares

No.

AlmasPlain ye a eee bd cohol eae oye incon ee ee 142
Horestdale;Smmnd ped ys mee. earels o eusgera se er ae 12
IeYeL(E aiforey tel blelefo0 logis Aries Meic Meee Newer Ann awelse Soe 19
DA HELANCISCO URECiwer: ela yes ensea cup renee se nee Omer oie ee as 42
Sau) brancisco Red, smudred Interior... 245 anne ens I
Wioodriib smudgedh pac. wierac ccc, oe oererr ee aed oeetrrae 53
Irie Eterminate sah ae soe es clors crepe es ee ee 19
Burnished interior, brown ware; not smudged............. 1
Wotalhtor lami aresion vette te ie eine oe ele eee ey eres 295
Total for’Great Kiva) Hooper Ranch Pueblo... .... 2244-252 4564

IV. Statistical Analysis of Painted Pottery Types
from Upper Little Colorado Drainage

By LEsuiE G. FREEMAN, JR.

Research Assistant, Department of Anthropology
University of Chicago

INTRODUCTION

This study was designed to discover whether interpretations more
far-reaching than those yielded by our former methods of analysis could
be derived from the data at hand from our six sites, without incurring
prohibitive expenditures of time and money. The ideal tool for the
study had to be one which did not require the intervention of many
operations between the raw data as represented by our archaeological
collections and the conclusions which could be expected to result. For
this reason, a statistical study immediately suggested itself. The par-
ticular method chosen as best suited to the task and the data was
the Robinson-Brainerd seriation technique (Robinson, 1951; Brainerd,
£951).

Some criticism of the Robinson-Brainerd method was offered by
Lehmer (1951), when the technique was proposed. The Robinson-
Brainerd technique does not correct for differences in sample size, and
Lehmer proposed that this could be remedied by operating with mean
standard errors, instead of the original ‘‘coefficients of similarity.”’ Both
the original method as presented by Robinson (1951) and the revision
proposed by Lehmer have inherent advantages and disadvantages, which
I shall not attempt to evaluate. I have chosen to use the method as
originally presented, since Lehmer’s method requires random sampling,
or at least a definition of the universe from which the samples are drawn.
Our data do not meet these requirements, so the use of parametric
statistics in their analysis cannot be justified. In addition, the calculations
involved in the original Robinson-Brainerd technique are simpler than
those proposed by Lehmer, and the rationale behind the operations
is easier for the non-statistician to follow.

88 PREHISTORY OF EASTERN ARIZONA, I

CHOICE OF MATERIALS

It was determined that the materials which best fitted the Robinson-
Brainerd method were the painted wares. The types of painted pottery
represented in our collections are fairly numerous, and the types them-
selves are well enough fixed for the purposes of a seriation. Further,
individual types have a temporal existence so limited that one can ex-
pect some change in popularity of a given type over a fairly short time
period. Some types are well established as horizon markers, and one
can date their appearance and disappearance from an assemblage quite
well, so that they provide an internal check on the results of any sup-
posedly chronological ordering imposed upon them.

Limiting the analysis to painted wares had some drawbacks for I
was forced to use small samples in the seriations, but I felt that the ad-
vantages inherent in the consideration of painted wares alone out-
weighed the disadvantages of so doing. Had time permitted, it would
have been desirable to reseriate the materials, including some at least
of the available utility wares. Since this was not done, I have no idea
whether or not it would have yielded the same results, or better or worse
ones. It would certainly be worth while to undertake such a study in
the future.

SOME METHODOLOGICAL CONSIDERATIONS

The temporal sequence of the sites themselves could be closely approxi-
mated by inspection, but though the ends of the sequence were easily
recognizable, the relative temporal order of the Rhoton, Thode, and
Chilcott sites was not as evident. I hoped that the seriation would estab-
lish a finer chronological sequence than could be drawn by eye, and that
once this sequence had been established our attention would be drawn
to other factors causing differences between samples. Ideally, if the
seriation of a number of samples is correct, any abrupt discontinuity
in the materials of one sample compared to the rest, if it is inexplicable
by considerations of stylistic change in a single tradition over time,
can be due to other factors. Some of these factors are known. The
intrusion of a tradition foreign to the area concerned is one. The looting
of abandoned sites by culturally dissimilar groups, for example, to pro-
cure potsherds for tempering materials, is another. The preservation of
obsolete materials as heirlooms, and the mere collection of curiosities
_ have also been suggested (Martin and Rinaldo, 1960b, pp. 206-208).
While realizing that all the possible factors are not yet known, I hoped
that once temporal considerations are controlled, the nature of some
such discontinuities would point out one or more possibilities as the
more likely causal factor.

STATISTICAL ANALYSIS OF PAINTED POTTERY 89

My main interest, then, lay first, in establishing the relative chrono-
logical order of the sites; second, in establishing the relative chronological
order of the rooms within each site. Therefore, I seriated not only the
sites, but the floor materials from each site. Each seriation yielded a
probable temporal order of materials, but to determine which end of
the sequence was late and which early, the seriation had to include some
samples whose relative chronological position was known. Where it
was possible, collections from superimposed floors were used, but often
I had to include material from a floor and the fill above it to get direction
from the seriation. I tried to avoid using fill samples, since they might
have accumulated over long periods of time and for that reason might
have proven difficult to fit into the seriation. Collections from fills were
purposely used in cases where the number of floor samples was so small
that the trends in pottery popularity through time based on floor materials
alone would have appeared meaningless.

My lower working limit of size of sample in this study was 23 sherds.
Besides the fact that sample size was limited when I restricted consider-
ation to painted wares, large samples often had to be ignored because
they behaved as mixed samples in the seriation. In some cases, this may
have been due to the continued occupation of a floor throughout the
time period represented by the rest of the samples, so that materials from
every period were represented in the floor in anomalous proportions.
Also, my desire to consider as much floor material as possible often
caused me to accept small samples, as the excavated material from
floors included fewer sherds than that from fills. Since the samples were
so small, I feel that the results of the seriations alone should not be used
as anything other than possible corroborating evidence for interpretations
drawn from other data, and clues to further investigation. The seriations
in themselves do not warrant even the statement of probability of correct-
ness usually made in statistical studies.

The conclusions drawn in this study refer primarily to the seriated
materials. The study would be of little value, however, if the results
of the seriation had no reference except to the seriated materials. We
must assume that the painted ware samples from floors, at least, are
part of pottery assemblages which are correlated with assemblages of
other cultural materials. We assume, then, that inferences drawn from
the painted ware samples hold generally true for the occupations they
represent. The same assumption cannot be made about fill materials.
They may, of course, represent more than one occupation. However,
the chronological position of these occupations will be that of the mixed
painted ware collection representing them. Still, one cannot extend

90 PREHISTORY OF EASTERN ARIZONA, I

the inferences drawn from the seriated materials to statements about
the occupation of the sites as a whole; they are directly applicable only
to the structures and areas excavated.

Before proceeding to the actual seriation, I made use of a method
which was first developed by Arthur J. Jelinek (1960) for indicating
graphically the relative positions of the samples. This method consists
in the construction of a ‘“‘map”’ on which the relative similarity among
the samples is indicated by their position and the nature of the lines
joining them (fig. 46). The location of the samples and the nature of
their connections are determined by the respective sizes of the Robinson-
Brainerd coefficient of similarity between any two samples. The maps
allow one to see at a glance the inter-relationships among samples, and
are amenable to both temporal and non-temporal interpretation. With-
out this method my task would have been materially more difficult. I
relied on it to yield a first approximation to the seriations. (See Martin,
Rinaldo, Longacre and Freeman, 1961, for analysis of sherds on which
seriations are based.)

BASIC PROCEDURE

The percentage of each type of painted pottery in each sample was
calculated. Only sherds which could be definitely classified were used
in this calculation. Each sample was then compared with every other
sample. The differences in percentage of each type between the two
samples were added, giving a total difference between the two samples.
Now the maximum possible difference between two samples is 200. Two
samples would be this different if 100 per cent of the pottery in sample
1 were of different types than 100 per cent of the pottery in sample 2.
The calculated total difference was subtracted from the maximum possible
difference to give the coefficient of similarity.

The coefficients of similarity were then placed in a symmetrical
matrix. In this matrix, the diagonals, left blank, are relationships of
identity, so that the blanks represent coefficients of 200 (the maximum
similarity). The ideal arrangement of samples in this matrix shows the
highest coefficients on the diagonal, and decreasing coefficients to the
upper right and lower left corners. This ideal was approached as closely
as possible.

The temporal direction of the inter-site seriation was determined
by the presence or absence of early and late painted ware types in the
end samples. The direction of the intra-site seriations was determined
by the positions of one or more floor samples relative to their respective
fill samples, or by the relative positions of superimposed floors from
the same room. Lastly, graphs of the popularity of each pottery type

63
Key

Coefficient of Similarity

(d)
180 - 199
170 —179 Sennen
160 -169

¢Rim Valley

Thode SC Chilcott

e Rhoton

¢ Goesling

Key to (b),(c), & (d)

Symbol Coefficient of Similarity

170) = ASI.
Iso — 169
150' = 159

140 - 149

1 = Floor $ = Below Floor A= Fill K=Kiva
KiL1 = Kiva 1, Floor 1 5At1= Room 5A, Below Floor |}

Fic. 46. Schematic illustration of the relative similarity between samples of pot-
tery.

(a) Chilcott sites; (6) Rim Valley Pueblo; (c) Hooper Ranch Pueblo; and
(d) site totals.

100

Red Mesa Black on White
90

Kiatuthlanna Black on White
20

White Mound Black on White

Al2 Atl All A Trench
Sample

1=Floor {= Below Floor
Al2=RoomA, Floor 2
A Trench = Trench through room A

Fic. 47. Percentages of three pottery types by levels at the Goesling Site.

STATISTICAL ANALYSIS OF PAINTED POTTERY 93

based on the percentage of each type in the total painted ware assemblage
in each sample were constructed, so that the fluctuations in popularity
of each type through time could be observed.

THE INTER-SITE SERIATION

The map shows the relationships of the site samples (fig. 46, d).
Sample sizes and the final seriation matrix for this ordering appear below.

TaB_e 6.—SAMPLE SIZE OF SHERDS AND FINAL MATRIX
FOR INTER-SITE SERIATION

Sample Size Number
of
Site sherds

WRG an as a Cia a et a Mg cana coe amino 1587
SEENON LGN ees terse ote cht We oer ee nee een cream et eye nak tence 41
REM BE iar. 1-6 cone pe eg OEE ERT oh LO es bE ay 695
in (oYe Coe aaets take cis Speer tcl ETRE: Coo Ca ane ee ee 233
sPevaaTat WAU spi 9 Sic See RCO aie ere sa et cna ea Men ta cote etree re we oe 418
Heed OIE Ne neeeg er eter el Neran fee Meat cot eee RSA GIT eC ds oo eo 4998

Final Matrix
Goesling Rhoton Chilcott Thode Rim Valley Hooper

Goesling.... 2... = 24 15 12 5 oi
Riboton..256)¢ 24 = 167 165 84 17
PO ds» a 15 167 — 183 108 20
PEEING) as Ge eas 12 165 183 = 105 49
Rim Valley.... 5 84 108 105 = 7
PAGOVER: S50 x x < : y 17 20 49 Tl =

Due to the appearance of late pottery types at the Hooper Ranch,
the order is from Goesling (early) to Hooper (late).

INTERPRETATION

The Goesling Ranch Site and the Hooper Ranch Site are at opposite
ends of the seriational scale, and both show little similarity in painted
ware collection to the rest of the sites or to each other. The Chilcott
Ranch Site and the Rhoton and Thode Ranch Sites show much more
similarity among themselves than any of them shows to any other site.
We seem to have an early site, Goesling, separated widely in time and
cultural affiliations from a group of three sites, Rhoton, Chilcott, and
Thode. Separated from them by relatively great divergences in sherd
collection is the Rim Valley Site, which, however, resembles them more
than it does Hooper. This is the more striking since the geographic

94 PREHISTORY OF EASTERN ARIZONA, I

distance from the Hooper Ranch Site to the Rim Valley Site is very
short, and one might have expected that the Rim Valley Site and Hooper
Ranch Site could have been occupied coterminously by people with
much the same cultural apparatus. How much such differences are due
to non-random representation of the total settlement at each site in
the excavated material is impossible to determine, but the gap exists
between the excavated portions of the two settlements.

THE INTRA-SITE SERIATIONS

The Goesling Site.—This site was not seriated internally, as only three
unmixed samples were available and all three were from Room 1A:
material from Floor 2, a collection of sherds from the fill between
Floors 2 and 1, and the later material from Floor 1 itself. The percentages
of each of the three major types of painted ware are shown in figure 47;
one type, Wingate Black-on-Red, was excluded, since it is represented
by only one sherd, which was found in a mixed collection from Room A,
level 2, including both floor and fill material. Of the remaining three
pottery types, Red Mesa Black-on-White forms early a large percentage
of the total assemblage of painted wares and this percentage declines
somewhat in time. Kiatuthlanna Black-on-White makes up only 7 per
cent of the total painted ware assemblage on Floor 2, increasing to 16
per cent on Floor 1. White Mound Black-on-White constitutes an al-
most negligible percentage of the assemblage throughout time (less than
1 pervcent).

TABLE 7.—SAMPLE SIZE OF SHERDS FROM GOESLING SITE

Number
of
Room sherds
AN AEMGOT Dir ecstasy stays che Ae dere tone uk aR Te A ee 307
A: belowsBloor Des 42 eee), Ae oe ea eo ee 466
AS IGG Be coos eh oh Sat RS suey er Benes oe ees 233
Trench through: Room Ay 604+ ss 4 sly be Stem ma eet ee a pute ee 454

(Floor 1 is the upper floor)

The Goesling Site is relatively homogeneous, but it must be remem-
bered that only two floors in one room are represented in the Goesling
samples, and the materials represent a single, short cultural horizon.

The Rhoton and Thode Sites——Material from these two sites was not
amenable to seriation, except in the inter-site comparisons. It is largely
surface and fill materials, which could not be ordered well, alone. The
Thode Ranch Site materials are all from room fills, with no large samples

STATISTICAL ANALYSIS OF PAINTED POTTERY 25

from floors and thus do not possess the internal stratigraphic relationships
necessary to determine the direction of the seriation.

The Chilcott Site—This is actually three sites. Since Site 3 and Site 2
show a much greater degree of similarity in painted ware assemblage
than either does to Site 1, it was determined to treat Sites 3 and 2 as
units, mixed though they are, in the seriation of the materials from Site 1.

In Site 1, the only definitely unmixed sample is that of Room 6,
below the floor. However, since it was felt that graphs of pottery popu-
larity were desirable for the Chilcott Site, fills from both Room 6 and
all other rooms were seriated. The results and sample size are shown below.

TasLe 8.—SAMPLE SIZE OF SHERDS FROM CHILCOTT SITE
AND FINAL MATRIX

Sample Size Number
of

Room sherds
GaNElOWAHOOL Set oii rie te ee ein aes Lee 49
Gis ll ee RE ae PA oie te Ae OM nen ekg or an DTC Cer ENe caer 35
AOE) Meee Bh tea a Ear ALIN hg seas MCG a atloy es sity Diol wp acae. eee ota 119
Hr dTLicmreeeaetoe: , Mme cre Rots tame aes ieteae Se te oa Me ete Pate wee 55
Dhalilionety. sea avin amet tet. tame ee Re rok ito ME ode aunt Ay, 2 214
AeA eae Ae ye pe con RE ee ee PU A ane cide th a, eae Bee 103
2580 THN Goer Peete, NORE SE Me aah Re ee tani ec Re ee Ea ie Pe Ree RR Ree Ce 25
Stat an ee LIN e te ade, haa ate tre Nes PR Re Es Geb ae oo 29
Syren es +e Wms ates op Tere tene cote Detter hy ORAL ee ae ene roars eh

ROOM. sho « 6 5 1 6 2. 4 3 Site Site
below
floor fill fill fill fill fill fill 3 2
6, below
fiSOr'...: « - 169 153 134 133 122 122 110 104
Bettie ee 169 - 184 161 159 145 1152 134 130
hase ae get bs 153 184 - 177 175 161 156 138 135
(9 Ue ae 134 161 WAT, ~ 190 179 171 159 150
a TD ais ees 133 159 7s, 190 180 169 154 150

- 161 163 148
Dy tll shies 122 152 156 171 169 161 = 181 178
RPS ie sien 110 134 138 159 154 163 181 = 178
BUGS vers. 104 130 135 150 150 148 178 178 =

It will be noted that there is a high degree of similarity between
each sample and the samples immediately adjacent to it. The excavated
areas represented in the seriation seem to show a rather uniform direction
of change in painted ware assemblage, which one would expect, if a
single cultural group had occupied the three sites during the time period
here represented. The uniformity of change, it must be remembered,

96 PREHISTORY OF EASTERN ARIZONA, I

may be non-temporal, and a function solely of the representation of
the assemblages we have from the excavation. It is, however, hard to
see why any other factor beyond temporal change need be called upon
to explain the seriation results. Further, the fact that this uniformity
is shown on the pottery graphs, with all types changing in quite regular
fashion, adds weight to the significance of the results and makes it less
likely that they are purely accidental.

The position of the materials from Room 6, below the floor, and
the fill in Room 6 in the seriation make it reasonable to assume that
the materials below the floor in Room 6 are early, and those in the fill
of Room 3 are late in Site 1. The seriation also places materials from Site
3 and Site 2 as later than any from Site 1 and justifies the conclusion that
Site 2 is later than Site 3. We also note that all the excavated rooms
on Site 1 had filled or been filled before the materials from Sites 3 and
2 accumulated. Since the collections from Sites 3 and 2 are all fill or
surface materials it is possible that late Site 1 and Site 3 were occupied
contemporaneously.

Figure 48, a and 6, shows the percentage of each type of painted
ware in the total painted ware assemblage in each sample. The per-
centage of Wingate Black-on-Red has been omitted, since it occurs
sporadically, late, and in very small quantities (only 4 sherds on the
whole site). The graph shows the increase of Snowflake Black-on-White
from 46 per cent to 90 per cent, the decrease over time of Reserve Black-
on-White from 44 per cent to only 2 per cent, and the appearance of
Kiatuthlanna Black-on-White, its climb in popularity to 11 per cent
of the total late in Site 1, and its absence from Sites 3 and 2. Tularosa
Black-on-White is present in small proportions of the total assemblage
throughout the sites. The presence of Kiatuthlanna Black-on-White here
is problematical. It is chronologically out of place. Arguments that
it appears due to the discovery of an abandoned site, whence it was
brought to the Chilcott Site to serve as tempering material, seem to
me unconvincing. If sherd temper were being used, enough broken
local material should have been available for use by the time Kiatuthlanna
Black-on-White appears on the site. Furthermore, one would expect
that the curve for Kiatuthlanna Black-on-White would not show the
gradual increase that it does, but rather either a fairly uniform percentage
_ or a random increase and decrease, if for some reason it were a popular
tempering material and constantly available. I would be able to reconcile
an isolated peak or two on the graph with the discovery of small quan-
tities of Kiatuthlanna Black-on-White by one or two fortunate Chilcott
residents, but it seems to me that an explanation of the present curve

100 100

%o %
90 90 ae
— Red Mesa Bicck on White ——
80 80 /
—-— Tularosa Black on White /
70 70 os As
—-—-— Kiatuthlanna Black on oe =
60 White 60 par
/
50+7 —-—-— Snowflake Black on White
40 — Reserve Black on White

GN on. IA OA 2A Os Sa 1S3. S2
Sample

(b)

100 100

%o %

90 —— Red Mesa Black on White 90 —-— Reserve Black on White

80 —-— Tularosa Black on White 80 —— Wingate Black on Red

70 —-— Kiatuthlanna Black on 70 ——-— Snowflake Black on
White White

AIeGL <GAYBE~AA “BAe. Fish AUG CX Bibs Ay BASEL “ne
Sample Sample
(c) (d)
S=Site L= Floor += Below Floor A=Fill Material
64= Room 6, Below Floor Ba= Room B, Fill S3=Site 3

Fic. 48. ‘Trends in painted pottery types illustrated by samples from Chilcott
Sites (2 and 6) and Rim Valley Pueblo (c and d).

98 PREHISTORY OF EASTERN ARIZONA, I

on that basis requires too many hypothetical conditions. There remain
a number of possibilities, among which one must mention the heirloom
hypothesis, and the possibility of the long-continued manufacture of
this pottery type by an individual or group, perhaps a clan. These sug-
gestions are highly speculative, and if this were the only site where
Kiatuthlanna appeared in an anomalous setting, I should be inclined
to discard them all, or accept the first over the other two.

The Rim Valley Pueblo.—Neither the Rim Valley Pueblo nor the
Hooper Ranch Pueblo materials yielded a particularly satisfactory seri-
ation. Figure 46, 6, shows the mapped interrelationships among the
Rim Valley samples. The seriation was based on 8 samples. The sample
size and final seriation matrix are shown below.

TaBLeE 9.—SAMPLE SIZE OF SHERDS FROM RIM VALLEY PUEBLO
AND FINAL MATRIX

Sample Size Number
of
Room sherds

AS HOO a 2 ce fee ais is poms BOM a en ee Pe Oe eee 25
(ORR 3 (070) cae a ee at een, ee A et oa ers eter uate > 26
CAE. RE ee ede ya are ae Pec ree ee eee 1B:
Bs HOOP: fk es chs es oes Aas sade Pa eee aE RLS a ee 70
Neg 11 OA ee eee ee Re See Ae Ar eee er ee aa ee 45
Breil Ceres Merete ee brn teas sac ae ae ae eC oo Oe ne te 29
Ds HOOT: Seth a keto ie ae oho hend, SSeS her ra eG eR OT «ee ee ore 30
FAS HloOr.... Somtateon shoals Qiceaeve Mos he Pa eRe ee ee ee eee 50

Final Matrix

ROOM 2A eee ue A G CG B A B F H
floor floor fill floor fill fill floor floor
Ae HOOTH Gs ates hee - 134 140 111 100 76 61 112
Coors see ce LS: - 174 174 143 129 5 gh 119
Cl ofl 2 ies eee ee IAD 174 - 164 154 129 111 99
ibs floors) occ. ee eel 174 164 - 140 132 120 98
AMA eric oan ee 100 143 154 140 - 174 153 97
Beil 6 ee ee 76 129 129 132 174 — 149 86
POO) aba 61 117 111 120 153 149 - 118
He floor usa cheats nll 119 99 98 97 86 118 -

As can be seen, the sample from Room H, floor is more similar in
the assemblage of painted wares to samples at the ends of the represented
_ time range than it is to any of the middle material. This may be because
it is a “mixed sample.’ This would be the case if H, floor had been
occupied throughout the time period represented, and if, in addition,
more pottery had been broken and trampled into the floor during both
early and late times than during the middle period.

STATISTICAL ANALYSIS OF PAINTED POTTERY 99

As can be seen from figure 46, 5, where the relationships between
the samples are presented graphically, all but H, floor are related in
a more or less linear temporal manner, but H, floor is a “flyer,” and
the reasons for its differences from the other samples must be due to
something other than chronologically based change in an isolated cultural
assemblage, if the seriation is correct. However, the samples are so
small that speculation on this point based on the seriation alone may
lead to fallacious conclusions. It is worth mentioning that if more than
one sample like H, floor had been included in the seriation, seriating
the data would have been well-nigh impossible.

Figure 48, c, d, shows the increase of Kiatuthlanna and Tularosa
Black-on-White through time, the decline of Reserve Black-on-White
from a large percentage of the total painted ware assemblage (neglecting
H, floor), and the increase and subsequent decline of Snowflake Black-
on-White and, to a lesser extent, Wingate Black-on-Red. It is interesting
that the direction of change in popularity is diametrically opposed between
Snowflake and Wingate, at least until the sample from F, floor is reached.
I am tempted to speculate on very tenuous grounds again. If at least
two clans occupied this site during the represented time range, and
if they differed in the manufacture of pottery so that one clan made a
higher percentage of Snowflake Black-on-White in proportion to Wingate
Black-on-Red than the others, then perhaps alternating clan dominance
would account for the appearance of this curve.

The sample from H, floor, as expected, behaves anomalously, the
percentage of Reserve Black-on-White in particular being very high.
Once again, Kiatuthlanna Black-on-White is present in a late setting.

The Hooper Ranch Pueblo.—This site afforded the most dubious seriation
of any constructed with these materials. As can be seen from figure 46, c,
the positions of samples in relation to one another scatter widely. Three
samples, Kiva 3, floor, 5B, floor, and 3A, floor 2, bear little resemblance
to the other samples, and little to each other. There is not a single pottery
type in common between 3A, floor 2 and 5B, floor. As mentioned earlier,
without the aid of the graphic presentation afforded by Chart 2 there
would have been no indication of which sample should start the seriation,
or in what direction it would proceed. Even the chart does not show
the discrepancies between 3A, floor 2 and 5B, floor, and between them
and the rest of the samples as well, as both the aforementioned samples
actually cannot be placed on the chart. They have only been so placed
for ease in comprehending the overall picture.

The seriation itself was based on 11 samples. Sample size and the
final seriation matrix are shown below.

100 PREHISTORY OF EASTERN ARIZONA, I

Tas_e 10.—SAMPLE SIZE OF SHERDS FROM HOOPER RANCH
PUEBLO AND FINAL MATRIX

Sample Size pes
oO

Room sherds
BA MOOV Diva coo ate tre Se Ca IEE ane, ee eT car a ee ens 27
1 OAS SH OOR2 hin ko hoe nhs Siete eee CR I ne ee aa 64
AAT HOOK is fst "dood S sdycte sere RAS, CRIT Pee o> ohh MMs pee AE ea taeca e 584
SAC below hoor Leys «eee vio oe cae eh ear cee cen ee eee 3M)
DASE GOL, races ste eqorstaccrcierere Sree TONE eT eRe CE ee neg 38
DA SHOORM TPs iit. Sid. ated LE Le RA Cas OE iS ete ne eee mR 30
NI DAN MOOT: carteye a +s PRO RA OREO oe oe Ta ce ee 28
civ doors Tite, eeetoeee pone tens Mere ee ore Peete ieee ee ee a 113
ST Vah SAH OOR? Veeco Ne hee den eater ee preaiclees rents em meee ae 515
ovat KOO) Gs, een ee ee RE eeE Te eR, Senn) S Cio ead eee erate 43
£)) B59 6 COTO) cea baat pil eRe Shan ore! Ae Nat we Ms eh ene aad. bien i ee OE 2 es 83

Final Matrix

Room see eels ZAY 1OAy 4Ay SA 9A 9A 112A) Kiva Kiva (GAs
floor floor floor below floor floor floor 1 3 floor floor
2 2 Dee OOT: a2 1 floor1 floor
SAG HOOr 2a. 44a co.. - Be eo tA?) CAD) Oe AA 47 Sy eon 0
OAS Moore cease. ihe = ile 98 83 112 114 86 106 96 48
AAW LOOT nis aiiea eh oe By Ale — eS 2 eel OS een ee
SAN belowloor 1a. 42 98 SL Re 345 328128) i See
DACHOOT Wt. sis ae AD) + 83h Wi A173) © 143 1361345 OS h D4 eee
OA HOOTe aera c eva fe 87 At?” W210 145) 1437 = 1445 136 onl O eee
IDASHoorssse. sce | 44 4 Sy 182 S68 144 GS) 135 4s
Keivaels loons mceiya e AD 86) SA Oet289 DSA 1366S — 29a Ome
Keivaes HOO eer 37 LOG) SOS 397 9 0S GG: SiS Si 20 — eS
SAMHOOr ase) saree. ol = Ome OS a O50 O4e 20a 4 se wO se oe 49
5SBetloorres anes OMIEAST GAD 2 ies ol 260. 3379939) 53250

The direction of the seriation is probably from 3A, floor 2 (early)
to 5B, floor (late), as shown by the relative positions of floor 2 and floor 1,
Room 9A. It would not be wise to base any conclusions on the results
of this seriation alone. Figure 49, a-d, shows the percentage of the total
decorated ware sample constituted by each of the major types represented
in the sample. The anomalous character of the samples of 3A, floor 2
and 5B, floor can be seen well. There is a seeming similarity between
the assemblage of 3A, floor 2, at the Hooper Ranch, and that of H,
floor, at the Rim Valley site (fig. 48, c, d). On this very tenuous basis
the suggestion is ventured that there may be some sort of cultural similarity
between the late settlers at Rim Valley and the early ones at the Hooper
Ranch, and that the settlers of both sites during this common period of
occupation, if such it be, belong to a tradition divorced from that of the
main settlement at either site. Still, it is best to remember that the data
here presented are insufficient to warrant these speculations. Attention
is also called to the fact that two sherds of Kiatuthlanna Black-on-White

100 — Tularosa Black on White Tele)

% fo — Reserve Black on White
90 —-— Pinedale Polychrome 30

--— Querino Polychrome —-- Red Mesa Black on White

—-— Snowflake Black onWhite

JOAL2 SAt 9A1LI KIL1 BAL 1OAL2 SAt 9A1L1 Kil BAL
Sample Sample
(a) (b)
100 100
So %o
90 — St. Johns Polychrome 90 — Wingate Black on Red
80 --- Kwakina Polychrome 80 —--— Heshotauthla Polychrome
70 Pinedale Black on Red 70 —-— Springerville Black on White
60 60
50 50
40 40
30 ee
20 20L
A

Oo Jeg ie a3 = Oo
ZAL2 | 4AL2 | SAL2 12AL 5BL 3AL2 | 4AL2 | 9AL2 12AL 5BL
1OAL2 5SAt 9A1I Ki! BAL 10A1L2 5At SALI Kill BAL
Sample Sample
(c) (d)
1 = Floor += Below Floor K = Kiva
ZA12 = Room 3A, Floor2 KiL1= Kival, Floor 1

Fic. 49. Trends in painted pottery types illustrated by samples from Hooper
Ranch Pueblo.

101

102 PREHISTORY OF EASTERN ARIZONA, I

(not shown on the graph) were found on Kiva 1 floor, and two on Kiva 3
floor. This may be accidental, but it also suggests an earlier provenience
for the materials in those samples than is indicated in the seriation.

Evidently Tularosa Black-on-White was the dominant ware at the
Hooper Ranch Site, and it seems to have increased in popularity until
the terminal occupation of Room 9, floor 2; then it decreased. Wingate
Black-on-Red has a late “‘vogue”’ and then decreases, being at its highest
peak of popularity earlier than Heshota-uthla Polychrome, which does
not reach its peak until we reach the material from the floor of Room 8A.
Both types have disappeared from the floor of Room 5B. Room 5B
is an anomaly, much different in cultural content from the rest of the
rooms. In it, St. Johns Polychrome has taken the dominant position
held by Tularosa Black-on-White in the rest of the excavated materials.
Room 5B, floor gives the appearance of being a mixed sample, if the
rest of the seriated materials are in their proper place. The “‘pottery
popularity’> curves make it seem more probable that the seriation is
not entirely correct, as their fluctuations have less the appearance of
normal curves than is the case on the other sites.

CONCLUSIONS

(A) The site materials studied in this section seem to fall into three
distinct groups, each with some temporal duration, to which I shall refer
as periods 1 through 3. The earliest period seems to be that represented
by the materials from the Goesling Site. This period is characterized,
in the seriated material, by 80-92 per cent of Red Mesa Black-on-White,
from 7-19 per cent of Kiatuthlanna Black-on-White, and a trace of
White Mound Black-on-White.

Period 2, represented by the materials from Rhoton, Chilcott, and
Thode, is much different in painted ware assemblage from the first.
At Chilcott, Snowflake Black-on-White has appeared and dominates the
painted wares, becoming more popular while Reserve Black-on-White
becomes less popular, until at last Snowflake Black-on-White makes up
90 per cent of all the painted wares. Tularosa is ever present, but only
from 2 to 9 per cent of the total painted wares. Kiatuthlanna Black-on-
White appears early, climbs to 11 per cent and then disappears. Red
Mesa Black-on-White constitutes a small but increasing percentage (to
6 per cent of total painted wares) until the end of our represented period.

Though Rim Valley is different from the earlier sites, it bears some
remarkable similarities to the Chilcott Site. The earlier portion of the
Rim Valley Site shows a quite similar increase of Snowflake and decrease

STATISTICAL ANALYSIS OF PAINTED POTTERY 103

of Reserve, though Snowflake does not seem to have attained the popu-
larity at Rim Valley that it had at Chilcott. The outstanding differences
in the excavated collections from the Rim Valley and Chilcott sites seem
to be three in number. First, Tularosa Black-on-White makes up a high
percentage of the painted wares of Rim Valley quite ‘‘early,” and con-
tinues to increase in popularity through time. Second, there is between
5 and 20 per cent of Wingate Black-on-Red until quite “late”? at Rim
Valley. Third, the late portion of the seriated materials from Rim Valley
shows the decline in popularity of Snowflake Black-on-White ware. Rim
Valley seems to me assignable in part to Period 2, in part to Early Period 3,
both parts showing new cultural influences.

There may be a cultural stage temporally intermediate between Rim
Valley and Hooper, as mentioned in the discussion of the Hooper Ranch
seriation, and during which both Hooper and Rim Valley were occupied
at more or less the same time. However, the evidence for this, from the
floor of Room H at Rim Valley, and floor 2, Room 3A, at Hooper, is
dubious.

At the Hooper Ranch Site, which represents Period 3, the excavated
material is distinguished from the previous materials by the appearance
of late types of painted wares, among them Heshota-uthla Polychrome,
Pinedale Polychrome and Black-on-Red, and St. Johns Polychrome. Tula-
rosa Black-on-White increases in popularity until Room 9, floor 2, and
from then onward it declines. The presence of both early and late ma-
terials in the Hooper Ranch collections suggests that the duration of occu-
pation represented by the Hooper materials is a long one in comparison
with the materials from the other sites. The presence of Red Mesa in
this context seems strange.

I strongly question the fixing of Room 5B, floor as “‘late’’ at the
Hooper Ranch. Although the seriation ‘‘works” best with Room 5B,
floor in that position, the sample is so anomalous that were the sample
from Room 3A, floor 2 not included in the seriation, Room 5B, floor
would seriate equally well at either the late or the early end of the se-
quence. I am less inclined to doubt the early position of Room 3A,
floor 2, though there are good grounds for so doing. Chief among the
reasons it has been included is its resemblance to Room H, floor, at Rim

Valley.

If I had no more than the data included in this chaper, I should be
inclined to derive from them an initial cultural phase represented by
the Goesling Ranch Site; a ‘‘gap”’ in the cultural record; and a new phase
represented by the materials from Chilcott. The early portion of Rim
Valley would then seem to me to be a blend of the Chilcott and another

104 PREHISTORY OF EASTERN ARIZONA, I

phase, including an increasing amount of Tularosa Black-on-White and
the continuation of Wingate Black-on-Red in the painted ware assem-
blage. I should be tempted to see the further development of the Rim
Valley phase in the early materials at Hooper Ranch, and either the
development or adoption of a number of late painted wares there. After
the “abandonment” of Rim Valley, I should be tempted to postulate
the intrusion into the Rim Valley-Hooper area of a group of “‘foreigners”’
with a distinct material culture and their subsequent withdrawal or
amalgamation with natives of the area.

These speculations are, of course, not seriously offered as any kind of
culture-historical scheme for the area. I realize that most of them may
well prove totally erroneous, but their presentation may enable the vis-
ualization of further problems, or corroboration of results from other lines
of research.

(B) From the position of the samples from Room 3, fill, at Chilcott
(25 sherds), Room F, floor (30 sherds) and Room H, floor (50 sherds),
at Rim Valley, and Room 3A, floor 2, at Hooper (27 sherds) in the
seriation, it is obvious that such samples are not suited to the Robinson-
Brainerd seriation method. A swift glance at the Hooper Ranch seriation
will show that even larger samples don’t always seriate well with this
method. This is probably because such samples have been accumulated
over long periods of time.

Because of the unsatisfactory nature of some of our samples and the
limitations of the method, I again stress two statements previously made.
First, no inference made above applies to any site as a whole. These
statements apply only to the materials from which they are drawn.
Second, the evidence from the seriation is to be taken as suggestive, and
in some cases, it is hoped, corroborative, but never as conclusive. How-
ever, I do feel that techniques like the Robinson-Brainerd seriation
method are now and will increasingly become of utility in studies like
the present one. I hope I have demonstrated some of the utilitarian
aspects of such methods in archaeological analysis, while realizing still
more that I have demonstrated some of their limitations. I have been
encouraged rather than discouraged by the results of the applications of
the Robinson-Brainerd method to our data. The method should yield
much more dependable results when applied to large random samples
of surface materials or to large scale excavations.

V. An Analysis of Pottery Design Elements,
Indicating Possible Relationships
Between Three Decorated Types

By CONSTANCE CRONIN

Research Assistant, Department of Anthropology
University of Chicago

During the summer of 1960 members of the archaeological staff of
Chicago Natural History Museum excavated seven sites in the Little
Colorado drainage of eastern Arizona. When the pottery was classified
in the field, five established types were separated—Kiatuthlanna Black-
on-White, Red Mesa Black-on-White, Reserve Black-on-White, Tularosa
Black-on-White and Snowflake Black-on-White. The first four types have
been relatively well studied, but Snowflake Black-on-White was less well
known. It was first named by W. and H. S. Gladwin (1934, p. 22)
and described by Colton (1941, pp. 62-63); however, it had never been
completely analyzed from a large sample and the descriptions tended
to be too general for use in a detailed study of relationships with other
pottery types.

The present study was undertaken in an effort to analyze the con-
stituent elements of the designs found on Snowflake Black-on-White
pottery and also to inquire into the degree of relationship among the
five types. The basic factor chosen for analysis was the design element.
Each sherd was classified by its design element, and in this way small
discrete units were separated and then recombined so as to reveal basic
units and groups of designs which enable the worker in this field to recog-
nize any one pottery type as a distinctive entity and which set it off
from all other pottery types. Somewhat similar but not identical studies
had been undertaken in the past. Beals, Brainerd and Smith (1945,
pp. 87-137) compared Kana-a, Black Mesa, Sosi and other pottery type
designs (but not elements) from a series of sites. Martin (1939, pp. 431-
445) studied, by element, Abajo Red-on-Orange as compared with La
Plata Black-on-Orange. Therefore the present project was a pilot study
to ascertain the lineage of Snowflake Black-on-White pottery, and its

105

106 PREHISTORY OF EASTERN ARIZONA, I

subsequent growth through time, thereby adding to the general fund of
theory concerning the relationships and changes of pottery types in any
given area. Since so much archaeological reconstruction relies heavily
on ceramics, not only in the Southwest but also in Central and South
America and the Near East, systematic studies are vital as aids in these
reconstructions.

A cursory study of the sherds in the field suggested that Snowflake
Black-on-White might have evolved from earlier ceramic types, perhaps
specifically from Kiatuthlanna Black-on-White and Red Mesa Black-on-
White.

A superficial inspection of illustrations of sherds and whole pieces of
Kana-a Black-on-White and Black Mesa Black-on-White suggested that
these types might also have influenced the development of Snowflake
Black-on-White. One should bear in mind, however, that the Snowflake
Black-on-White found by the Museum staff was nearly always associated
with Kiatuthlanna and Red Mesa Black-on-White.

The work was divided into two phases: the first, undertaken by
Walter Boyer, formerly a ceramic restorer at the Museum, and myself,
involved the actual sorting and setting up of the inventory of design
elements present in all five pottery types; the second, that of interpreting
the results, was primarily my own work, but a number of people aided
me greatly by their criticisms and advice. This group includes Dr. Paul S.
Martin, Dr. John B. Rinaldo, Dr. Elaine A. Bluhm, Mr. William A.
Longacre and especially Dr. Arthur J. Jelinek, all of whom have my
heartfelt thanks.

This paper follows the two-fold division used in the study itself.

SORTING

The 2188 sherds were sorted on the basis of design elements only,
regardless of type. The elements were delineated as each new combina-
tion was observed for the first time. No attempt was made to fit a new
and slightly different element into an existing category, for it was felt
that some of these apparently minor differences might become important
when the changes in one pottery type were followed through time. In
this way, 45 categories of design elements were finally separated.

The sherds were then re-sorted into types by sites. Thus the Rim
Valley group was sorted into ‘‘Kiatuthlanna at Rim Valley,” ‘“‘Snow-
flake at Rim Valley” and ‘“‘Red Mesa at Rim Valley.”’ This sorting was
done by using the generally accepted criteria for pottery type recognition:
presence or absence of slip; whiteness of slip; intensity of paint; temper;

ANALYSIS OF POTTERY DESIGN ELEMENTS 107

proportion of black to white; fineness and blockiness of elements; posi-
tioning of design on a pot; and the general ‘“‘feel”’ of the total design and
technique of manufacture on each sherd.

The last step in the sorting process subdivided each of the groups
by design elements of pottery types at sites. Each of the numerous groups
then contained ‘‘X design element of Y type at Z site.’ The chart
(Table 11) of total design elements, prepared after the first step, was
utilized here so that the number of elements remained the same.

ANALYSIS

In order to regularize the vast amount of data and the numerous
variables in this study, a series of graphs and bar charts was utilized.
These suggested a closer relationship between Kiatuthlanna and Snow-
flake than between Red Mesa and Snowflake, as had first been con-
jectured, and clearly showed that the relationship between these types
was much closer at earlier sites than at the later sites, since fewer design
elements were shared through time. (Since the Tularosa and Reserve
types proved too divergent in elements shared with the other three types,
we decided to omit them from the analysis. Our main concern was with
establishing relationships, and these two types, though perhaps related
to the rest, were sufficiently dissimilar to justify exclusion.)

To clarify further the relationships between Kiatuthlanna, Red Mesa
and Snowflake, the data were quantified by applying the Brainerd-
Robinson method (Brainerd, 1951; Robinson, 1951) to the percentages
of each design element, both for each type and for each site (Tables 12
and 13). (For an explanation of the Brainerd-Robinson method, see
p. 87.) Two series of coefficients of similarity were arrived at, one of
which showed degree of similarity within types at different time levels:
Red Mesa at Chilcott 1, with Red Mesa at the earlier site, Goesling,
and at the later site, Chilcott 2 (Table 12). These figures confirmed
and agreed with our previous impressions regarding relationships between
types and also revealed some additional unexpected correlations which
are set forth below.

CONCLUSIONS

It is apparent that no firm conclusions can be drawn from this study,
but some possible correlations can be suggested on both a specific and a
general theoretical level.

By the use of the processes described above, our initial hypothesis
concerning the relationships between Red Mesa and Snowflake was not

108 PREHISTORY OF EASTERN ARIZONA, I

confirmed—Red Mesa and Snowflake are not closer to each other than
either is to Kiatuthlanna—but a different relationship is apparent (Table
13). In the earliest site (Goesling) Snowflake Black-on-White is probably
not present and the coefficient of similarity between Kiatuthlanna and
Red Mesa is 121.2, pointing out a definite but not extremely close rela-
tionship between the two types. In the next later site (Chilcott 1) Snow-
flake appears for the first time, along with Kiatuthlanna and Red Mesa.
Here the similarity between Kiatuthlanna and Red Mesa has dropped
to 94.4 and the relationship of Kiatuthlanna to Snowflake is 137.6, while
the ratio of Red Mesa to Snowflake is 98.0. At this time level, then,
Snowflake is closer to Kiatuthlanna than Red Mesa is to Kiatuthlanna
or to Snowflake.

At Rim Valley, another site where all three pottery types occur to-
gether but at a later time level than at Chilcott 1, the figures (Table 13)
reveal greatly attenuated relationships between the three types. The
relationship between Kiatuthlanna and Red Mesa has dropped to 57.0,
that of Kiatuthlanna and Snowflake has decreased to 97.9, and the Red
Mesa-Snowflake ratio is now 68.1. The decreasing degree of closeness
of all three types to each other is clearly evident here, but the figures
also show that Snowflake is still closer to Kiatuthlanna than it is to
Red Mesa or Red Mesa to Kiatuthlanna.

One might postulate that Snowflake began as a 2-1 blend of Kiatuth-
lanna and Red Mesa design elements not long after Red Mesa had grown
out of Kiatuthlanna. It is perhaps naive to say that pottery types change
through time but the question here is, how do they change? If we can
demonstrate that one type came about as the result of a blending of
manufacturing principles of two existing types, then we should be able
to demonstrate the ‘“‘drift’? of each. The concept of linguistic drift was
formulated by Sapir (1921) but it may be equally applicable here. An
initial unity between Kiatuthlanna as the parent and Red Mesa and
Snowflake as daughter types does not necessarily imply the same line of
development for each through time. And, indeed, this study shows that
the very close similarity of types near the time of origin may give way
to quite individual and specific evolutionary lines as stylistic trends impel
each type in a different direction from its source.

_ Even if the suggestion given above is true, we still expected to find
the same regular though decreasing set of relationships of a type through
time as we found between types at a site. For instance, if the coefh-
cient of similarity of Kiatuthlanna to Snowflake at Chilcott 1 was 137.6,
we assumed that the coefficient of similarity of Snowflake at Chilcott 1

ANALYSIS OF POTTERY DESIGN ELEMENTS 109

and Snowflake at Chilcott 2 would be higher, since a type should be
closer to itself than it is to another type. But such is not the case, for
generally speaking there is a greater degree of similarity (shared design
elements) between types at one site (e.g., Kiatuthlanna and Snow-
flake at Chilcott 1) than between different time levels of one type (e.g.,
Kiatuthlanna at Chilcott 1 and Kiatuthlanna at Rim Valley). Red Mesa
in particular exhibits an extremely erratic course, jumping from 76.8 at
Goesling to 107.5 at Chilcott 1 and then back down to 67.9 at Chilcott 2.
Since any coefficient of similarity below 100 is all but meaningless for
showing relationships, are we to assume that Red Mesa is more Red
Mesa at Chilcott 1 than it is at the other sites? Snowflake is more regular
in its passage through time, but even here the divergence at the latest
time period, Rim Valley, is greater than its similarity at the point of
origin, Chilcott 1. Kiatuthlanna is difficult to assess here since it is
found at only three sites, but even so the figures seem meaningful, since
the extremely low coefficient of similarity is not what one would expect
to find in one pottery type.

With respect to the design elements themselves, several trends are
apparent in our limited sample both with regard to uses of elements
in the decoration of the three types, and with respect to the overall
distribution of the elements through time.

The observations for the three types are as follows:

Kiatuthlanna Black-on-White——Fine line and checkerboard decoration
occurred in all samples and the distribution of ticked fine lines and
ticked triangles suggests continuous use throughout the distribution of
this type in this study.

Earlier Kiatuthlanna seems to have been characterized by the use of
squiggle-hatched elements and triangular solids.

Later Kiatuthlanna was apparently characterized by the use of wider
lines, diagonal hatching or none at all, sawtoothed solids, and the rec-
tangular scroll. Absent elements include squiggle lines and spirals and
medium line.

Red Mesa Black-on-White-—Fine line decoration is common to all
samples and the distribution suggests that checker elements were also
universally used, as were spirals and ticking. There appears to be a trend
of less frequent usage of fine lines in combination with solid elements
through time.

Squiggle lines characterize earlier Red Mesa, but no squiggle hatching
was encountered.

110 PREHISTORY OF EASTERN ARIZONA, I

Later Red Mesa is characterized by the use of sawtoothed solids,
greater use of solids in general, and diagonal hatching.!

Snowflake Black-on-White-—Wide line and opposed solids are in fre-
quent use through the whole range of our samples. The distribution sug-
gests that fine line and solids were used through the whole range.

Early Snowflake seems characterized by the use of squiggle hatching
and perhaps checkered elements.

Later Snowflake makes use of diagonal hatching and occasionally
ticking, checker and spiral-scroll elements.

Thus we can see that the methodology used in this study is a valuable
technique both to set out a detailed pottery type description and to trace
genetic relationships between types. This method lends itself to both
graphic and statistical presentation and may prove a useful aid in future
ceramic research.

This study was undertaken in an attempt to delineate intertype relation-
ships and also to discover the worth of this technique for further expanded
studies. The latter aim we feel has been well demonstrated and we can
only hope that the results of and the questions raised by the first stated
purpose will be followed up and expanded by other workers in this field.

NAMES OF DESIGN ELEMENTS REFERRED TO IN TABLE 11

Code
no

Wide Line 3
Medium Line . 2
Fine Line . 5 ee, pre cee Cae ae PORT Oh ey ve ae |
Fine Line and Solids Be lates Lo Sin hee ay a. oe eta, uta ~ See ie ok ice | oy alee eee
Fine Line and Triangles Heel hl ceet See a eS
Bine Wine and Wlickedslriangles! ss, 7 3) i a 2c is CEA Le)
Line and Dot 5 mates) Me prio) Shuag heise a atodae ce Keak awa can 6. eine cone ae
Line and Single Terrace . . rer area | Clare ae ase ets ee 8
Single and Double Ticked anes no! ss AS tee ee Ve
Single and Double Ticked Lines and Ticked Rtasiole saa Solids oy Se abl ike ae

1The sample from Chilcott 1 Site is peculiar in missing a number of elements
common to Red Mesa at the Goesling and Thode Sites. These absent elements include
‘ticking, checker and squiggle lines and suggest that the Chilcott 1 sample may be
later than indicated by other means or perhaps indicates that several trends were
initiated here. These would include the use of diagonal hatching on Kiatuthlanna
and Red Mesa while squiggle-hatching distinguished Snowflake. Other techniques
unique here include complete lack of use of ticked elements on all types and the only
instance of the use of opposed solids on Kiatuthlanna.

ANALYSIS OF POTTERY DESIGN ELEMENTS 111

NAMES OF DESIGN ELEMENTS

(continued) Code
no

eked ime and jsolidsrand Plamrbine "2s es wi a, ee ees oe 8
ducked dime anudinianglerand Plaintliney. 9% fia fh) eae Se see, 14
Breer ine "2: 2 rit ooo ah ON eR ee eee Ble Gy) aoe ek
Squiggle Hatch .. . SR ger eh Ra tee co ter ant ey a ar ar a eee!
Squiggle Hatch and Fine en, hee aie ra OS GS sy ae Wien LS 7.) oe reg aD,
Squiggle Hatch and Narrow Hands Te Roa Rei tM NN, Bek Cy Ae a
meee Hatch and Ciryilmear Bands {0.460 % 2. F & Pe BA ee TD
Beuiecie Hatchand Angular Bands 9 65.055. 6 « ee he Pay ee 5 ab 26
Peete ACRE AMIEL ACD GS Te ic is “aa oe ees Ee Ws 8 os esd) 8
Casal LAME UME SIO 2 i Oe gd cae se ls SR ae le y ae
WinvonvalshlatcoperagimMcntss eee he tas ee eta eee ee Cae ONL oda erg ate 8
Interlocking Spiral. . .. . BAS ae act, SM Re GY ot OR
Simple Spiral and Circle and Cewei F aneenis pes eee ace eh as ee eee Od
Doticdeand plate heserollsy Metra tee ee ee eas nee oh TH oe Sg ees ee OO
PRCCPALCTT AIS SCLO Mien 54 11k Aco 9s, ey ayes et Mert epee oe, Ue, ee he ee
iiianeuar Scerolims . 2: ana oe te ey ee oe AL)
Interlocking Rectangular Scroll with Key Badines hace et ee ee
Interlocking Solid and Hatch Rectangular Scrolls and Solid Seralls Pe eee eo Res
Dieplicle Masiclta pera ee ue Ae eh eaN yg ed ie renee ed een i eta ce Mes Gee ie oS es boas AD
Haicheunanple 9, - Se ee eR ey ee cate een Ofte lS
Ticked Triangle and Single fecace: FO Nil ks SUR 5 ee ED, ote By a eas 5
ickedwunaAnole ander aCMentt a6 lee a cede eh Ps es cc ay ed a ee en iste ew M2
PC MARSA ICING AMEE Sart oe UE oo A ee tes Mele gk Wg, PL hy abc el ke
Opposed Solids ... . Ge GY ot ice At GE Ce ar ee ee ee ne
Opposed Solids and Baniegle Batch’ EL lnc ot Re eee ee
Opposing Solid Step Triangle . . . Ne any Sc ee Irae me Ge Wert aor ee |
Opposed Solid and Hatch Step Tianele SC) aya een) Fed ee eee eae Gi
Mrpcsedeltaten and moldy Merracess.) . ao. eo ge Se ee ew ss OO
PCat eu IAI pam. era h Meet) cae: cebean 3) By Se ver ek can Sar ORs ns ae
Nepaivevtaralelopranise.. seed. saws. awienle cA ee oe ee aD
RIE ois, aod Ae SCM ca rae SOA to eet wey 9
DIST eMC CC CtmE ments ts tame tbe celui cay, a vote LE ww ns Go ee
DN AMIOME MANGE Kein atte fut er lay an ae VS Sees Ben ei So) Se Saw
Rae A Ae Rees ete: Ge eae swe Oa es ea ee oe

VIRGO LE ATICOYIS( 5 Gene Cente ET hae sok ef RI, oe ke MA ce he a 2 Peng

112

PREHISTORY OF EASTERN ARIZONA, I

TasLe 11.—PERCENTAGES OF GIVEN TYPES BY DESIGN ELEMENTS

No. of sherds
Design no.!

i.)
is)

—
AaANRPACAURP ND

ieee)
- 0

Goesling
360 554
K RM
a #
aii
13.6 Tat
WARN are
10-3. ~ 232
jl) Rs me Ee GO
19 22.0
8 250
nO) Bes
6.4 4
tA
14 1:8
Php lets:
a0) aut
Pas 4
3.6 4
2B, “z3
POS S128
25
3 Sih
£6 Atal
oS 2.5
35
4-7 ae4
126
25 ee)
29)
8 4.5
1.3
ib emg Or
4
LG we 22a
OFS meee
4
ih a2,
3 8)
iat = Ses

1A= Kiatuthlanna;

RM= Red Mesa;

AT GIVEN SITES

31
Kk

NNDDN

16.

ae
2)

Chilcott 1 Chilcott 2
105 294 ils 17
RM iS RM S

On oe esoes 237-5
Sih aie hed

4 4.8 a
TOSS 15.4

Ai) Theil
a9 as
1.0 <3
55
1.0 Auf 5.9

2, A Oy eed 11.8

4 5.4 Bao)

A 4.8 44:8 (540 la 6

4 8.6 5
2.9
Bes aS
1.0 25

a7,
130) ee
ao

I om en kal) Tet
1.9
1.9
2.9 Well

1 Ano 1359 Te, Li

2 AS Ore =e O
Sots A

10
1: On Stes Tesi
2
2 Ae)
ja,
AVG 2 BeS1e3: 23:1 D8
S= Snowflake.

Chilcott 3
19 15
RM iS
3126 53-3
26:25
Sy
575 Ono
Rr be <a Seye
6.6
6.6
a3
5
Ses
6.6
1055" 3323

ANALYSIS OF POTTERY DESIGN ELEMENTS

3111}

TaBLeE 11.—PERCENTAGES OF GIVEN TYPES BY DESIGN ELEMENTS

AT GIVEN SITES (continued)

Thode Rim Valley

No. of sherds 46 68 22 67 139

Design no... RM S Kk RM Ss
3 5927, ea | 10.8
a 19.6 The ot SILAS 953
1 8.7 as
9 1.5 7.5 1.4
8 6.5 ils)
10 4.5
6 im es 326
21 ies: 15
fi 4.3 1.5
4
28
14 Sill
20 4.3 15
SY 15
39
25
19
26
38 15
43 217
35 4.3 4.5
32 3.0 1.4
34 4.3 2.9 Si4(0)
30 4.5 7
42 15 1.4
40 1Wieels: 1.4
Pal
36 6.0 i
5 5.9
i HS)
11
12 S15i)
24 Dae i les 4.5 TZ.
44 oe 1053
29 205
41
31 22
33 2.9 ‘ie
22 aT al
16 4.5 5 1.4
15 Tis 9.1 5 1.4
17 pap a2 i,
18 16.1
45 L5e2 SU By wiiso 21:6

1A=Kiatuthlanna;

RM=Red Mesa; S'=Snowflake.

Rhoton
7 20
RM iS.
143 25.0
50)
14S
14.3 50
28.6
10.0
20.0
28.6
5.0
30.0

114 PREHISTORY OF EASTERN ARIZONA, I

TaBLe 12.—BRAINERD-ROBINSON RATIOS, SHOWING SIMILARITY
WITHIN SINGLE TYPES AT SITES OF
DIFFERENT HORIZONS

C2-C3. C3-T T-RV C1-RV G-RV

Pottery ‘Types G-C1—-C1-C2
Kiatuthlanna..... 37.0 = = = = 44.0 170
ede Mesaneeaene 76.8, L075 67.9 (420 ORS == =
Snowflake........ = Wey INOS Sp NOS INOS 66 = =

TaBLE 13.—BRAINERD-ROBINSON RATIOS, SHOWING SIMILARITY
WITHIN POTTERY TYPES AT SINGLE SITES

Pottery Types G Cl C2 C3 a RV R
Kiatuthlanna-
Red Mesa..... (Palla? 94.4 — — — 47.0 —
Kiatuthlanna-
Snowflake...... — 1376 == — — 97.9 —
Snowflake-Red
Mesa so ee — 98.0 62.4 105.6 63.8 Gifen 38.5

G=Goesling Site; C1 =Chilcott 1; C2=Chilcott 2; C3=Chilcott 3; T=Thode;
RV=Rim Valley; R=Rhoton.

VI. Artifacts

By Joun B. R1iNALDo
Associate Curator, Department of Anthropology
Chicago Natural History Museum

INTRODUCTION

The stone and bone artifacts were analyzed with the aim of tracing
the cultural developments within the area of the upper Little Colorado
and comparing them with developments in neighboring areas. Although
we continued to be interested in the ways in which the artifacts were
made and used, a comparison of artifact types by areas and horizons
took precedence in this analysis. (For dimensions, proveniences and de-
tailed descriptions of particular stone artifacts see Martin, Rinaldo, Long-
acre, and Freeman, 1961.)

Before A.D. 850 changes in the stone and bone artifacts were few and
occurred at widely spaced intervals. After this time, change took place
more rapidly and items such as stone axes which were not part of the
native complex appeared as trait unit intrusions. Somewhat later we
find the use of coursed stone masonry structures, black-on-white pottery
and full-grooved axes.

Shells from the Pacific coast found at Hooper Ranch Pueblo (Martin,
Rinaldo and Longacre, 1961, p. 108) indicate that there was trade be-
tween this area and the region to the south and west. Such traits as
hachured black-on-white pottery, a crude sort of banded masonry, full-
grooved axes, and certain features of the Great Kiva (deflector and
masonry-lined vaults) make it appear that there was also trade between
the Little Colorado and the Chaco district to the north. This is borne
out by the recovery, in the Chaco district, of shells and pottery which
were probably traded from areas to the south and west (Judd, 1954, pp.
88-89, 196).

TOOLS USED IN THE PREPARATION
AND STORAGE OF FOOD

There appears to have been a cultural lag between the upper Little
Colorado and the neighboring areas to the south at about a.p. 300.

115

116 PREHISTORY OF EASTERN ARIZONA, I

Troughed metates and tabular two-hand manos, which were present at
the SU Site (Martin and Rinaldo, 1947, pp. 320, 328) and at the Bluff
Site (Haury and Sayles, 1947, pp. 66, 67), were lacking at the Tumble-
weed Canyon Site. The lack of pottery at the latter site may be another
indication of the conservative nature of this culture.

Manos
Over 140 manos or fragments thereof were removed from the eight
excavated sites (including the three Chilcott sites). These have been
classified into major groups according to the size and number of grinding
surfaces, and into minor classes based on the shapes of the grinding
surfaces in various combinations. A large number of fragments were
recovered that were too small to classify.

One-hand Manos (fig. 50).—Thirty-two specimens were recovered. The
majority of these are oval or sub-rectangular in outline (fig. 50). They
range in length from 10.1 to 16.5 cm., in width from 7.1 to 11.2 cm.,
and in thickness from 3.2 to 8.6 cm.

The manos in one sub-group are more sharply convex across the
short dimension than across the longer one. On the few specimens where
striae can be seen they cross the short dimension at an angle of about
80° to the long axis. These appear to be more closely related to the manos
of the Beach Sites such as Little Ortega Lake (Martin and Rinaldo, 1960a,
p. 17, fig. 4, 6) than to those of the later sites. They are also more like
those of the Cochise culture of southern Arizona, particularly Ventana
Cave (Haury, 1950, p. 313), than like those of more closely neighboring
Cochise sites such as Wet Leggett Site (Martin, Rinaldo and Antevs,
1949, pp. 66-71) or the Cienega Site (Haury, 1957, p. 20). These manos
came only from Tumbleweed Site. There were six specimens in the
group and they are associated only with basin metates.

Another division comprises manos with convex or bluntly convex
grinding surfaces. In two instances they are opposite a flat grinding sur-
face. There are seven specimens in this group, most of which come from
the Chilcott Sites (four specimens), although two came from the Thode
Site and one from Rim Valley Pueblo. This sort of mano is usually more
common on earlier sites both in this area (Martin and Rinaldo, 1960a,
pp. 70-73) and at Forestdale (Haury, 1940, pp. 99-100; Haury and
‘ Sayles, 1947, p. 66), although a few have been recovered from later
sites. These manos are more commonly associated with basin metates
but were probably also used with trough metates.

A third sub-group of the smaller manos has flat grinding surfaces.
Nineteen specimens of this type were found, and it is thus the largest

ARTIFACTS 117

Fic. 50. One-hand manos, Tumbleweed Canyon Site. Length of lower right
specimen, 13.4 cm.

sub-group of shorter manos. They were recovered from most of the
sites excavated, including the Tumbleweed Canyon Site on the early
end of the sequence and Rim Valley Pueblo on the later end. Occa-
sionally these manos are rectangular or sub-rectangular in outline. This
variety is occasionally associated with trough type metates. Generally
these manos appear to be a class which forms the link in the development
into the longer flat-tabular mano and eventually into the beveled mano.
They could have been used for a short time on a trough metate without
being worn to a convex shape on the sides of the trough because they
are short, but this type is believed to have been commonly associated
with a flat metate.

Two-hand manos (fig. 51).—These longer manos comprise the larger
of the two major groups and total 113 specimens. They range up to 25 cm.
in length (average length about 18 cm.), and the width is about 11 cm.
Occasional specimens are 13.5 cm. wide, and a few loaf-shaped speci-

118 PREHISTORY OF EASTERN ARIZONA, I

Fic. 51. Intermediate and late types of manos from Rim Valley Pueblo, Thode
Site, and Chilcott Site 1. Length of lower right specimen, 25.0 cm.

mens are over 5 cm. thick. These larger manos were found in the same
rooms with trough metates and slab metates. Only two longer specimens
were found on the Tumbleweed Canyon Site, and this sort of mano
occurs most often on later sites throughout the northern Southwest

(Woodbury, 1954, p. 70). By comparison, one-hand manos have only
a sporadic distribution on later sites.

ARTIFACTS AS

In this major grouping there were about 54 manos which had single
grinding surfaces ranging from flat to convex in shape. Many of these
were mere fragments. The majority of complete specimens are rectan-
gular in outline, although many have rounded corners; they were prob-
ably used on trough metates.

A second minor group consists of those with grinding surfaces beveled
into two fairly equal planes, but with no grinding surface on the opposite
or upper side. There are sixteen specimens in this group, and (with two
exceptions, one from the Hooper Ranch Pueblo, one from Chilcott
Site 1) they come from the Rim Valley Pueblo. This distribution—
primarily on the later sites—parallels the increase in popularity of this
type in other areas such as the Jeddito (Woodbury, 1954, fig. 9, p. 82),
the Rio Grande (Kidder, 1932, p. 71), and the Reserve area (Martin,
et al., 1956, p. 58), during late Pueblo III and early Pueblo IV.

RUBBING STONES
(Figure 52)

None of these tools were shaped in outline. The 26 specimens recovered
fall into two major groups (whether they have one rubbing surface or two
rubbing surfaces opposite each other). A further division may be made
on the somewhat arbitrary distinction between flat and slightly convex
rubbing surfaces. No rubbing stones were recovered from the Chilcott
Sites, and only one from the Great Kiva at Hooper Ranch Pueblo,
although several were recovered from the secular rooms. A few have
striations on their rubbing surfaces like the manos, and they may have
been used as small manos.

Fourteen specimens have single rubbing surfaces. Most of these rub-
bing stones are oval in outline. They range in length from 4.0 to 11.3 cm.,
in width from 3.0 to 10.0 cm., and in thickness from 0.7 to 5.0 cm. Six
specimens of this group were recovered from the Tumbleweed Canyon
Site and fewer from the later sites. Whether the diminished numbers
of this particular group in late sites denote an actual decrease in pop-
ularity of this tool throughout the area in the later phases is not quite
certain because ordinarily those with two rubbing surfaces are more
frequent on the late sites. However, the greater frequency of rubbing
stones at the Tumbleweed Canyon Site and their paucity at the Hooper
Ranch Pueblo corroborates the theory that they are scarce on the latest
sites, as was seen in the Reserve area (Martin, e¢ al., 1956, p. 58; Rinaldo,
1959, p..229),

The group with two rubbing surfaces comprises 12 specimens, 3 with
flat rubbing surfaces and 9 with slightly convex ones (including one speci-

120 PREHISTORY OF EASTERN ARIZONA, I

Fic. 52. Rubbing stones, miscellaneous types, from Goesling Site, Thode Site,
Rim Valley Pueblo, and Hooper Ranch Pueblo. Length of lower right specimen,
5.8 cm.

men with this shape of rubbing surface opposite a flat_one).. These were
most common at the Thode Site and less popular both earlier and later.
In general they are thinner than the rubbing stones with only one rub-
bing surface.

PESTLES
(Figure 53, a, b, e)

These elongate crushing tools are less common in the upper Little
Colorado than they are in the Reserve area (Martin and Rinaldo, 1960a,
p. 64) or farther south in the San Simon Branch of the Mogollon (Sayles,

ARTIFACTS 121

1945). Only four of these were recovered from three sites out of the eight
tested. The pestles fall into three classes: cylindrical, pear-shaped, and
multiface.

The cylindrical pestles are elongate, roughly cylindrical tools with
tapering ends, the larger extremity battered from use. The larger speci-

Fic. 53. Pestles, miscellaneous types, and hammerstones, Tumbleweed Canyon
Site and Rim Valley Pueblo. Length of e, 22.4 cm.

men is 22.4 cm. long and 10.2 cm. in diameter, the smaller about 10 cm.
shorter and 1.0 cm. less in diameter. The larger specimen comes from the
Tumbleweed Canyon Site and is very much like one from the SU Site
(Martin and Rinaldo, 1940, p. 52, fig. 23) and also like one from Crooked
Ridge Village (Wheat, 1954, p. 117, fig. 43, d).

122 PREHISTORY OF EASTERN ARIZONA, I

Another pestle is long and roughly pear-shaped, its smaller end rough-
ened from use. It is 11.5 cm. long, 7.0 cm. wide, and 4.9 cm. thick.
It was recovered from Room B at Rim Valley Pueblo, a room which
lacked a mortar or even a basin metate, but which was provided with
three flour receptacles with stone slab bottoms. One of these slabs had
been roughened and the pestle may have been used with it.

A multiface pestle came from the same room. Like many pestles
of this type it has one end pitted and battered from use as a pestle and
one broader surface striated from use in grinding. It could have been
used in the same flour receptacle. Multiface pestles were recovered at
Point of Pines (Wheat, 1954, p. 117, fig. 43, e) and in the Reserve area
(Martin, Rinaldo, and Barter, 1957, p. 56).

METATES
(Figure 54)

The nether milling tools which were used with manos fall into four
major groups within which some minor distinctions may be made. These
are basin metates, trough metates with only one end of the trough open,
through trough metates, and flat metates. Thirty-nine specimens were
recovered, but most of these are fragments. We were able to distinguish
between basin metates, trough metates, and slab metates in fragmentary
form, but we could rarely distinguish between the two types of trough
metates.

The basin metates (fig. 54, left) are with one exception (a fragment)
from Tumbleweed Canyon Site. These are thick slabs of igneous rock,
without regularity of outline, having a shallow basin in one broad surface.
This basin is usually smooth in the center and pitted from pecking near
the periphery. All of the specimens were broken but enough could be
pieced together from the scattered fragments to give us a good idea of
their original appearance but only a rough idea of actual dimensions.
One of these that may or may not be typical was 32.0 cm. long, 30.0
cm. wide, and 2.6 cm. thick. These are similar to the dimensions and
shape of the “‘thin slab’’ basin metates from the Beach Sites (Martin and
Rinaldo, 1960a, p. 24), and similar in form to those of the Chiricahua
stage of the Cochise Culture (Sayles and Antevs, 1941, pl. 9). They
are also similar to those of the Hilltop, Penasco and Pine Lawn Phases
(Haury and Sayles, 1947, p. 64; Sayles, 1945, p. 50; Martin, 1943, p. 186),
although trough metates were somewhat more popular during most of
these “‘pithouse”’ phases.

A nearly complete specimen of trough metate with trough open at
one end only was found at the Goesling Site (fig. 54, center). This metate

“WS (gp “usuTIOods WY SII Jo ySusTT “YsnoN YSnosy) YUM
ueurtads yys141 ‘AyUO pus suo ye usdo ysnoxy YIM UdUTTDAdS 3a}Ua9 ‘9d A} ulseq uourtoods Ja] :sayej9uN Jo soddy dary], “$S “OIG

123

124 PREHISTORY OF EASTERN ARIZONA, I

is made from a generally oblong slab and has a flat shelf for the mano
to rest on at the closed end. The sides of the trough are nearly straight,
the bottom and sides of the slab rough hewn. Except in size (it is smaller)
it is much like the metates of the Modified Basket Maker period (Roberts,
1940, p. 118; Martin, 1939, pp. 398-399), but also like those at the Twin
Butte Site (Wendorf, 1953, p. 128).

Through trough metates (fig. 54, right) occurred at the Chilcott
Sites and all the later sites in this area. These specimens are made from
fairly thick oblong blocks and the trough runs from end to end, although
in some supposedly little-used specimens it slopes up at the near end.
One of the whole specimens (from the Rim Valley Pueblo) has the
following dimensions: length, 43.5 cm.; width, 27.0 cm.; thickness, 8.5
cm.; width of trough, 22.5 cm.; depth of trough, 4.8 cm. There were
seven complete specimens recovered. They are comparable to metates
from the neighboring areas and broadly similar ones are found throughout
the Southwest (Bartlett, 1933, p. 23-27; Martin, et al., 1956, p. 73).

A few small fragments of slab metates were recovered from the later
sites. They are too small for further identification or analysis, but are
enough to indicate the presence of a type which was the predominant
one at Table Rock Pueblo.

SMALL METATE-LIKE GRINDING STONES

Three small metate-like grinding stones were recovered in Room A,
Rim Valley Pueblo. One of these measures 27.0 cm. long, 25 cm. wide,
and 7.5 cm. thick, with a depressed grinding surface on one side ap-
proximately 12.0 cm. in width and 0.5 cm. in depth. These surfaces
run the length of the stones as in trough metates, and the scratches they
bear resulting from use run in this direction also.

These tools are similar to some of the smaller metates recovered at
the Point of Pines site, Arizona W:10:51 (Wendorf, 1950, p. 54), and
the grinding slabs from Ruin B, Nantack Village (Breternitz, 1959, p. 65).
They were also recovered from sites in the Reserve area such as Higgins
Flat Pueblo (Martin, et al., 1956, p. 78) and Three Pines Pueblo (Martin
and Rinaldo, 1950b, p. 468).

MOorTARS
(Figure 55)
The seven mortars found are with one exception stones with cup-

shaped depressions excavated into one surface. They range in length
from 15.8 to 29.5 cm., in width from 10.6 to 19.0 cm., and in thickness

ARTIFACTS 125

Fic. 55. Mortar from Thode Site. Length, 28.0 cm.

from 4.1 to 13.5 cm. The cups are from 5.0 to 10.7 cm. in diameter and
from 0.8 to 7.0 cm. deep. They were recovered from the Goesling and
Thode Sites and from Rim Valley and Hooper Ranch Pueblos.

These appear to be similar to mortars and stone bowls from Point
of Pines (Wendorf, 1950, pp. 57-58; Breternitz, 1959, pp. 41-42) and
from the Reserve area (Rinaldo, 1959, p. 241; Martin and Rinaldo,
1950b, p. 470). Only one specimen was neatly worked on the exterior;
the others were rough. However, specimens from the dwelling rooms of
the Hooper Ranch Pueblo were more specialized in nature (Martin,
Rinaldo and Longacre, 1961, p. 71).

Por Covers
(Figure 56, lower)

Two stone discs with flat broad surfaces and rough-hewn edges were
recovered, one from the Great Kiva at Hooper Ranch Pueblo, the other
from Pithouse A at the Goesling Site. They are 16.2 and 9.8 cm, in

126 PREHISTORY OF EASTERN ARIZONA, I

diameter respectively, and 2.3 and 1.1 cm. thick. They are similar to
objects found in place as jar covers. This type of artifact—rare in the
Mogollon area—is more frequent on sites to the north such as Tseh Tso
(Brand, Hawley and Hibben, 1937, p. 95) and might possibly repre-
sent the diffusion of this trait from the north.

HAMMERSTONES
(Figure 53, c, d)

Tools of this type are fairly common in most Southwestern sites.
We collected 29 of them, many from the later sites (Rim Valley Pueblo,
Hooper Ranch Pueblo). They are generally angular stones, although
some are reduced through use to a round shape. Those we collected
were from 5.9 to 11.5 cm. in diameter (or greatest dimension). Marks
of use and association with other artifacts indicate that they were used
for several purposes—for roughening the surfaces of milling stones (peck-
ing), for pounding, and for percussion flaking.

Por Rests

These crude stone objects, which occurred only at the Rim Valley
Pueblo, were simple, unshaped oblong blocks of stone set in the firepits
to support the cooking pots and hold them against a corner of the firepit.
This type of object has been recovered from the dwelling rooms at Hooper
Ranch Pueblo, Table Rock Pueblo (Martin and Rinaldo, 1960a, p. 256),
and Foote Canyon Pueblo (Rinaldo, 1959, pp. 250-252).

TOOLS USED IN POTTERY-MAKING

Many of the milling tools such as manos, metates, mortars and pestles,
which were used for crushing grain and seeds, were also used for grinding
pigments for paint. We found manos, metates and mortars with pigment
on their grinding surfaces in the rooms at Rim Valley Pueblo and at
Hooper Ranch Pueblo. They were also probably used for pulverizing
clay. These tools have been discussed above. Gourd scrapers used for
scraping the surfaces of unfired vessels to smooth them were not recoy-
ered. We found several polishing stones (fig. 57). These are generally
oval in outline and have one flat facet derived from long use. These were
found at Rim Valley Pueblo and the Hooper Ranch Pueblo. They range
in length from 3.1 to 6.7 cm., in width from 1.9 to 5.1 cm., and in thick-
ness from 1.3 to 4.8 cm. ‘They are all made of dense stone.

Fic. 56. Maul, axe, and pot cover from Rim Valley Pueblo and Hooper Ranch
Pueblo. Diameter of lower specimen, 16.2 cm.

127

128 PREHISTORY OF EASTERN ARIZONA, I

Fic. 57. Medicine cylinders and pot polishing stones from Hooper Ranch Pueblo,
Rim Valley Pueblo, and Goesling Site. Length of lower right specimen, 4.1 cm.

TOOLS USED IN THE CONSTRUCTION OF HOUSES

The few tools described below have traditionally been classified under
the category concerned with building. This assignment has been made
primarily on the basis of ethnographic information. The provenience
of these tools in an archaeological context has furnished remarkably
little evidence as to their use.

ARTIFACTS Hee,

One axe and one maul were recovered from Rim Valley Pueblo.
Choppers were recovered from three of the eight sites investigated. Axe-
grinding slabs were found in Rim Valley Pueblo and in the dwelling
rooms at Hooper Ranch Pueblo. Axes and mauls were recovered from
the dwelling rooms at this pueblo during the 1959 field season.

AXE
(Figure 56, upper right)

This tool may have been used for cutting the roof members—beams,
poles, splints and brush. This axe is of the three quarters grooved type,
with the groove located near the middle. The sides and the poll are almost
flat. The bit and other broad surfaces are polished. This specimen is
13.2 cm. long, 7.0 cm. wide and 4.9 cm. thick. It is of a form which
Roberts (1932, p. 141) has classified as tabular. The poll is longer than
on the majority of three quarters grooved axes, the bit is only medium long.

The three quarters groove tends to classify this axe as a ‘“‘southern”’
type. The proportions of the poll and bit are generally similar to those
of axes from the Canyon Creek Ruin (Haury, 1934, pl. 71) and from
Foote Canyon Pueblo (Rinaldo, 1959, fig. 105).

Mau.
(Figure 56, upper left)

The maul or grooved hammer was found in the fill of a dwelling
room at Rim Valley Pueblo. It is full grooved and has flat faces so
that it has been classified as belonging in the tabular type. This imple-
ment is made of a heavy basalt stone and is 12.0 cm. long, 7.5 cm. wide
and 5.8 cm. thick.

Full-grooved mauls appear early in the Mogollon culture but they
appear to decrease in popularity. They are not as abundant on the
later sites as on the earlier ones. The full-grooved type had a more
widespread use than the three quarters grooved type.

AXE-GRINDING SLABS
(Figure 58)

In one surface these thick slabs or blocks have a broad shallow groove
of the shape and size that would be produced by grinding a stone axe.
The width of the groove corresponds roughly to the size of the blades
of the axes recovered from ruins in this area.

130 PREHISTORY OF EASTERN ARIZONA, I

Similar grooves, although usually in bedrock, have been reported
from other sites in the Mogollon area (Hough, 1914, p. 4; Martin, et al.,
1952, p. 38; Rinaldo, 1959, p. 244). They were recovered only from
Hooper Ranch Pueblo and Rim Valley Pueblo during the 1960 season.

CHOPPERS
(Figure 59)

Rough choppers were probably used for many other purposes besides
cutting roofing timber for houses, but apparently axes replaced them
during the later periods and so they are included here with axes. They
are usually of a convenient size to grasp in the hand. One edge is steeply
chipped by percussion to form a sharp cutting edge, and usually a portion
of the natural smooth surface of the stone on the opposite margin is
left intact to provide a comfortable place to grasp the implement. They
range in length from 7.2 to 9.8 cm., in width from 6.1 to 9.1 cm., and
in thickness from 2.9 to 6.2 cm.

Choppers occurred at most of the sites that we excavated. The biface
type (with cutting edge chipped from both surfaces) was found only
at the two latest sites—Rim Valley Pueblo and Hooper Ranch Pueblo—
and in general the uniface type of choppers appears to be more common
in the upper Little Colorado drainage. Our sample may be inadequate
because this seems to contrast somewhat with the distribution of similar
implements farther south where biface choppers are found throughout the
sequence (Haury, 1950, Table 19; Martin, et al., 1952, fig. 71).

TOOLS AND WEAPONS USED IN HUNTING AND WARFARE

Although we recognize the fact that many of these tools were used
in several activities, we follow traditional practice in assigning a category
to them, as we did with the construction tools. Projectile points, blades
and even some small oval biface scrapers tend to grade from one category
to the other, so for this reason also we cannot be specific about uses.

PROJECTILE PoINTs

The small triangular lateral notched projectile points (fig. 60, 7-/)
appear to occur consistently late in this sequence as they do in neighboring
areas. The specimens in the collection from the Hooper Ranch Pueblo
and the Thode Site are not uniform in certain details such as the place-
ment of the notches, but as a group they are easily distinguished from the
larger diagonal notched points, for example.

131

Axe-grinding slab from Hooper Ranch

8.
Length, 30.5 cm.

Fic.

Pueblo.

Choppers and large scraper from Tumbleweed Canyon Site, Rim

Fic. 59.
Valley Pueblo, C

men, 8.5 cm.

hilcott Site 1, and Goesling Site. Length of lower right speci-

Y
4

132 PREHISTORY OF EASTERN ARIZONA, I

A similarity may be seen between these small, triangular, lateral
notched points and some from Point of Pines (Wendorf, 1950, fig. 32, b-/;
Breternitz, 1959, pp. 47, 66, fig. 38, &, r) and from the Reserve area
(Martin, Rinaldo, and Bluhm, 1954, p. 125, fig. 64, A-w; Martin, Rinaldo,
and Barter, 1957, fig. 42, f-7; Nesbitt, 1938, pl. 47, B). Furthermore,
although the resemblance is not as close as it is to points from the Mogollon
area, some points from Pueblo III sites in the Anasazi area tend to be
similar instyle (Judd, 1954, p. 255, pl. 73; B, a-e; Roberts, 1932546,
pli 59: a—e)

On the other hand, the projectile points from the earlier sites (fig. 60,
a-d, h) tend to be larger and have barbs which the later points lack.
Although some of these points are lateral notched, more of them tend
to be diagonal notched.

Only five notched or shouldered projectile points (fig. 60, a-d) were
recovered from Tumbleweed Canyon Site, each one of them quite differ-
ent from the others. All are of medium size (3 or 4.cm. long). Two are
diagonal notched, one is corner notched with a broad straight stem and
two have expanding bases with small shoulder-like projections. These
correspond roughly to points from the Pine Lawn Phase (Martin, 1943,
fig. 72, B, fig. 73, E) and from the Circle Prairie Phase (Wheat, 1954,
fig. 54, f, h-k). This scarcity of notched points contrasts markedly with
the number of blades (fig. 61) and bases without notches (42). Many
of these are thin and must have been used as projectile points or knives.
Others are thick and steeply chipped at the edges and may have been
used as scrapers.

ARROW-SHAFT TOOLS

The arrow-shaft straightener (fig. 62, c) is the only one of its kind
recovered. It may be only partly finished inasmuch as the groove is
rough, not polished like the grooves on most tools of this kind. It is made
from a thin rectangular basalt pebble and the groove runs lengthwise
down the middle. It came from the Great Kiva at the Hooper Ranch
Pueblo and is 6.5 cm. long, 5.6 cm. wide, and 1.6 cm. thick.

An arrow-shaft smoother (grooved abrader; fig. 62, @) came from
the same structure. This has a longitudinal groove of the same width
from end to end.

Both of these are simple tools, although broken examples of more elab-
orate types came from the same site (Martin, Rinaldo, and Longacre, 1961,
p. 102). Arrow-shaft tools are usually scarce on sites earlier than the
Tularosa Phase or Pueblo III. They occur predominantly on late pueblo

Fic. 60. Projectile points, miscellaneous types. Length of m, 3.0 cm.

153

134 PREHISTORY OF EASTERN ARIZONA, I

Fic. 61. Blades from Tumbleweed Canyon Site and Hooper Ranch Pueblo.

sites and in a general Upper Gila, Little Colorado, Rio Grande distri-
bution. They are rare even on a late horizon in the neighboring areas
to the north or south.

These tools need not necessarily have been used for shaping arrow
shafts or foreshafts; they could have been used for smoothing prayer
sticks or spindles.

ARTIFACTS 135

HOUSEHOLD UTILITY TOOLS

The tools included in this category are those that probably were used
for several purposes. These include cutting edges such as flake knives,
saws, and scrapers, and perforators such as drills and punches.

FLAKE KNIVES
(Figure 63, c, 7)
Approximately 270 utilized flakes were recovered from the eight

sites. These range from thin flakes with some almost microscopic chipping
along one edge to somewhat thicker flakes with well-defined secondary

Fic. 62. Abrading stones (a, 6), arrow-shaft tool (c), and smooth saw (d) from
Hooper Ranch Pueblo. Length of d, 6.4 cm.

136 PREHISTORY OF EASTERN ARIZONA, I

chipping on one broad surface and along more than one edge. Although
these are far from uniform in shape of outline, they tend to be oblong.
Most of them are made from chert or chalcedony flakes, but there are
some fine-grained basalt, fine-grained quartzite and felsite flakes.

They have diminishing distribution from early to late. Almost half
were recovered from Tumbleweed Canyon Site (122). The Chilcott
Site 1 yielded over a sixth, the Thode Site and Rim Valley Pueblo about
a sixth each, and the Hooper Ranch Pueblo Great Kiva about a twelfth;
the remainder are divided between the three smaller excavations, which
do not seem comparable. This decline in popularity seems to parallel
that which appeared in the areas to the south wherever comparable
information is available (Martin, et a/., 1952, p. 489).

Thin cutting edges were probably used something like our pen knives
for whittling wood (arrow and dart foreshafts, prayer sticks, spindles),
cutting other soft materials (leather, string, fiber), or skinning animals.

SCRAPERS
(Figure 63, a, b, d-1)

Approximately 116 small scrapers were recovered. Although they
were found at all of the sites, the majority of them (64) come from the
Tumbleweed Canyon Site. The next largest group (29) is from Hooper
Ranch Pueblo. These are only a little more specialized in form than
the flake knives. They are small (2.0 to 7.0 cm. long; 1.6 to 5.7 cm. wide),
rough, thick (0.4 to 4.0 cm.) flakes with some secondary chipping at a
steep angle along one or more edges. They are generally plano-convex
in cross section and the convex surface was shaped by percussion chipping.
The available information, though inadequate for a truly accurate esti-
mate, appears to indicate a decrease in these tools similar to that of the
flake knives.

The large scrapers might be classified as scraper-planes. They are
generally plano-convex in cross section and have steep secondary chipping
along one edge. There were not enough of these found to consider the
distribution significant in indicating an increase or decrease in popularity.
They came from both early and late sites: —Tumbleweed Canyon Site (3),
Chilcott Site 1 (4), Rim Valley Pueblo (4), and Hooper Ranch Pueblo,
Great Kiva (1).

Saws
(Figure 64, 7, 7)

These implements are thin flakes with one or more margins chipped
into a series of deep notches to form a serrate cutting edge. Only two of

Fic. 63. Flake knives (c,7) and small scrapers (a, 6, d-7) from Tumbleweed Canyon
Site, Chilcott Site 1, Goesling Site, and Hooper Ranch Pueblo. Length of 7, 5.8 cm.

138 PREHISTORY OF EASTERN ARIZONA, I

Fic. 64. Drills, punches, saws, and blades from Hooper Ranch Pueblo, Goesling
Site, Chilcott Site 1, and Rim Valley Pueblo. Length of 7, 3 cm.

these saws were recovered, one from Hooper Ranch Pueblo, Great Kiva,
and one from Rim Valley Pueblo. This late distribution is in accord
with their occurrence in the Reserve area, where they are found in the
San Francisco Phase at the earliest; even at Forestdale (Haury, 1940, p.
107) they do not occur earlier than the Forestdale Phase. There are some
surface indications that they may occur earlier north of Concho (Bret-
ernitz, 19575 p. 78).

One square-cornered fragment of a smooth saw (fig. 62, d) was
found in the Great Kiva at Hooper Ranch Pueblo. Only enough of the

ARTIFACTS 139

cutting edge remains to enable one to classify it. These tools also occur
primarily in late sites (Rinaldo, 1959, p. 252).

DRILLS
(Figure 64, a, e-h)

A half-dozen drills were recovered from the sites, but only one or two
came from each site. One is the plain-shafted type and the others are
the flanged type. The drills in this latter group have slender points
which taper from broad bases. They average 3.7 cm. in length.

Because drills are one of the less common chipped stone artifacts in
the Southwest—although they are not rare—our present generalizations
on their distribution will be subject to revision. However, they do appear
to be more frequent in the very early levels and sites and relatively less
frequent in the later ones.

WEAVING TOOLS

Evidence seems to indicate that bone awls and bodkins were used
in weaving baskets and in separating the warp and weft elements on
the loom. Molded spindle whorls were, of course, used as a form of
fly wheel on spindle shafts in the process of spinning yarn (Kent, 1957,
pp. 472-473). Some of the more symmetrical worked sherds with holes
bored through their centers may also have served as whorls.

Bone AWLS
(Figure 65)

These implements were recovered from the Goesling Site, the Thode
Site, Rim Valley Pueblo and Hooper Ranch Pueblo. They fall into
four types: (1) the ulna type (fig. 65, &); (2) those made from split long
bones with the condyle unaltered except by the original splitting (fig.
65, a, d, f-1); (3) the same type as No. 2 except that the condyle is partly
worked down (fig. 65, c); (4) awls made from bone splinters (fig. 65, 4, 7, /).

Only the ulna type appears to have a significant distribution. The
only specimen of this type found during the 1960 season comes from the
latest site. Although they have been recovered from earlier sites in
prior seasons, they are more frequent from the later sites (Martin and
Rinaldo, 1960b, p. 229). This was also true in the Reserve area (Rinaldo,
1959, p. 264), and it appears to be the situation at Point of Pines (Wendorf,
1950, pp. 77-79; Wheat, 1954, pp. 159-160; Breternitz, 1959, p. 51).

140 PREHISTORY OF EASTERN ARIZONA, I

The bodkin tip (fig. 65, m) is a broad, flat, blunt point decorated
with an incised zigzag line. It was found in Rim Valley Pueblo. Another
scrap of bone (fig. 65, m) is decorated with a “negative lightning” design
formed by a pattern of incised lines and dots. This was recovered from
Hooper Ranch Pueblo. Art work of a generally similar nature was
seen in a bone efhgy pendant from the dwelling rooms at Hooper Ranch
Pueblo (Martin, Rinaldo and Longacre, 1961, p. 106).

Most of the awls have tips that are round in cross section. Only two
(in addition to the bodkin) have tips that are laterally flat. These may
have been used for a different function than the round pointed awls,
such as plaiting (Di Peso, 1956, pp. 414-415).

SPINDLE WHORLS
(Figure 66)

Two modeled clay spindle whorls (fig. 66, c, d) were recovered from
Chilcott Site 1. These are a gray color and resemble a pulley or a
spool in shape. They are about 3 cm. high and slightly less than that
in diameter. Similar whorls were found at the Los Muertos Site
(Haury, 1945, fig. 71, 7, 7, p. 117); Babocomari Village (Di Peso, 1951,
p. 107, pl. 44, D); Tuzigoot Ruin (Caywood and Spicer, 1935, p. 66,
pl. 15, D); and Snaketown (Gladwin, et al., 1937, p. 245, pl. 212, m).

Sites in the Papagueria of southern Arizona have produced more
modeled clay spindle whorls than sites farther north (Haury, 1950, p. 360)
or in other sections of Arizona, and this culture element is believed to
be of Mexican derivation (Di Peso, 1956, pp. 396-397). Although they
have been found as far north as Flagstaff (McGregor, 1941, pp. 74-76)
they are more common farther south. With the exception of a few speci-
mens from Tularosa Cave in San Francisco levels (Martin, et al., 1952,
p. 196) they generally are late in occurrence.

Ten disc-shaped worked sherds (fig. 66, e, f) perforated through the
center were found. Seven of these came from the Goesling Site, one
from the Thode Site and two from the Hooper Ranch Pueblo Great
Kiva. These are common in pottery-bearing sites throughout the South-
west.

ORNAMENTS

Stone and shell pendants and beads as well as fragments of shell
bracelets and a ring are classified as ornaments. A few small, unperforated
objects of a shape similar to that of the pendants but a little larger possibly
should be included as unfinished pendants. One of the pendants is

Fic. 65. Bone awls, incised bone fragment, bodkin tip and ring material from
Goesling Site, Rim Valley Pueblo, Hooper Ranch Pueblo, and Thode Site. Length
of 0, 6.7 cm.

141

142 PREHISTORY OF EASTERN ARIZONA, I

Fic. 66. Spindle whorls, worked sherds and miniature jar from Chilcott Site 1,
Goesling Site, and Hooper Ranch Pueblo. Length of 7, 11.9 cm.

grooved near one end; the others are perforated near one end. The
beads are all centrally perforated.

None of the ornaments is elaborately decorated or shaped. Incised
designs or even conventionalized zoomorphic shapes are lacking and
only types simple in nature were recovered. On these sites ornaments
were relatively rare or absent. In general they appear to be more plentiful
and elaborate in sites in the southern part of Arizona than they are
in the north.

ARTIFACTS 143

Fic. 67. Pendants, bracelet fragments, and ring fragment from Goesling Site and
Hooper Ranch Pueblo.

PENDANTS
(Figure 67, upper right)

A few tabular pendants were obtained from the digging. ‘Two came
from the Hooper Ranch Pueblo (one of turquoise, one of bone) and
two from the Goesling Site (another of turquoise and one of clam shell).
A fifth pendant, of white limestone, is grooved near one end for suspension.
This came from Rim Valley Pueblo. The bone, shell and white stone
pendants are oblong in shape, and are longer than wide. ‘The
turquoise pendants are almost as wide as they are long. One is roughly
triangular in shape, the other rectangular with rounded corners.

144 PREHISTORY OF EASTERN ARIZONA, I

BEADS

The beads are of two types: small, centrally perforated discs and what
is sometimes termed “‘truncate olivella’” (Morris, 1919, p. 93). All of
these came from the Hooper Ranch Pueblo. Both types have been
recovered from both early and late sites of the Mogollon and Anasazi
cultures.

BRACELETS
(Figure 67, lower)

These specimens are all fragments of the thin type of shell bracelets,
and all came from Pithouse A at the Goesling Site. This type appears
to have an over-all distribution, occurring throughout the Southwest
in both early and late sites and levels. The thick type, which occurred
in a dwelling room at Hooper Ranch Pueblo (Martin, Rinaldo and
Longacre, 1960, p. 45) but not in the excavations made during the
1960 season, appears to be late in its distribution (Gladwin, et al., 1937,
p. 142; Nesbitt, 1938, p. 108).

RINGS
(Figure 67, lower center)

One fragmentary shell ring was found in Pithouse A, at the Goesling
Site, and is the only specimen of this type recovered.

Shell rings are not as common as bone rings in sites north of the
Mogollon Rim. Shell rings have been reported from Pueblo Bonito
(Pepper, 1920, p. 371), Snaketown (Gladwin, et al., 1937, pp. 144-145),
the San Simon Village (Sayles, 1945, pl. 52), Quiburi (Di Peso, 1953,
p. 179), San Cayetano (Di Peso, 1956, p. 95), and Arizona W:10:51
(Wendorf, 1950, p. 89).

Bone RING MATERIAL
(Figure 65, 0)

This specimen is mentioned here as further evidence of the use of
bone rings by the people of Hooper Ranch Pueblo. It is a hollow section
of long bone including a portion of the condyle. A deep groove encircles
the end opposite the condyle. The specimen is 6.7 cm. long and 2.4 cm.
in diameter.

A few rings and several specimens of long bones prepared as ring
material were recovered from the dwelling rooms (Martin, Rinaldo and
Longacre, 1960, p. 50). These rings have been recovered mostly from

ARTIFACTS 145

late ruins south and west of Zuni such as Arizona W:10:51 (Wendorf,
1950, p. 81), Kinishba (Baldwin, 1939b, p. 321), Canyon Creek (Haury,
1934, p. 126), Hawikuh (Hodge, 1920, p. 145), and Pinedale (Haury
and Hargrave, 1931, fig. 16).

TINKLER
(Figure 67, upper left)

A single fragmentary specimen of a conical tinkler was recovered
from the Great Kiva at Hooper Ranch Pueblo. Near the smaller end
there is a notch through which a string could be passed.

Similar conus tinklers come primarily from late horizons after a.p. 1100
and from as far east as Pecos (Kidder, 1932, p. 190), as far west as the
Elden Pueblo near Flagstaff (McGregor, 1941, p. 281), north in the
Aztec Ruin (Morris, 1919, p. 94), and south in the Hohokam sites (Haury,
1945, p. 149; Gladwin, et al., 1937, p. 145), and at San Cayetano (Di Peso,
30,pp. 21-92):

In the upper Little Colorado drainage, they also occurred at Table

Rock Pueblo (Martin and Rinaldo, 1960b, p. 225) in the larger of two
kivas.

Cut SHELL

One very small piece of cut shell with a notched serrate edge was
found at Chilcott Site 1. Cut shell pendants or mosaic pieces with nacreous
surfaces and scalloped or notched edges were recovered at Los Muertos
(Haury, 1945, p. 150) and Snaketown (Gladwin, et al., 1937, p. 142,
pl. 119). Cut shell specimens seem to have a distribution primarily in
the Hohokam area.

CEREMONIAL OBJECTS

Three groups of objects are included in this category: cylinder stones,
the sacred stone image, and some of the worked sherds.

CYLINDER STONES
(Figure 57, upper)

These rough approximately cylindrical objects are made of vesicular
basalt. Five of them were found, three in the Great Kiva at Hooper
Ranch Pueblo, one at Rim Valley Pueblo, and one at the Thode Site,
the latter two in rooms.

146 PREHISTORY OF EASTERN ARIZONA, I

These objects have a distribution that extends from the SU Site
(Martin and Rinaldo, 1940, p. 62, fig. 28) west as far as Tuzigoot (Cay-
wood and Spicer, 1935, p. 86). They are common in the Flagstaff area
(Bartlett, 1934, p. 26; McGregor, 1941, p. 178; Smith, W., 1952a, pp. 127—
129), and occur in the Jeddito area (Woodbury, 1954, pp. 181-182).
They appear to be more common on the earlier horizons than on the
later.

SACRED STONE IMAGE
(Figure 42)

This object is treated at length in Chapter II. Although stone images
of animals, corn mounds, erosion remnants, petrified wood and fossils
have been found frequently in prehistoric sites, anthropomorphic images
apparently were comparatively rare before the Spanish conquest (Fewkes,
1924, pp. 377-397; Martin, et al., 1956, pp. 84, 94). They have been
reported from Pecos (Kidder, 1932, pp. 86-91; Lambert, 1957, pp. 93-
96) and Te’ewi (Wendorf, 1953, pl. 35), but these are the only pre-
historic specimens our search has revealed unless a stone ornament from
Pueblo Bonito (Judd, 1954, fig. 20, 0) is so considered.

WoRKED SHERDS
(Figure 66, a, b, e, f, A, 2)

Most of the 23 disc-shaped worked sherds that were recovered came
from the Goesling Site. One came from the Chilcott Site 2 and one
from the Hooper Ranch Pueblo.

Worked sherds of other shapes—oval, triangular, fragmentary—were
more evenly distributed. Out of 22 specimens in the mixed group,
10 came from the Goesling Site, 8 from Chilcott Site 1, 2 from Rim
Valley Pueblo and 2 from Hooper Ranch Pueblo. These are about 5.0
cm. in greatest dimension.

Throughout the Southwest and in other areas to the south and east,
worked sherds have been found in most sites where pottery has been
recovered.

SUMMARY

The distribution of the stone, bone and shell artifacts generally cor-
roborates certain trends and developments observed previously in both
the excavated and the surveyed sites, but it also adds details to pre-
viously incomplete observations. The following artifact types appear to
decrease in frequency from early to late: (1) one-hand manos, (2) basin

ARTIFACTS 147

type metates, (3) rubbing stones, (4) mauls, (5) drills, (6) barbed pro-
jectile points. A few others appear to increase in frequency from early
to late: (1) long two-hand manos, (2) beveled manos, (3) small triangular
projectile points, (4) trough type metates, (5) bone awls made from ulnas.
A few traits have only a late distribution: (1) arrow-shaft tools, (2)
pot rests, (3) bone rings, (4) shell rings, (4) conus tinkler pendants.
Another small group of traits appears to have come into the area as the
result of trade, gifts, or some other means. ‘These are the modeled clay
spindle whorls and the shell ring, and possibly the three quarters grooved
axe, all of which seem to be southern in origin. Stone cylinders and
stone disc-shaped pot covers could have been northern elements, although
they appear in much greater frequency than the former traits and prob-
ably were more completely accepted into the local culture.

On the whole, though, the basic tools of the culture such as the
manos, metates, choppers, scrapers, flake knives, and projectile points
continued in use throughout the sequence of the upper Little Colorado
culture and were subjected only to a slow process of modification.

VIL. Archaeological Reconnaissance

in Eastern Arizona

By WitxirAM A. LONGACRE
Field Assistant

INTRODUCTION

An archaeological surface survey under the auspices of the National
Science Foundation was conducted in east-central Arizona as part of
the 1960 Southwest Expedition of Chicago Natural History Museum.
This investigation extended the survey begun in the previous year.
During the two seasons more than 5,000 miles were covered by truck,
and an intensive reconnaissance of approximately 50 square miles was
made on foot. As a result, 170 new sites were discovered.

In 1959, work was concentrated in the valley of the Little Colorado
River from St. Johns to Springerville and in a large triangular area
outlined by Highways 60 and 61 as they merge east of Show Low, the
right side of the triangle being Highway 666 between Springerville
and St. Johns. In addition, some time was spent in the foothills of the
White Mountains south and west of Springerville, and in the region near
Snowflake and Mesa Redonda.

In 1960, the survey concentrated upon the Snowflake—Mesa Redonda
region and the White Mountains south of an imaginary line drawn be-
tween Show Low and Springerville. Further reconnaissance was carried
out in the Little Colorado River Valley between St. Johns and Springer-
ville, and in the area surrounding Show Low.

The region investigated in this survey (fig. 68) occupies a portion of
the Colorado Plateau in east-central Arizona. It includes part of the
upper drainage of the Little Colorado River and portions of several
of its tributaries. It is roughly outlined by parallels 34° 30’ on the north
and 34° 20’ on the south, with meridians 109° 20’ and 110° the eastern
and western boundaries, respectively. The topographical and ecological
setting of the survey area has been described elsewhere (Martin, Rinaldo,
and Longacre, 1961, pp. 150-153).

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150 PREHISTORY OF EASTERN ARIZONA, I

ORGANIZATION

As in the report prepared on the 1959 survey (op. cit.), the following
terminology has been used:

A site is defined as an area used by prehistoric peoples as indicated
by cultural detritus. This rather inclusive definition would include areas
of occupation ranging from small camp-sites with no evidence of archi-
tecture to large above-ground structures of more than 100 rooms.

It was decided to record each site only once, and later each site:-was
broken down into occupational components and labled ‘“‘a,”’ “‘b,”’ “‘c,”’ etc.,
on the basis of the pottery analysis. When this was done, the 107 sites
recorded during the 1959 season expanded to 154 temporally different
components, and the 63 sites found during the 1960 season, to 89 com-

ponents.

Presentation of the material in a temporal framework presented a
problem. The Pecos Classification proved to be unsatisfactory because
it was too general. The discrepancy between time and cultural inclusion
in it is recognized. The system of phase-designation is now accepted
by most archaeologists in the Southwest and therefore would be the
ideal way to present this report. Information gained from excavation,
however, is relatively incomplete in the surveyed area, and I could
not justify an attempt to assign phases.

I decided to present the material in the form of rough time periods
based upon admittedly arbitrary “‘groups,’ with dated pottery types
or the absence thereof as the delimiting factors. It is hoped that the
presentation of the material in this manner will better facilitate a later
incorporation into future archaeological studies within the area.

The use of the term “group” here does not connote the exact meaning
that Colton gave ‘‘Ceramic Group” (Colton, 1946, pp. 18-20). Below
is a list of groups, pottery types included, and tentative dates:

Group I.—Pre-pottery: absence of pottery, stemmed projectile points
with concave bases, various stone tools such as choppers, scrapers,
and knives. Dates: 2000 B.c.—a.p. 500.

Group II.—Pottery: Plain Wares (Alma Plain and Lino Gray).
Dates: A.p. 500-700.

Group III.—Pottery: White Mound Black-on-White, Kiatuthlanna
Black-on-White, and Red Mesa Black-on-White. Dates: A.p. 700-
900.

Group IV.—Pottery: Reserve Black-on-White, Snowflake Black-on-
White, Wingate Black-on-Red, and Show Low Black-on-Red.
Dates: A.p. 900-1100.

ARCHAEOLOGICAL RECONNAISSANCE 151

Group V.—Pottery: Tularosa Black-on-White, St. Johns Polychrome.
Dates: a.p. 1100-1300.

Group VI.—Pottery: Zuni Glazes, Pinedale Polychrome, Pinedale
Black-on-White. Dates: a.p. 1300-1500.

FIELD PROCEDURE

Each site visited was given a survey number. A random collection
of pottery and/or artifacts was made. The site was carefully described
as to its extent, condition, topographic-geographic setting, and spatial
location. The pottery and artifacts were sorted and, where possible,
placed into described types and counted. All the above information was
entered on “Site Cards.” The collections and cards for each site are
available in the Department of Anthropology, Chicago Natural History
Museum. The pottery counts, analyses, and counts of artifacts along
with a description of each site found in 1959 and 1960 are published on
micro cards (Martin, Rinaldo, and Longacre, 1960; Martin, Rinaldo,
Longacre, and Freeman, 1961).

TEMPORAL-SPATIAL OCCUPATION OF THE
SURVEYED REGION

The combined findings of the two seasons are outlined below on the
basis of geographical location and the “‘group” affiliation of the com-
ponents or sites. A total of 243 components was found, broken down as
follows:

Little Colorado River Valley:

112 Components located:
11 Pre-pottery (Group I)
8 Plain Ware (Group II)
30 Early Black-on-White (Group III)
40 Reserve Black-on-White (Group IV)
19 Tularosa Black-on-White (Group V)
4 Zuni Glaze (Group VI)

**Triangle”’:
27 Components located:
11 Pre-pottery (Group I)
4 Plain Ware (Group IT)

5 Early Black-on-White (Group ITT)
4 Reserve Black-on-White (Group IV)

152 PREHISTORY OF EASTERN ARIZONA, I

3 Tularosa Black-on-White (Group V)
0 Zuni Glaze (Group VI)

Snowflake—Mesa Redonda

67 Components located:
10 Pre-pottery (Group I)
2 Plain Ware (Group II)
16 Early Black-on-White (Group IIT)
26 Reserve Black-on-White (Group IV)
13 Tularosa Black-on-White (Group V)
0 Zuni Glaze (Group VI)

Show Low Area:
13 Components located:

5 Pre-pottery (Group I)
3 Plain Ware (Group II)
2 Early Black-on-White (Group ITT)
1 Reserve Black-on-White (Group IV)
0 Tularosa Black-on-White (Group V)
2 Zuni Glaze (Group VI)

White Mountains:
24 Components located:

0 Pre-pottery (Group I)

0 Plain Ware (Group IT)

7 Early Black-on-White (Group III)
14 Reserve Black-on-White (Group IV)
3 Tularosa Black-on-White (Group V)
0 Zuni Glaze (Group VI)

SITE LOCATIONS

Key To Tastes 14-20

Numbers refer to number of sites or components in the designated area, located in
each topographic position.

Letters refer to the position of the site:

A=on mesa top

B=on “tier” or “bench” on side of mesa

C=knoll or ridge on flat in valley

D=on valley floor, on flat

E=bluff or point of land jutting into the valley

F=on knoll or hill in high area or uplands

G=on shore of presently dry lake

H=“‘cliff dwelling”

ARCHAEOLOGICAL RECONNAISSANCE 153

Tas_Le 14.—GROUP I: PRE-POTTERY (2000 B.c.—a.p. 500)

A B (@. D E F G H Total

Little Colorado River Valley.... 0 3 + 1 1 2 0 0 11
pa et) | aha RM Weer le ea ns 0 3 2 2 1 2 0 0 11
Snowflake—Mesa Redonda...... 2 2 2 3 1 0 0 0) 10
Show leowwArea tng, gered an 1 0 0 0 0 0 4 0 5
White Mountains... 8 ont.08 2s 0 0 0 0 0 0) 0 0 0
Ota es niott conte rg 3 8 9 6 3 4 4 0 257)

Tasie 15.—GROUP II: PLAIN WARES (a.p. 500-700)

A B C D E F G H Total

Little Colorado River Valley.... 0 1 2 3 2 0 0 0 8
rein Gi raters 88, on Sys AWS exes (0) 2 1 1 0 0 0 0 4
Snowflake—Mesa Redonda...... 1 0 0 0 0 0 0 1 2
Shaw oOweArediiss) seen eae 2 0 0 1 0 0 0 0 3
Wihite Mountaims....°... 02.0.5. 0 0 0 0 0 0 0 0 0
scstale ett ete ee oe ees 3 3 3 5 2 0 0) 1 17

TasLe 16.—GROUP III: EARLY BLACK-ON-WHITES (a.p. 700-900)

A B c D E F G H Total

Little Colorado River Valley.... 1 1 9 90 0 0 0 30
OL RARIELCLC Aes. Nahas Feu Nees, ae, Sate 0 5 2 0 0 0 0 0 5
Snowflake—Mesa Redonda...... 0) 0 12 2 2 0 0 0 16
OW IUOWHATEA:: ta.5 cr oce oct bie adie 0 0 1 0 1 0 0 0 2
White Moutttains, sii. ecco 0 0) 5 0 1 1 0 0 hi
=) 3) 2a RRR Rey SRE el rie er ie ere age 1 Ain 20 11 14 1 0 0 60

Tas_e 17.—GROUP IV: RESERVE-SNOWFLAKE BLACK-ON-WHITE
(A.p. 900-1100)

A B C D E F G H Total

Little Colorado River Valley.... 0 Za 64 ede 1 0 0 0 40
REMI L a pinata Sai fis cule gehix fe 0 2 2 0 0 0 0 0 4
Snowflake—Mesa Redonda...... 1 Os 22, 6) 0 0 0 0 26
PUT ONIN Aen gh vn stipe nc as nv 0 0 0 0 1 0 ) 0 1
WY ite Montag. .Uoii5-saik'e A vcaca-s 0 0 9 0 1 4 0 0 14
gales | Ieee ag oe en ne? 1 Ata TAs 1A 4 0 0 85

154 PREHISTORY OF EASTERN ARIZONA, I

TasLe 18.—GROUP V: TULAROSA BLACK-ON-WHITE
(a.p. 1100-1300)

A B C D E F G H Total

Little Colorado River Valley.... 0 A gilsl 0 6 0) 0 0 19
*“rlanglec al okie eon ores 0 2 1 0 0 0 0 0 3
Snowflake—Mesa Redonda...... 0 0 13 0 0 0 0 0 13
Show low Aredian oe ee 0 0 0 0 0 0 0 0 0
Wihites\iountams: so) oo eee 0 0 1 0 0 2 0 @) 3
“Lotal 22 atest oot eee 0 4 26 0 6 2 0 0 38

TasBLe 19.—GROUP VI: ZUNI GLAZES (a.p. 1300-1500)

A B CG D E F G H Total

Little Colorado River Valley.... 0 0) 3 0 1 0 0 0 4
eriang leu. Gy ars, uate ah ers bey oy. 0 0 0 0 0 0 0 0 0
Snowflake—Mesa Redonda...... 0 0 0 0 0 0 0 (0) 0
Showdiow Area: - i eeeneee 1 0 0 0 0 0 1 0 2
White Mountains2*..2.%.-2....- 0 0 0 0 0 0 0 0 0
otal so te ee 1 0 z 0 1 0 1 0 6

TasLe 20.—LOCATIONAL PREFERENCES FOR THE ENTIRE

SURVEYED AREA

Number of

Position Components
Yee ees ee Sere ee RAR cre eR LA are casa eu toa 9
Bisa ceo ere Aare ee Ra Le ee ee ete DS
Re ae re nero, oe eRe hein eta Are 119
1D Se errant ce tirin eo oP cin eae tet n.d ch tae tos et 36
| ES a ese IES MEET en Mee rank, oe ee aes AS 39
TFRs gs ccen eae ayaa h vant ee ica oin te aeAD e a 11
Goats Pia Sao ee oa Ee TE eet ree 5
Ls Ree rik a An nin Seem Ache Watiny oat 1

ARCHAEOLOGICAL RECONNAISSANCE 155

In summary, the pre-pottery peoples in this region lived high up
on the sides of mesas on “‘tiers” or ‘“‘benches,”’ on knolls or ridges down
in valleys, or on the flat bottom lands. The earliest pottery-making
peoples (Group II) lived on the valley floor or on knolls in the valley,
on “‘tiers’’ on the sides of mesas, or on mesa tops. The people making
the earlier black-on-white pottery (Group III) show a definite preference
for knolls or ridges down in the valleys as favorable sites for their villages,
as do the later peoples in the area (Group IV through Group VI). Out
of a total of 243 components found in the region, 119 were located in
this topographic position, the home-site definitely preferred by the pre-
historic inhabitants of the area.

GENERAL SUMMARY

The earliest cultural evidence for the occupation of the area consists
of open sites, probably the scene of impermanent camps, indicated by
a scattering of stone tools. These sites occur along the shores of presently
dry lake beds, on knolls and ridges down in valleys, and high up on flat
areas on the sides of mesas. Two sites, both located on the beaches of
playas, were excavated by the Museum in 1958 (Martin and Rinaldo,
1960a). Martin and Rinaldo report a C14 date for one of these sites
(Laguna Salada) as ca. 3200 years ago. The other site (Little Ortega
Lake) may be older (op. cit., p. 115). No indications of permanent
architecture were found.

The artifacts found at the Beach Sites (op. cit., pp. 12-34) are some-
what similar to those which were collected on the surface reconnaissance.
Many of the sites had basin-type metates and pebble-type, one-hand
manos on the surface. In addition, quantities of stone tools, bifacially
worked scrapers, flake knives, and projectile points were collected. The
most sensitive indication of the cultural affiliations of this pre-pottery
material appears to be the projectile points. A wide range of forms was
found, but the presence of stemmed, indented-base types at many of
the sites provides some clue as to the affinities. This particular style of
projectile point evidently has a wide distribution over the Southwest.
It appears to be associated with the Desert Culture (Jennings, 1957)
and is reported at a number of early sites. The general style of the point
has been ascribed names by several authors reporting on widely separated
locations: The Pinto Point (Campbell and Campbell, 1935, pl. 13),
San Jose Point (Agogino and Hester, 1956, pp. 9-12), and Amargosa II
Points (Haury, 1950, fig. 61). Those found at Tularosa Cave (Martin,
et al., 1952, p. 497) are also examples.

156 PREHISTORY OF EASTERN ARIZONA, I

The pre-pottery material in this area of eastern Arizona has been
described as the Concho Complex (Wendorf and Thomas, 1951), based
on surface collections at a number of sites. Wendorf and Thomas ascribe
the majority of the Concho materials to the California desert cultures
with closest affinities to the Amargosa II component at Ventana Cave
and the Pinto Basin materials in California (op. cit., p. 107). Martin
and Rinaldo, basing their suggestion on the assemblage of implements
found at the Beach Sites, feel that the material has affiliations with those
described for the San Jose, Concho, and Cochise industries (Martin
and Rinaldo, 1960a, p. 115).

The material collected during the past two field seasons by the South-
west archaeological expedition of the Museum can add little to this
description. The sites are relatively small in area, ranging from 100
square feet to several thousand square feet, and they occur sporadically
thoughout the surveyed area. The implements suggest an economy based
upon collecting wild plant foods and hunting. This generalized Desert
Culture pattern seems to persist until some time after the beginning of
the Christian era.

Several qualifications are mandatory before presenting a description
of lithic materials from the pre-pottery sites.

First, almost all the pre-pottery sites in the sample have been visited
by local collectors over a period of years. Numerous trips to these sites
by collectors have resulted in rather large collections, and this fact may
possibly explain the relatively small number of projectile points and other
stone tools in our collections. For this reason, our sample of the surface
materials from these sites is incomplete.

Second, an increasing understanding of the material aspects of the
Desert Culture is a result of the excavation of dry caves in the Basin area.
Danger Cave (Jennings, 1957) is a prime example. We are beginning
to appreciate the role of stone tools in the assemblage. Unfortunately,
the surface sample for the surveyed area is restricted to open sites from
which we have only lithic material. The inadequacy of this sample (see
above) indicates a serious sampling error which is compounded by the
very nature of the minute fragment of the total material culture that our
collections encompass. Jennings (op. cit., p. 279) pointedly describes
the problem when he suggests that ‘‘. . . flint was cheap, expendable
and unimportant, whereas cordage, basketry, buckskin, bone and horn
tools, handles, arrows all represented greater skill, a greater expenditure
of effort, and had actually a higher practical and investment value than
did the stone. If flint were thus cheap one wonders how important it
was. How valid are detailed reconstructions of culture history based on
flint typology?”

ARCHAEOLOGICAL RECONNAISSANCE 157

Thus, on at least two counts, our sample is handicapped. In the
face of this problem, artifacts were classed into rather broad functional
classes: manos, choppers, projectile points, scrapers, and so on. These
were further divided on the basis of shape, size, and technique of manu-
factor. The results are summarized (figs. 69-74). For a more compre-
hensive view of the pre-pottery lithic materials of the Concho Complex,
see Martin and Rinaldo (1960a, pp. 12-34), Wendorf and Thomas
(1951), Thomas (1953), Breternitz (1957).

By a.p. 300 several important changes evidently had occurred in the
area. Settlement was somewhat more permanent. One site, the Tumble-
weed Canyon Site, was excavated by the Museum in 1960 (see Chap. I,
p. 19). Three shallow pithouses and three associated storage pits were
dug. The site was on an easily defended mesa with boulder walls aug-
menting the natural defensive character of the location. The paleo-
pollen analysis (Chap. VIII) indicates that these people had corn, although
it is felt that the corn served as an augmentation to the wild plant foods
gathered in the area, rather than a staple. Slight changes in the stone
artifacts are also noted. The manos and metates are, in general, similar
to those found on earlier sites. The projectile points show the preference
of these people for notched forms. The remainder of the stone material
is somewhat similar to that reported from the earlier sites with one ex-
ception, the presence of a new tool, a pestle found in one of the houses
(Chap. VI, p. 122).

Several pre-pottery sites located by the survey showed evidence of
rock-outlined pithouses. The lack of any sensitive indication that these
sites are as late as the Tumbleweed Canyon Site, compounded by the
fact that when these houses do occur they are associated with early sites
of the general Concho Complex, leaves us in a quandary as to the num-
bers and nature of these relatively late pre-pottery sites. No parallels
to this situation could be found in the literature. There are some rough
similarities between the Tumbleweed Canyon Site and the Flattop Site
(Wendorf, 1953) such as the small size of the houses and the presence of
basin metates, and some resemblance in the chipped stone artifacts found
at the two sites, but the differences (presence of pottery at the Flattop
Site as well as lateral entrances to the houses, rectangular manos and
troughed metates) appear to outweigh the similarities. It is interesting to
note that these two sites are located in the same drainage (the Little Colo-
rado River) and are probably more or less contemporary.

About 300 years after the occupation of the Tumbleweed Canyon Site,
the area was occupied by pottery-making people who lived in pithouse
villages. At this time, two types of pottery were introduced as part of

Fic. 69. Projectile points from pre-pottery sites. Point in upper left (broken)
2 cm. long.

Fic. 70. Miscellaneous tools from pre-pottery sites. Top row, left, scraper (con-
cave-convex in cross section), 4.2 cm. long. Remainder of top row, flake knives.
Middle row, drills or perforators. Bottom row, blade fragments.

158

ARCHAEOLOGICAL RECONNAISSANCE 159

two distinct cultures. One group of people, with cultural ties north of
the area, was making an unslipped gray ware (Lino Gray), and another

Fic. 71. Scrapers and utilized flakes from pre-pottery sites. Upper left, scraper
3.5cm. long. ‘Top row, three on left, bifacially worked scraper knives; three on right,
end scrapers. Second row, side scrapers. Bottom two rows, utilized flakes.

group was making an unslipped brown ware (Alma Plain). In many
respects these two cultures shared a similar way of life. Both groups
lived in small pithouse villages containing from three to ten or more
houses each. They were agricultural peoples, probably by this time de-
pending for most of their food on their own crops augmented by natural
plant foods and the products of hunting.

The villages of the people utilizing the gray pottery were concentrated
in the northern and eastern portions of the region. ‘The sites yielding
brown pottery were concentrated in the northern and southern reaches
of the survey. On most of the sites with Lino Gray pottery, traces of
Alma Plain appear as intrusive trade pottery, and the Brown Ware sites
show traces of Lino Gray.

160 PREHISTORY OF EASTERN ARIZONA, I

Fic. 72. Scrapers from pre-pottery sites. Specimen at upper left, 4 cm. long.
Top row, plano-convex scrapers or ‘‘pulper-planers.’”? KRemainder, bifacially worked
scrapers showing variation in size and shape.

The following occupations of the area are not as easily understood as
the above. It is felt that the people who made the brown pottery might
represent either a direct migration from the Mogollon centers to the
south and east, and consequently represent a hybrid culture, or more
probably mirror strong Mogollon influence as the result of culture con-
tact and acculturation on the part of indigenous populations. The people
who made the gray pottery seem to be closely allied with the Anasazi to
the north.

The period beginning at approximately A.p. 700 is characterized by
an increase in both the number of sites found and the individual size of
each site. It is felt that this may be an indication of a population increase
which was relatively sudden, and judged from the nature of pottery and
other artifacts from sites occupied at this time, was markedly Mogollon
in character. From this time on, in fact, the nature of the prehistoric
occupation of the area is dominantly Mogollon. Brown utility wares are
found from this period through the latest sites we record in the region.

ARCHAEOLOGICAL RECONNAISSANCE 161

At least in the eastern portion of the surveyed area, the painted pottery
is closely allied with the painted series worked out for the Mogollon in
Pine Lawn Valley by Martin and Rinaldo. The analysis of stone arti-
facts appears to substantiate the pottery evidence.

Through time, the sites became larger, the pottery and artifacts more
complex and sophisticated, and the people more numerous. By a.p. 1200,
a significant bifurcation of culture appeared within the limits of the sur-
vey. In the east, especially in the valley of the Little Colorado River,
the Mogollon tradition was culminating in very large pueblo villages,
some with pan-village or inter-village rectangular Great Kivas. The
pottery was colorful, some decorated with glaze paints. One can follow
a Mogollon sequence in design style in an unbroken line from some of

Fic. 73. Large bifacially percussion-flaked scrapers/choppers from pre-pottery
sites. Specimen at upper left, 6.5 cm. in length.

162 PREHISTORY OF EASTERN ARIZONA, I

Fic. 74. Choppers and manos from pre-pottery sites. "Top row, choppers. Bot-
tom row, pebble-type ‘“‘one-hand”’ mano and mano fragment. Specimen at upper left,
8.5 cm. long.

the earliest black-on-white styles through the glazes. In the western
portion of the area, however, a somewhat different pattern seems to
emerge. Here, centered in the area north and west of Mesa Redonda,
near the modern town of Snowflake, cultural remains reflect differences
in the ceramics as well as major differences in ceremonial architecture
compared to those found in the Little Colorado River Valley. Circular
Great Kivas make their appearance in this locale—the only time and
place in the entire surveyed area with one exception. A circular Great
Kiva was excavated by the Museum at the Mineral Creek Site in 1959
(Martin, Rinaldo, and Longacre, 1961). The circular Great Kivas
located near Snowflake are associated with large pueblo villages, just as

ARCHAEOLOGICAL RECONNAISSANCE 163

their rectangular counterparts are in the east. The circular kiva seems
to be an Anasazi trait. Thus one is faced with the problem of explaining
the circular kiva among a people who seem in other respects to be strongly
Mogollon in nature. The dominant decorated pottery type at this period,
also, does not seem to fit into a Mogollon pattern. Here, design ele-
ments made up of balanced and opposed solids are most abundant in the
ceramics. In the eastern portion of the surveyed region at roughly the
same time, the Mogollon Reserve—Tularosa series with design elements
made up of solids and hachured scrolls is the preference. Small quanti-
ties of intrusive Anasazi trade pottery (Tusayan White Ware), almost
identical in design style with the locally made pots, were recovered on
sites in the Snowflake region. ‘This fact, along with the architectural
evidence, leads one to suspect Anasazi influence in this small portion of
the surveyed area. The presence of Mogollon brown utility wares in this
area in conjunction with the seemingly Anasazi nature of much of the
Snowflake sub-culture is one of the many intriguing complexities that
must be explained.

CONCLUSIONS

My task now is to present an interpretative synthesis for the sequence
of prehistoric events in this region.

The earliest occupants of this area appear to have been small groups
of nomadic intensive collectors. Primary subsistence of these groups was
probably based upon collecting wild plant foods augmented by hunting.
The known material culture indicates a generalized Desert Culture adap-
tation to the environment. The distribution of sites may indicate a
seasonal round of settlement, probably based upon the harvest cycle
of various plant foods. I would suggest that the open unsheltered sites
might have been occupied during the warmer months, probably utilized
for short periods of time in the collecting activities of these groups.

Location of these sites probably depended upon availability of water
and proximity of a food source. Examples of these locations would be the
sites in the lower elevations of the area such as the Beach Sites. More
sheltered locations such as those sites at the bases of cliffs or on ‘‘tiers”
on the sides of mesas may represent sites occupied during colder periods.
The figures on site locations (p. 154) indicate roughly three times as
many sites in a rather unprotected spot as those which incorporate natural
shelter in their location. This would be the expected pattern in the
seasonal round. Regular movements to new collecting areas as harvests
ripened, probably returning to favored camp areas, would result in a
number of frequented sites occupied during the collecting season. Fewer

164 PREHISTORY OF EASTERN ARIZONA, I

naturally sheltered sites may simply reflect the same population in a
smaller number of stable wintering camps. Evidence for the periodic
occupation of a favored site can be seen in the several styles of projectile
points present at each of the excavated Beach Sites (Martin and Rinaldo,
1960a, pp. 24-29). These types may represent the style preferences in
projectile points in different periods of time among the people utilizing
the beach locations as camping spots. One might expect such style
changes, considering the fact that the periodic occupation of such favored
sites probably took place over a period of several hundreds of years.

Apparently none of the sites of this early period was selected with
an eye to defense. Clearly most of them are in unprotected locations
which would be most difficult to defend. The sites which are high on
the sides of mesas were set against the base of a cliff. In all cases, the
the tops of these cliffs are easily accessible. Several large rocks dropped
from above would underline the indefensive nature of such locations.

This pattern of settlement location is not shared with sites of this
early time period in neighboring areas to the east and southeast. Danson
(1957, p. 103) reports a defensive character for ‘‘pre-Pueblo I”’ sites
in the area east of the Vernon region. Bluhm (1960, p. 541) reports
a similar pattern in her summary of the settlement patterns of the Pine
Lawn area.

The combined data of settlement pattern and material culture suggest
some sort of band socio-political organization for the peoples of this period.
If my speculation on the seasonal round of collecting for these groups is
well-founded, I may then suggest a system of defined territoriality for
each social group. Perhaps there was economic co-operation among
bands in such things as large seed harvests or rabbit or antelope drives.

This Desert Culture pattern proceeded with great continuity for at
least two thousand years. The earliest date for material in our area is
ca. 1550 B.c. It is probable that this material has even greater antiquity.
The pattern continues until some time after the the birth of Christ. The
earliest date thus far on major modifications of this generalized Desert
Culture Base is approximately A.p. 275. These major modifications are:
the beginnings of agriculture in the area, the first appearance of houses,
settlement definitely oriented toward defense in one part of the region,
the development of preserving and storage techniques, and relatively
permanent settlement. This period of great change is exemplified in the
Tumbleweed Canyon Site.

We feel that these changes reflect the acceptance of foreign
exploitive-adaptive methods for subsistence on the part of the indigenous
peoples. These techniques probably were introduced from the Mogollon

ARCHAEOLOGICAL RECONNAISSANCE 165

area to the south or southeast. The beginnings of agriculture (raising
corn, probably along with beans and squash), combined with the technical
knowledge of preserving and storing surplus foodstuffs, would have allowed
relatively permanent settlement and an increase in population, and would
have increased the time available to both sexes as their production
techniques were refined. An agricultural base would also have provided
the aged and young with a role in food production not present for them
in a collecting-hunting economy. This would have appeared in their
usefulness in tending the growing crops, in the harvest, and in preparation
of the foodstuffs for storage.

In the Tumbleweed Canyon site we have probably captured these
far-reaching changes in a relatively early portion of their introduction.
The people who occupied the site probably still depended heavily upon
natural plant foods for their subsistence. The assemblage at this site
reflects close ties with the material culture of the Concho Complex.
In these respects the data from the Tumbleweed Canyon site suggest
great continuity with the past. In the additions to this Concho Complex
Base can be seen the complex changes foreshadowing the later prehistory
of this particular area of the Southwest.

The defensive nature of this site presents a problem of explanation.
The defenses were much too elaborate to be explained by a fear on
the part of these people of wild animals robbing their stored foodstuffs.
It may be better explained by a fear of other people. This, of course,
raises the problem of identifying these unknown peoples. There are
two possibilities: These people are either local groups, similar to those
who occupied Tumbleweed Canyon, or they are people from some-
where outside the area.

The data I have at present suggest that the unknown people referred
to above were not local and that the defensive nature of the Tumbleweed
Canyon Site was in response to foreign peoples. If I assume that sites
of this period are those with small, rock-outlined pithouses and lacking
pottery, then there are very few sites and a small population. All other
sites with pre-pottery pithouses that have been located thus far have not
been defensive in nature. They occur on locations of earlier Concho
Complex sites. If I postulate a group of liberal people accepting such
radical innovations as corn agriculture and permanent settlement, sur-
rounded by conservative groups maintaining a Desert Cultural pattern
with local friction aroused to a point of conflict, it is difficult to explain
the non-defensive aspects of these other sites.

The very presence of exploitive techniques foreign to this area indicates
contact on some level with outside peoples. The suggestion that these

166 PREHISTORY OF EASTERN ARIZONA, I

unknown peoples were from some other area raises the problem of the
nature of this encroachment. Were they moving into the area to establish
villages? No evidence was discovered that would indicate foreign peoples
were settling in the area at this time.

Do we have evidence suggesting that foreign peoples were passing
through the area? The evidence at hand does suggest that the defensive
nature of the Tumbleweed Canyon Site was in response to a threat pre-
sented by exotic peoples passing through the area and utilizing the
Little Colorado River Valley as a natural route of travel. This hypothesis
is supported by the non-defensive nature of the other sites of this period.

All are located away from the valley itself, in the area designated
as the “‘triangle’’ (Martin, Rinaldo, and Longacre, 1960, pp. 174, 176).
These sites are far from the major route of travel that the valley was
to become and probably was, to an extent, by this early period. The
threat presented by outsiders passing through would not have been felt
by the groups removed from the valley itself, but they were able to
benefit from the innovations that such outside contact provided. The
advantages of living on the edge of a well-watered and fertile valley
such as the Little Colorado Valley probably was, evidently outweighed
the negative aspects of such a location.

After this inital period of new exploitive techniques, the peoples of
the area began to add new items to their culture and expand and refine
older techniques. Deeper and larger pithouses were constructed, the
art of ceramics was learned, and expanding agriculture allowed for an
increased population.

For the first several hundred years after the Tumbleweed Canyon
Site was occupied, both Anasazi and Mogollon ideas were filtering into
this area. By a.p. 800, however, the pattern began to assume an ever-
increasing Mogollon character which it never lost.

By a.p. 800, fairly large pithouse villages were in the region, with
a firm agricultural base. By A.p. 1000, population had greatly increased
and some peoples were living in above-ground pueblo units. The next
several hundred years saw the number of villages decrease, but the
individual size of each greatly enlarge. This pattern continued, eventually
culminating in the large pueblos in the region by A.p. 1350. Beginning
about A.D. 1000 new settlements were made only on major waterways
such as the Little Colorado, and the rugged portions of the region such
as the “triangle” were abandoned. By a.p. 1350, the only permanent
settlements in the area were either along the Little Colorado itself, or
Silver Creek. one of its tributaries.

ARCHAEOLOGICAL RECONNAISSANCE 167

There are many questions that could be raised, but at this stage in
our knowledge they are not answerable. Future archaeological work
in this region should clarify such problems, many of which we do not
even recognize. We shall have to refine the chronology and enlarge
our comprehension of the cultures of the area in order that we may be
able to seek answers to such basic questions as: What is the role of
this region in the contacts between the Mogollon to the south and the
Anasazi to the north? What significance does this area hold for an
understanding of the late development of Zuni and Hopi cultures? Is
there any information in this sequence which may aid our understanding
of the Salado Culture to the south and southwest?

VIII. The Pollen Analysis of Eighteen

Archaeological Sites in Arizona and New Mexico

By JAMES SCHOENWETTER

Department of Anthropology, Southern Illinois University

ACKNOWLEDGMENTS

This project was initiated through funds given by the National Science
Foundation (Grant No. G13039).

The Geochronology Laboratories of the University of Arizona allowed
me use of the facilities of its palynological laboratory and gave generously
of the time and experience of its staff in checking the results and inter-
pretations presented in this report. To Professor T. L. Smiley and Dr.
Paul S. Martin of this laboratory grateful thanks are tendered for the
supervisory roles they have accepted.

The Department of Botany of Southern Illinois University, through
the generosity of its chairman, Dr. Walter B. Welch, lent a research
microscope to the project.

The Department of Anthropology of Southern Illinois University
allotted office space and facilities which made the progress of the research
a far smoother operation than might otherwise have been the case.
To the members of the staff of this department and to the members
of the staff of the Museum at Southern Illinois University, especially
Dr. Walter W. Taylor and Professor P. Armillas, I wish to express my
appreciation for their patience in reading this report in manuscript and
for their courteous and helpful suggestions.

INTRODUCTION

The archaeologists’ interest in pollen analysis stems from their recent
tendency to place greater emphasis on the relationships between culture
and environment when analyzing prehistoric remains. This has par-
ticularly stimulated palynological research, which has been carried on
in association with archaeological research in the arid Southwest over

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POLLEN ANALYSIS 169

the past few years. The results of some such pollen studies, however,
are as yet unpublished, since they can best be interpreted only after
thorough analysis of the accompanying archaeological materials. When
this project was being formulated it was realized that pollen studies
undertaken upon archaeological sites which were already well described
would yield information which could be more quickly disseminated and
perhaps most relevant to the question of the nature of the relationships
between culture and environment.

Over the past twenty years Chicago Natural History Museum has
excavated and reported upon an impressive number of sites in eastern
Arizona and western New Mexico. These sites encompass a respectable
span of time and allow a rather substantial basis for discussing the single
culture they represent: the Mogollon. It was natural, then, to attempt
the pollen analysis of such well-known sites as the SU Site, Wet Leggett
arroyo, the Promontory Site and Higgins Flat Pueblo in the Pine Lawn,
New Mexico, area; and also to investigate Site 30, Table Rock Pueblo
and others in the area around Vernon, Arizona.

The major objective of this research project was the development
of a pollen chronology for the eastern Arizona—western New Mexico
area north of the Mogollon Rim. We hoped that this would date and
allow a comprehension of such environmental fluctuations as may have
occurred. This objective has been essentially fulfilled, for the pollen
analyses of many archaeological sites showed sufficient regularity to sup-
port the construction of such a pollen chronology. A close degree of
fit can be shown between this chronology and other pollen and dendro-
logical chronologies from the arid Southwest. When the pollen chronology
is fully developed, a valuable stratigraphic tool will be available to the
archaeologist interested in this region.

The final objective of the study was the investigation of whatever
aspects of the relationship between culture and environment were made
manifest in the course of the work. As an adequate reconstruction of
the environment of the area investigated can be made for different time
levels, a discussion of the relationships between the environmental changes
evident in the pollen record and the cultural changes evident in the
archaeological record will be presented. It is recognized that this is an
interpretation of the evidence, but the result is considered as a testable
hypothesis for future research.

Some of the interpretations in the following pages may be chal-
lenged, and further work may uncover errors, gaps and misorientations.
I have attempted to demarcate clearly evidence, conclusions from the
evidence, and interpretations based on these conclusions. However, I

170 PREHISTORY OF EASTERN ARIZONA, I

hope that the work will be regarded only as a step forward. Comments,
suggestions and, especially, future development of palynological research
along these lines are welcome.

METHODS AND TECHNIQUES
SAMPLING

As pollen analysis is a relative, rather than an absolute, dating tech-
nique, it was first imperative to collect sediment samples which could
be dated with some degree of certainty. Most of the archaeological
sites could be, or had already been, absolutely dated by radiocarbon,
tree-rings, or ceramic typology. When test pits were dug into a site
of known date, sediment samples could be collected which were assumed
to be of the same age as the period of construction generally recognized
for the site. It was necessary to collect the samples from previously
unexcavated rooms or areas, however, to insure the collection of un-
disturbed sediments.

To increase the likelihood of gathering sediment samples which dated
from the period of construction, samples were taken from the floors of
rooms in the sites. A stratigraphic series of samples was then taken from
the profile of the test pit, and such sub-floor features as pits were also
sampled. This technique yielded one sample which could be regarded
as the same age as the site (the floor sample), a series of samples which
could be regarded as younger than the date of site construction by an
unknown number of years (the fill samples), and one sample which might
date either from the period of construction or some time earlier (the
sub-floor sample).

After archaeological sites of known date had been sampled, some
sampling was also undertaken on newly surveyed, unexcavated, archaeo-
logical sites. Since these could be roughly dated by associated pottery
types, they served to fill in certain gaps in the chronology. In this report
the initials ““LS” precede the survey number given to sites of this type.
They are identical with those described by Longacre (Martin, Rinaldo,
and Longacre, 1960; Martin, Rinaldo, Longacre and Freeman, 1961).

Sediment samples were also collected in stratigraphic sequence from
the banks of arroyo cuts. In some instances these arroyo sites were selected
for their provenience to archaeological materials; in other instances it
was hoped that though the samples were undated they could be tied into
the dated series and would serve as a control that was uncontaminated
by ‘‘cultural preference” for certain pollen types.

POLLEN ANALYSIS 171

A few samples were also taken from the muck or silt in cattle (stock)
tanks. The open water surfaces of tanks act as natural pollen traps for
the surrounding floral complex (Martin, Schoenwetter and Arms, 1961).
Pollen recovered from such locales can be considered representative of
the ecological conditions in the immediate area.

The total number of samples collected during the summer of 1960
was 263. Samples from five arroyos accounted for 100 of these—four
arroyos in the Vernon, Arizona, area and one in the Pine Lawn, New
Mexico, area. Four samples were collected from cattle (stock) tanks. Of
the 159 samples taken from archaeological sites, 35 were from five sites
in the Pine Lawn area and the rest were from 13 sites in the Vernon area.

Sampling technique was based on the principle that stratigraphic
information was of vital and primary importance. The major limiting
factor in palynological sampling is that pollen grains are microscopic
and easily wind-blown. Efforts must therefore be made to avoid con-
tamination of the samples by recently disseminated pollen or ancient
pollen from other samples. Under ordinary field conditions it is nearly
impossible to avoid every source of contamination, but if reasonable
caution is exercised large amounts of contamination are not expected
and small amounts will not alter main conclusions drawn from the data.
The sampling technique used in the present study may help to guide
other workers, and so is described in detail in Appendix A (p. 206).

EXTRACTION

The procedure followed for extracting fossil pollen was that in general
use at the Geochronology Laboratories of the University of Arizona
for post-glacial arid land sediment samples. Because of time limitations,
and because the types of sediment involved varied widely in texture,
amount of organic material, etc., it was deemed unprofitable to ex-
periment with a selected series of samples to determine the best extraction
technique or techniques that could be utilized. In the interests of ex-
pediency and uniformity, all of the samples were processed by the same
technique.

The extraction technique consists of three basic steps. In the initial
step, the non-silicious fraction of the sample is separated from the silicious
fraction (Arms, 1960). In the second step, the non-silicious fraction is
subjected to a series of well-known procedures which dissolve much of
the organic and non-organic materials from the pollen-bearing matrix
(Erdtman, 1954; Faegri and Iverson, 1950; Wodehouse, 1935). In
the final step, that fraction of the matrix which has a lighter specific

WZ. PREHISTORY OF EASTERN ARIZONA, I

gravity is captured by flotation (Frey, 1955) and is then prepared for
viewing under the microscope. In Appendix B (p. 207) the extraction
technique is described and discussed in greater detail.

ANALYSIS

Though some of the samples resulting from the extraction process
were given cursory inspection at the Geochronology Laboratories to
ascertain that pollen had been recovered, the bulk of the analysis was
undertaken at Southern Illinois University. This involved preparing
and examining the microscope slides, recording their contents, and pre-
paring the text and figures of this report.

Certain limitations affected this phase of the project. No laboratory
facilities were available to process the samples. Therefore, samples which
needed further chemical treatment before their pollen content could
be adequately evaluated had to be ignored. Sometimes the amount of
pollen that could be found on a slide was so small that many slides had
to be examined before a statistically useful count was accumulated for
a given sample. It seemed best to analyze first those samples which were
least difficult to work with; then to go back, if necessary, to the more
difficult ones to fill in such chronological or spatial gaps as were found.
Since most of the samples from archaeological sites were productive of
pollen, it was decided to concentrate upon them rather than upon the
arroyo samples.

A group of ten sediment samples was analyzed by the Geochronology
Laboratories as a check on my counting and identification. Their results
were generally consistent with mine, though some differences did occur.
It was found that counts made by the Geochronology Laboratories tended
to show greater amounts of arboreal pollen, while my own tended to
find greater frequencies of economic pollen, especially Cleome. In major
pollen features, such as the dominance of cheno-am pollen, etc., however,
the counts were in agreement.

Counting and identification of pollen was done at 440 magnifications.
A count of 200 pollen grains from each level, exclusive of unknowns,
was the goal but it could not always be obtained without a great deal
of difficulty. The 200-grain count was selected because its statistical
reliability has been investigated for arid land sediments (Martin, Schoen-
wetter and Arms, 1961), but counts between 150 and 200 grains were
also considered usable.

The figures accompanying this report are of two types. Figure 75
is a composite pollen diagram showing the results of the pollen counts
from a group of archaeological sites in the Vernon, Arizona, area, with
the youngest at the top and the oldest at the bottom. Figure 76 shows the

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Fic. 76.- Analysés-of three samples of pollen from modern surface and pollen diagrams of two archaeological sites from the Pine Lawn, New Mexico, area.

ARIZONA, I

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POLLEN ANALYSIS 173

results of the pollen counts of three surface samples as well as the pollen
diagrams from two archaeological sites in the Pine Lawn, New Mexico,
area. Figures 77 and 78 are graphic arrangements of selected information.
Figure 77 shows selected data from the analyses of the best dated samples
from archaeological localities in the Vernon, Arizona, area, arranged
chronologically according to time estimates provided by the archaeologists.
The samples are from the floors of dwelling units or from well-dated
occupation levels and so are definitely from the period to which they are
attributed. It must be emphasized that the dating in most cases is not
absolute; it is only a reasonable estimate. Figure 78 shows certain signifi-
cant palynological features from the analysis of sediment samples from
the modern surface at archaeological and cattle tank localities in the
Vernon area. These samples were thoroughly investigated, but only
selected data are shown in the text figure.

COMMON NAMES OF POLLEN TYPES
AND ECOLOGICAL NOTES

In this report three main structural categories are utilized when dis-
cussing conditions of plant ecology: grasslands, parklands, and forest.
Short grasslands (Nichol, 1952, pp. 203-205) are today evident in the
Vernon, Arizona, area above 1800 meters elevation. In this zone Juniperus
and Pinus edulis (pinyon) occur sporadically in favorable micro-
environments, but arboreal vegetation is predominantly absent.

The parkland begins (ca. 2050 meters elevation) where Pinus and Juni-
perus become common, but the trees are relatively low and the canopy is
very open. At higher elevations (above 2120 meters) the forest zone exists
where arboreal vegetation is dominant; P. edulis and Juniperus give way
to P. ponderosa and the canopy becomes more closed. Deep shade is found
only at higher elevations than the localities sampled in this study.

Three other categorizations of plants are also used: hygric, arboreal
and economic. Hygric plants are those which only grow in a very moist
environment (Dansereau, 1957, p. 206). In this report, only Typha and
Cyperaceae are included in this group. Salix, Juglans and Alnus might
also have been included, but since their water requirements are not so
limited they are placed with the arboreal plants.

Arboreal plants are those commonly recognized as trees. In this
report the category includes Pinus, Juniperus, Quercus, Salix, Juglans and
Alnus.

Economic plants are those which are either cultigens or wild plants
considered economically important to man. This group includes ea,

174 PREHISTORY OF EASTERN ARIZONA, I

Cucurbita and Cleome. Cleome is included because pollen attributable to
Cleome serrulata has been found in very high percentages in sediments
taken from Pueblo III rooms at Wetherill Mesa (Schoenwetter, 1960b)
and Chaco Canyon (Martin and Schoenwetter, Manuscript b) as well
as alluvial sediments presumed to date from Pueblo III at Binne-Ettini
Canyon (Martin and Schoenwetter, Manuscript a). It is assumed that high
percentages of this zoogamous pollen type in cultural contexts are the re-
sult of its selection by man for some economic purpose. Today the plant is
used by Indian groups in the Southwest as a pot herb, a subsistence food,
and a source of pigment. It is usually gathered or allowed to grow as
a tolerated weed in agricultural fields (Robbins, e¢ al/., 1916; Whiting,
1939):

Since many may be unfamiliar with the scientific names of the plants
for which pollen types have been identified in this study, the following
list of common names is included. Notes on the ecological contexts in
which these plants are usually found are added to facilitate interpretation.

Alnus: Alder. A shrub or low tree common to the flood plains of permanent streams
in the upper parkland and forest zones.

Cactaceae: All plants in the cactus family. Most of the pollen found is probably
referable to the prickly pear group (Platyopuntia). In the study area these plants typify
arid and semi-arid micro-environments.

Cheno-am: Pollen types referable to the Chenopodiaceae (goosefoot family) and
the genus Amaranthus (pigweeds). This is an artificial pollen category necessary be-
cause the pollen of the two plant groups cannot be presently distinguished with greater
accuracy. ‘The designation “‘cheno-am’’ follows the precedent of Martin, Schoen-
wetter and Arms (1961). A common member of the Chenopodiaceae is Cheno-
podium album (lamb’s quarters) and a common member of the genus Amaranthus is
Amaranthus palmeri (pigweed). ‘These plants are typical of disturbed sediment condi-
tions such as occur today in arroyos, along roadsides, and along the dissected flood
plains in the grassland zone.

Cleome: Probably Rocky Mountain bee weed, Cleome serrulata. Identification of
this pollen type is not positive because the pollen grain is very small. The plant today
is found in the parkland and grassland zones and is known to be gathered and semi-
cultivated by Indian groups.

Compositae: All plants in the sunflower family. Smaller divisions of this group can
be made on palynological grounds but with the equipment available these would have
been uncertain. Plants of this family occur under an extremely wide range of environ-
mental conditions.

Cucurbita: Squash. Though the cultivated and wild species of this genus are not
separable on the basis of pollen type the context in which the pollen was found implies
that this is the cultivated form.

Cyperaceae: All plants in the sedge family. Typically, sedges are found under
conditions of hygric environment such as the margins of ponds, marshes, cienagas, etc.

Ephedra: Mormon tea. Though this is not a very common plant in the area it is
occasionally found in the parkland and grassland zones.

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ARBORE AL CHENO-AM COMPOSITE ME SIC ECONOMIC
AGE SITE fo) 20 40 60 80 ioo N
A.D.
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1100 Mineral Creek Site
900 ES="28
800 site --20
700 Ls ~4
275 Tumbleweed Canyon
ee Laguna Salada

? Little Ortega

Fic. 77. Important palynological features of samples of pollen from occupation
levels at archaeological sites in the Vernon, Arizona, area.

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175

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ARBOREAL
Site
Cattle Tank No. |
Table Rock Pueblo
LS-4
LS-34 Pithouse |
LS-34 Pithouse 2
Cattle Tank No.3
[$-28

Rim Valley Pueblo

Hooper Ranch Kiva

Room |8 209

Room I6 7
Mineral Creek
Site 30-31 Arroyo

Site - 30

Cattle Tank No.4

78. Samples of pollen from modern surface at various elevations in the Ver-

non, Arizona, area.

POLLEN ANALYSIS Ley

Gramineae: All plants in the grass family with the exception of ea. Grasses
occur under a wide range of environmental conditions.

Juglans: Walnut. Found today along the flood plains of permanent streams below
the parkland border.

Juniperus: Juniper, locally called cedar. Typically, this is a plant of the parkland
and lower forest zones, but it may extend onto the grasslands.

Malvaceae: All plants in the mallow family. Most of the pollen grains are prob-
ably referable to the genus Sphaeralcea (globe mallow). Pollen of the genus Gossypium
(cotton), which belongs in this family, was not observed though its pollen is distinctive.
Sphaeralcea grows under a variety of environmental conditions.

Pinus: Pine. Smaller groupings than those on the generic level can be made on
the basis of pollen statistics (Martin, Schoenwetter and Arms, 1961) but the data and the
equipment did not lend themselves to this type of analysis. Pines are primarily park-
land and forest plants, but a few may invade the grassland zone.

uercus: Oak; typically found under forest and upper parkland conditions in this
yP yf pper p
area.

Salix: Willow. Pollen identification is not positive in all instances. Typically,
this plant is found along shallowly dissected flood plains in the lower parkland and
grassland zones.

T»pha: Cattail; a plant of hygric conditions, like Cyperaceae.

Kea: Corn; exclusively a cultivated plant.

RESULTS
ARROYO SITES

Series of sediment samples were collected and processed from five
arroyo localities. One series, that from Wet Leggett arroyo in the Pine
Lawn area, is directly relevant to this paper since this area was the locale
of a group of archaeological finds which are considered of Cochise cul-
tural affinity (Martin, Rinaldo and Antevs, 1949). The description of
the alluvial sediments by Antevs allowed placement in time of certain
strata, but because of the intervening years of active erosion at Wet Leg-
gett arroyo Rinaldo and I had some difficulty in relocating the strati-
graphic sections described by Antevs.

It was thought that the samples collected from the strata which con-
tained Cochise artifacts would be the most ancient in the prospective
pollen chronology. Unfortunately, none of the 15 sediment samples col-
lected produced enough pollen for analysis.

None of the other series of samples taken from arroyo sites were directly
related to the archaeology of the Vernon area, where they were collected.
Little work was done on them, since the archaeological samples were
mostly productive and a pollen chronology could be recovered. All of
the samples were processed, however, and some will be used in the future
as part of another report on pollen studies in the Mogollon area.

178 PREHISTORY OF EASTERN ARIZONA, I

BEACH SITES

Two ancient beaches on the shores of playas in the Vernon area have
yielded artifacts and other evidence of human occupation (Martin and
Rinaldo, 1960a). At the Laguna Salada Site charcoal was recovered
which was radiocarbon dated at 1420+60 B.c. (Gro 1614). The Little
Ortega Site, on a nearby playa, could not be dated directly but the artifact
assemblage contained more chipped and fewer ground stone implements
than were observed at Laguna Salada, suggesting an older occupation if
this culture developed in a manner similar to that of the culture found in
Ventana Cave (Haury, 1950, pp. 543-544).

The occupational debris and the artifacts are embedded in the com-
pacted lake silts. The sedimentary types are uniform, no stratigraphy is
apparent in the walls of the trenches, and artifacts and charcoal beds
occur from the surface to a depth of 75 cm. It is highly unlikely that the
cultural materials were washed into their present position or that they
were lowered from some upper level by deflation. The sedimentary de-
posit, and the pollen it contains, appear to date in each case from the
period of cultural activity.

The pollen spectra of the Little Ortega Site are distinct from those of
the Laguna Salada Site (fig. 75). At Little Ortega, pollen from Com-
positae is the dominant microfossil throughout all samples, averaging
38 per cent, and Juniperus pollen frequencies are consistently higher than
those of Pinus. At the Laguna Salada Site cheno-am pollen is the domi-
nant microfossil throughout all samples, averaging 53 per cent, and Pinus
pollen frequencies are consistently higher than those of Juniperus. The
difference in the pollen spectra cannot be attributed to differences in the
local environment, since both sites are situated in approximately the same
environment; both are on ancient beaches at approximately the
same elevation.

It seems certain that the differences in the pollen spectra reflect en-
vironmental conditions at different periods of time: that at the Laguna
Salada Site at approximately 1420 B.c. and that at the Little Ortega Site
at some other time. The artifacts collected appear to indicate that the
Little Ortega Site is earlier in time, and investigation of later sites in the
Vernon area reveals no palynological evidence contradictory to this view.

PiTHOUSE VILLAGE SITES

The oldest pithouse sampled was the Tumbleweed Canyon Site in the
Vernon area. This site contained charcoal from which a radiocarbon
date of A.D. 360-+50 has been obtained by the Groningen Laboratory.

POLLEN ANALYSIS 179

The pollen spectrum of the sediment sample taken from the floor of
the pithouse is unlike those found at the earlier beach sites (figs. 75 and
77). There is about as much cheno-am pollen (27 per cent) as Com-
positae pollen (34 per cent) and about 18 per cent of arboreal pollen.
Nine pollen grains of Zea were recovered.

Two samples from the pithouse fill show results dissimilar to those of
the floor sample. The sample at 15 cm. depth has a higher percentage
of cheno-am pollen, but otherwise there is no essential change except
that <ea pollen is absent. The sample at 5 cm. depth is dominated by
pollen of P:nus and, in fact, is similar to no other subsurface sample ana-
lyzed. A surface sample was, unfortunately, not collected from this site.
At present, there are no pine trees in the immediate vicinity.

The Promontory Site (Martin, Rinaldo and Antevs, 1949) is located
in the Pine Lawn area and is a pithouse village tentatively dated between
300 B.c. and A.p. 500 by archaeological estimate. It is located on a ridge
in an area of pine forest with some juniper and oak at 6500 feet elevation.
The sample from the floor (fig. 76) has 42 per cent cheno-am pollen and
nearly as much (37 per cent) pollen from Compositae. The percentage
of Pinus pollen is surprisingly low, considering the present flora of the site
area. No ea pollen was found in the analysis of the floor sample.

In the samples from the pithouse fill gradual changes in the pollen
percentages can be observed through time. Cheno-am pollen reaches its
maximum frequency at 60 cm. depth (30 cm. above the floor) and then
begins a continuous decline. ea pollen is observed at the 60, 45 and
15 cm. levels. At the 45 cm. level Juniperus pollen is first seen; Quercus
makes its appearance at the 15 cm. level. From the 45 cm. level to the
modern surface, the percentage of Pinus pollen increases consistently until
at the surface it dominates the pollen spectrum. ‘These changes are evi-
dence of a gradual but persistent change in local flora from the time of
the construction of the pithouse. The present forest conditions observable
and demonstrated in the pollen spectrum of the surface sample were
apparently not to be seen at the time the pithouse village was occupied.
At that time there must have been fewer trees, but cultural factors such
as land clearance or biological factors such as blight have equal priority
with environmental change in accounting for the phenomenon.

The SU Site (Martin and Rinaldo, 1940), which dates from the same
period as the Promontory Site, was also tested. Only the surface sample
produced sufficient pollen for analysis (fig. 76).

Site LS-34 in the Vernon area consists of two pithouse areas, both of
which were sampled, and dates some time earlier than A.p. 700, since
only plain brown ware was found. Only the sample from the surface

180 PREHISTORY OF EASTERN ARIZONA, I

could be analyzed from Pithouse 1. At Pithouse 2 (fig. 75) the sample
from the floor did not yield to analysis; the fill and surface samples which
could be analyzed are dominated by cheno-am pollen and may date from
a period later than the floor sample by any number of years. Three
pollen grains of <ea were found in the surface sample from Pithouse 2.

At Site LS-4 in the Vernon area, no floor was observed in a pit going
down to 90 cm., but field notes indicate that it may have been missed.
Since the analysis of samples from the 60 and 90 cm. levels yielded sim-
ilar results (fig. 75), it is assumed that they are representative of environ-
mental conditions in existence at the time the pithouse was constructed.
Pottery recovered indicates occupation about A.p. 700 or 800.

The sample from the lowermost level of Site LS-4 shows a near
equivalence of cheno-am and Compositae pollen percentages (32 and 29
per cent), and arboreal pollen frequencies of about 20 per cent (figs. 75
and 77). At the 60 cm. level the percentage of Pinus pollen increases
5 per cent at the expense of Compositae pollen, but this is not statistically
significant.

Site 30 (Martin and Rinaldo, 1960a) is a pithouse village located in
pinyon-juniper parkland at 7000 feet elevation in the Vernon area. Dur-
ing the excavation of a trench in one house, a sub-floor pit was discovered
(fig. 75). The sample from the pithouse floor (110 cm.) did not yield to
analysis, but it is assumed that the sub-floor pit was constructed during
the period of major occupancy and that the pollen in the sediment sam-
ple taken from the pit approximates that which would have been recovered
from the floor sample. On the basis of radiocarbon dating and pottery
typology the period of occupation is estimated at A.D. 600 to 800, probably
a little closer to A.p. 800 (Martin and Rinaldo, 1960a, p. 120).

As with the other pithouse sites, the cheno-am pollen frequency (29
per cent) approximates that of the Compositae pollen frequency (39 per
cent) in the lowermost sample (figs. 75, 77). The arboreal pollen fre-
quency again is nearly 20 per cent. In the upper levels of the fill, Com-
positae pollen dominates the pollen diagram until the surface sample is
reached, when arboreal pollen shows greater frequency. The gradual
rise in Pinus and Juniperus pollen percentages from the 40 cm. level to the
surface is similar to that observed at the Promontory Site.

Samples were also collected at Turkey Foot Ridge in the Pine Lawn
area (Martin and Rinaldo, 1950a), but they proved unproductive except
for the surface sample (fig. 76).

One sample was collected and processed from LS-50, a pithouse site
in the Vernon area tentatively dated a.p. 800 on the basis of pottery.

POLLEN ANALYSIS 181

Since no room fill or floor was discovered in the test pit the single sample
was not analyzed.

PUEBLO SITES

From the pottery found at the surface of Site LS-28 in the Vernon
area, this pueblo appears to have considerable occupational depth.
Sherds from the fill of a test pit dug into one room for purposes of sedi-
ment sample collection did not aid in dating the room more precisely
than the pueblo itself; an estimated date between A.p. 900 and 1250 may
be given to the floor sample analyzed.

The floor sample from LS-28 gives palynological results similar to
those of the pithouse sites: cheno-am and Compositae pollen percentages
are sub-equivalent and arboreal pollen is about 20 per cent. Pollen of
economic plants occurs as well as some pollen of hygric plants (figs. 75,
77). In the upper levels, cheno-am pollen dominates the pollen diagram
(fig. 75).

The South Leggett Site in the Pine Lawn area (Martin and Rinaldo,
1950b), a pueblo dating a.p. 900-1050 by archaeological estimate, was
sampled but only the surface sample produced significant results (fig. 76).

Higgins Flat Pueblo is located near the San Francisco River in the
Pine Lawn area. The ruin is dated between a.p. 1000 and 1250 and is rec-
ognized as having been constructed in three stages (Martin, e¢ al., 1956).
In excavating a portion of one room for purposes of collecting samples
it was found that the fill extended beneath the masonry walls (fig. 76).
As the room excavated was not one of those included in the first stage of
construction at this site it appears that the masonry was laid down upon
a sediment surface which was part of the general dwelling area before
walls were put up to enclose it. Thus the sample collected at 120 cm.
(fig. 76) represents an early period in the history of occupation of this site,
and this sample more probably dates about A.p. 1000 than about A.p. 1250.

The pollen diagram from Higgins Flat Pueblo (fig. 76) shows a basic
similarity to that from Site LS-28 in the Vernon area (fig. 75). In both
instances the lowermost sample yields sub-equivalent percentages of cheno-
am and Compositae pollen and some Zea. The amount of arboreal pollen
in the oldest sample from Higgins Flat Pueblo (4 per cent) seems unchar-
acteristic, but it will be noted that the lower levels at the Promontory Site
also contained unusually low arboreal pollen percentages, and these two
sites are in the same area. With the exception of the two uppermost
levels, the samples taken above the datable level are dominated by cheno-
am pollen, as is the case at LS-28.

182 PREHISTORY OF EASTERN ARIZONA, I

The Mineral Creek Site in the Vernon area is dated by archaeological
estimate on the basis of pottery types and constructional features at about
A.D. 1000-1200 (Martin, Rinaldo and Longacre, 1961, p. 165). It is
unfortunate that a tree-ring date cannot be given for this ruin so as
to fix its placement in time with more precision, since pollen frequen-
cies in the floor sample from one of the rooms are definitely dissimilar
from those obtained from floor samples in the earlier pithouse and beach
sites. The probable range of error on the date is less than 200 years.
At a maximum, the change in the pollen record could have occurred no
earlier than A.p. 900 and no later than a.p. 1300. As the change is also
in evidence in the 105 cm. sample from Higgins Flat Pueblo, it may have
taken place after A.p. 1000.

In the floor sample (figs. 75 and 77) cheno-am pollen forms the major
portion of that observed (51 per cent), and the dominance of cheno-am
pollen frequencies continues in the subsequent samples. ‘This contrasts
strongly with the floor samples from all earlier dwelling units, where
cheno-am and Compositae pollen frequencies were sub-equivalent. Arbo-
real pollen accounts for only 1 per cent of the floor sample, pollen of eco-
nomic plants for another 2 per cent. Pollen of hygric plants also occurs.

Rim Valley Pueblo is located at 6800 feet elevation in the Vernon
area and dates a.p. 1000-1200 by estimates based on the pottery types
recovered. The floor sample and the upper samples are dominated by
cheno-am pollen (fig. 75). The floor sample yields significantly higher
percentages of arboreal pollen (22 per cent) than the floor samples from
other pueblo sites (figs. 75 and 77), but the elevation may be a compli-
cating factor here. Pollen of economic plants was observed in only one
of the levels of room fill, and it was Cleome pollen rather than <ea or
Cucurbita.

Hooper Ranch Pueblo in the Vernon area (Martin, Rinaldo and
Longacre, 1961) was the archaeological site most intensively sampled.
The site is located on a small rise near the Little Colorado River, a few
yards from a large grove of walnut trees. One of the reasons for sampling
this site intensively is the fact that clearly defined stages are seen in the
constructional development of the pueblo. In the first stage a small
pueblo was built and occupied for an unknown length of time. Later,
the pueblo was filled with trash and a second pueblo was built on top of it.
At some time a Great Kiva was constructed adjoining the pueblo. It
was hoped that significantly distinctive palynological features could be
demonstrated for the two stages of construction and that environmental
changes could be recognized which would account for the building ac-
tivity and/or the abandonment of the site. On the basis of pottery types

POLLEN ANALYSIS 183

it is estimated that the period of occupation was between A.p. 1200 and
1375 (Martin, Rinaldo and Longacre, 1961, p. 167).

Room 6B (fig. 75) dates from the early period of construction. Floor II,
at a depth of 2.3 meters below the present surface, was sampled as repre-
sentative of the oldest sediment attributable to the site. The fill from
2.05 to 2.25 meters was finer-grained and of a darker color than that
above it and is considered occupation fill, while that from 0.9 to 2.05
meters was lighter and coarser-grained and is considered as trash fill.
At 90 cm., Floor I was laid down during the later stage of construction.

The samples from Floor II and the occupation fill in Room 6B yielded
higher percentages of <ea pollen than any others collected in the course
of this project and are the only ones in which Cucurbita pollen was ob-
served. Typha pollen occurs in relative abundance, and the percentage
of arboreal pollen is low. Because of the high proportion of pollen of
cultigens, the pollen types which reflect the regional environment (cheno-
am, Compositae, arboreal) are necessarily in low proportion and the
sample from Floor II appears anomalous in figure 77.

As the samples progress upward through the occupation and trash
fill in Room 6B, it is seen that the proportion of pollen of cultigens
steadily decreases and that of cheno-am pollen steadily increases; thus,
the sample from Floor I shows a dominance of cheno-am pollen and
almost no pollen of cultigens, no pollen of Typha or Cyperaceae, and a
larger proportion of arboreal pollen than Floor II.

Rooms 16 and 18 belong to the later period of construction. The
former was sampled stratigraphically; the latter, except for the floor and
surface samples, was sampled in a random manner. Room 16 overlies
Room 6B; Room 18 lies near the edge of the ruin closest to the grove of
walnut.

In both rooms, Floor I contains small percentages of pollen of culti-
gens, a dominance of cheno-am pollen, no pollen of hygric plants and
about 5 per cent of arboreal pollen (figs. 75, 77). In short, analysis of
samples from Floor I in all three rooms is essentially equivalent. Sam-
ples from the upper levels in Rooms 16 and 18 (fig. 75) show no signifi-
cant increase in Zea pollen, though significant fluctuations can be observed
in the amount of Cleome pollen. Typha and Cyperaceae pollen grains
occur sporadically and the proportion of arboreal pollen fluctuates from
level to level and room to room; it also undergoes internal fluctuation
from dominance by one genus to another at various levels.

Samples from the Great Kiva were collected stratigraphically. The
floor sample from the kiva shows a far greater resemblance to the sam-

184 PREHISTORY OF EASTERN ARIZONA, I

ples from Floor I in Room 16 and Room 18 than the sample from Floor II
in Room 6B, and the samples from the kiva fill are more similar to those
taken from fill in the upper rooms than to those taken from the occupa-
tion fill in Room 6B. Apparently, the kiva was built during the second
constructional period. Seriation studies on the pottery contained in the
kiva may substantiate this conclusion.

Are the construction changes that have been observed at Hooper
Ranch Pueblo correlative with environmental changes? This basic ques-
tion is not completely answered by the data obtained by palynological
analysis. Certainly, there are differences in the pollen spectra recover-
able from the earlier and later construction periods, but since the basic
change is in the percentage and types of pollen of cultigens it must be
recognized that the difference could be accounted for on cultural grounds.
The Xea pollen may be present in larger quantities because the cornfields
were closer to the pueblo at that time; or perhaps people were bringing
ripe corn tassels into their dwelling; or possibly more corn was being
grown.

A certain coincidence of palynological features argues for the occur-
rence of an environmental change. The percentage of Cleome pollen in-
creases in the later period of construction; pollen of hygric plants occurs
more consistently in the earlier period and more sporadically in the later
period; pollen of Zuglans occurs consistently in the later period and rarely
in the earlier period; and arboreal pollen is more important in the later
period. If the change in the pollen record were due to the cultural
changes noted above, it might be expected that the percentage of all
other pollen types would increase as the percentage of <ea pollen de-
creased. The percentage of Typha pollen, however, decreases in the
later period.

Whether the cause is largely cultural or largely environmental, some
shift in economic emphasis seems apparent at Hooper Ranch Pueblo.
If the dating of the Great Kiva to the later construction period is correct,
a shift in religious emphasis may also be indicated. It is tempting to
speculate that as the corn harvest became less dependable the inhabitants
of the site turned to religion in an attempt to restore the previous favor-
able conditions.

Table Rock Pueblo, in the Vernon area, is also situated near the
Little Colorado, but it is located on a rocky hill overlooking a broad
stretch of the river (Martin and Rinaldo, 1960b). It is the youngest site
sampled, dated by radiocarbon (A.p. 1345-+-50) and dendrochronology
(outermost ring A.D. 1331) at about a.p. 1350. Soon after the site was
built the upper Little Colorado drainage basin area was abandoned by

POLLEN ANALYSIS 185

pueblo-building peoples. It was hoped that pollen analysis at this site
would give some clues to the reasons for abandonment.

Two rooms were sampled stratigraphically. As these rooms had not
been previously excavated or numbered, they were designated Room X
and Room Y. In reference to the site map shown in Martin and Rinaldo
(1960b, p. 164), Room X lies east of Room 25 and Room Y lies east of
Room 1.

Pollen spectra from the floors and fills of both rooms are nearly
identical (fig. 75). The samples are dominated by cheno-am pollen;
they are unusually rich in pollen of Ephedra; they have a relatively high
proportion of pollen of Typha and Cyperaceae; they have a low pro-
portion of pollen of economic plants; and they have arboreal pollen
percentages significantly higher than those of Floor II at the Hooper
Ranch Pueblo (Room 6B) but not significantly different from those of
Floor I (Rooms 16 and 18). Except for the Ephedra and the indicators
of hygric environment, the pollen diagram is quite similar to that of
the later construction period at Hooper Ranch Pueblo.

Site LS-24, a pueblo in the Vernon area dating from the same period
as Table Rock Pueblo, was sampled but not analyzed, as no definite
floor was established in the test pit.

SuRFACE SAMPLES

Surface samples were collected at the archaeological and arroyo sites
as controls on underlying samples. A few surface samples were also
collected from cattle tanks, where open water surfaces make conveniently
sampled pollen traps (Martin, Schoenwetter and Arms, 1961).

It is assumed, unless evidence has been found to the contrary, that
the surface samples are representative of the pollen that is being dissem-
inated today in the area of collection. On this basis, the surface samples
from Pithouse 2 at LS-34 and Table Rock Pueblo (fig. 75) have been
discarded from consideration. In these two instances, pollen of economic
plants which was found at the surface may represent contamination
from lower occupation levels.

The analysis of surface sediment samples in the Vernon area is shown
(fig. 78) in terms of three major palynological features (arboreal, cheno-am
and Compositae pollen) plotted against elevation. The surface samples
from the Pine Lawn area (upper part of fig. 76) were collected at 2050
meters (cattle tank), 1975 meters (Higgins Flat Pueblo), 2100 meters
(SU Site and Turkey Foot Ridge), and 2135 meters (Promontory Site).

Contrasts may be recognized in the results of surface samples taken
in the two areas. In the Pine Lawn area, surface samples taken at eleva-

186 PREHISTORY OF EASTERN ARIZONA, I

tions greater than 2100 meters are dominated by arboreal pollen; in
the Vernon area, arboreal pollen is dominant only at 2300 meters. In
the Pine Lawn area, those pollen spectra which are not dominated by
arboreal pollen are dominated by Compositae pollen; in the Vernon area,
those spectra which are not dominated by arboreal pollen are dominated
by cheno-am pollen or have sub-equivalent frequencies of cheno-am
and Compositae pollen.

Generally, the surface samples fall into four categories:

1. Those in which arboreal pollen is the dominant feature; namely,
Site 30, Cattle Tank No. 4 and the Promontory Site. These localities
are mostly within the forest border. Cattle Tank No. 1 is an exception;
it has arboreal pollen as the dominant feature but is located in the grass-
lands where no trees are visible for some miles.

2. Those in which cheno-am pollen is the dominant feature; namely,
those from Hooper Ranch Pueblo and the Site 30-31 arroyo. Surface
samples in which cheno-am pollen is dominant are mostly near streams
or arroyos.

3. Those in which the cheno-am pollen frequency and Compositae
pollen frequency are sub-equivalent; namely, the Mineral Creek site.

4. Those in which Compositae pollen is dominant; namely, the cattle
tank from the Pine Lawn area and Higgins Flat Pueblo. In the former
instance, the locality is at present filled with water during the entire
year and is large enough to be used as a mill pond. This cattle tank is
located in the upper parkland zone.

Higgins Flat Pueblo is located near the San Francisco River, where
the growth of cheno-am pollen producers might be expected to be great.
When the site was visited, the annual crops of Chenopodiaceae and
Amaranthus had not yet developed to the point where they could be
identified; thus, no data are available at present on whether these plants
grow at this locality. An explanation may be found to account for the
high proportion of Compositae pollen in the surface sample from this
site. The site is located on level ground near the river. The buried
masonry of the walls impounds moisture and hinders run-off. ‘Thus, ground
moisture reserves at this locality are unusually high for shallow-rooted,
non-arboreal plants.

Finally, in comparing the sub-surface samples from archaeological
sites (fig. 77) with those from the modern surface (figs. 76 and 78), a
number of striking similarities may be noted. The sample from Little
Ortega is more like that from the tank in the Pine Lawn area than any
other archaeological sample. The sample from Laguna Salada is similar

POLLEN ANALYSIS 187

to that from the Great Kiva at Hooper Ranch. The sample from LS-4
is nearly identical with that from the surface at the Mineral Creek Site.
The sample from Floor I in Room 18 at Hooper Ranch Pueblo is very
like that from the surface at Pithouse 1 at LS-34.

CONCLUSIONS

In constructing a pollen chronology for the eastern Arizona—western
New Mexico area from the information gathered in this study, two basic
problems presented themselves. First, it was necessary to determine the
date of the deposition of the pollen recovered and analyzed. Second,
it was necessary to determine that the pollen spectra attributed to a
given time horizon were actually characteristic of that horizon and
not merely characteristic of that particular locality.

The most common method of dealing with these problems is the selec-
tion of two or more series of superimposed sediment samples. By evalua-
tion of the stratigraphy of the sampled localities it is possible to determine
which of the samples are older and thus to obtain a relative chronology.
By comparing one series of samples with another, it is possible to determine
roughly how local factors of physiography, sedimentation or vegetation
may have affected the pollen record. Then some of the samples, or some
of the stratigraphic strata which have been sampled, may be dated
by radiocarbon, tree-rings or other dating techniques.

This method, however, has certain limitations if the results are to be
applied to archaeology. It is not usual to find many cultural horizons
in superposition or material remains deposited throughout sedimentary
columns sampled for pollen analysis. Also, the dating of such pollen
changes as occur in stratigraphic columns often has a greater range
of error than the archaeologist would prefer. This is especially true in
the arid Southwest. To date a change in the pollen record in this area
to between A.D. 1000 and a.p. 1400, for example, would be insufficient
for major archaeological interpretation, because many cultural changes
can be recognized within this period of time and the pollen change might
be related to all, some, or none of the cultural changes.

In this study, precision in dating many of the sediment samples was
possible because samples could be taken from the floors of habitation
units. If the dwellings could be dated by ceramic content, dendro-
chronology or radiocarbon, the date of the sediment samples was par-
ticularly well established. Samples collected above the floors of the
dwellings could be considered younger than the floor sample, but of
unknown absolute age, while those taken from the modern soil surface

188 PREHISTORY OF EASTERN ARIZONA, I

could be considered representative of the present period. Building the
chronology thus became a matter of fitting the recovered pollen spectra
into their known age relationships.

Since the samples of known date formed the basis of the chronology,
and since these samples were found superimposed upon one another
only in the few instances where constructional stages were in evidence
in the dwelling unit, there remained the problem of determining that
the pollen spectrum recovered for a given time horizon was characteristic
of that time horizon. The resolution of this problem has been approached
by two lines of reasoning.

First, there was one large group of samples which were all rep-
resentative of the same time horizon: the group of 20 ground surface
samples which represent the modern pollen rain. Comparison of
these samples, since the plant habitats from which they were collected
are known, allows some measure of the effect of local factors on pollen
deposition. It was found that surface samples taken from forest or upper
parkland habitats usually contain high percentages of arboreal pollen
(such as at Site 30, the SU Site, or the Promontory Site). Samples
collected from locales where water tables are permanently high (such
as the cattle tank in the Pine Lawn area) or where there is a relative
abundance of ground moisture (such as Higgins Flat Pueblo), contain
high percentages of Compositae pollen. Samples collected from locales
near streams (such as Hooper Ranch Pueblo) contain high percentages
of cheno-am pollen. A few of the samples do not contain high percentages
of any particular pollen type; these are usually from locales in the parkland
or grassland zones where streams are not close by and local conditions
do not indicate a high ground moisture content.

From these data the conclusion is drawn that local conditions of both
vegetation and ground moisture affect the pollen rain at any particular
site. It is recognized, however, that the two factors are inter-related,
since the vegetation is sensitive to the moisture conditions. If the site
sampled is in the upper parkland or forest zones arboreal pollen dominates
the pollen spectrum, but this zone is the one in which precipitation values
are higher and evaporation values decreased because of increased ele-
vation.

If the site sampled is within the grassland or parkland zones, where
there are no trees or the tree canopy is quite open, pollen of non-arboreal
plants dominates. The dominant type will be Compositae pollen if there
is a relative abundance of water locally available; it will be cheno-am
pollen if a stream (permanent or intermittent) flows nearby; it may be
neither if local conditions are otherwise.

POLLEN ANALYSIS 189

If, on the present time horizon, the samples taken from a particular
type of locality are consistently similar, it might be expected that the
same generalization would hold for former time horizons. On the other
hand, for two sites of a given time horizon pollen spectra would be
expected to be dissimilar if the same type of locality were not present
at both. For example, if local conditions of forest and ground moisture
were similar at the Tumbleweed Canyon Site and the Promontory Point
Site, the pollen spectra of the floor samples at both sites would be ex-
pected to be similar, since both are dated between 200 B.c. and a.p. 500.
If local conditions were dissimilar at the two sites, the pollen spectra
would be expected to reflect the difference.

It should be possible, if no climatic change has occurred in the
area to disrupt ecological relationships, to determine also the particular
type of locality from which the sediment sample has been collected
through its pollen spectrum. If the sample contains high frequencies
of arboreal pollen, it should come from an area where forest or upper
parkland conditions are, or were, locally evident. Similarly, it should
be possible to determine if the conditions were those now found below
the parkland border near streams or in areas of abundant local ground
moisture.

The second line of reasoning evolves from inspection of the pollen
diagrams from the various archaeological sites. It is seen that in all of
the sites which date later than a.p. 1000+100, except for Room 6B at
Hooper Ranch Pueblo, the entire pollen diagram is dominated by cheno-
am pollen. In sites which date earlier than a.p. 1000+100, excluding the
beach sites, the pollen diagrams are dominated by cheno-am pollen only
above the floor sample. This shift in the pollen record is noted for sites
in both the Vernon, Arizona, area and the Pine Lawn, New Mexico, area.
From these data it is concluded that a shift in environmental conditions
occurred about a.p. 1000 and that it affected the pollen record at almost
all of the localities sampled. Thus, there is some basis for considering
that shifts in the pollen records at given sites in the east-central Arizona—
west-central New Mexico area may reflect regional changes in environ-
ment rather than merely changes in local conditions. If the pollen shift
can be observed in pollen diagrams from two or more sites the likelihood
is increased that the phenomenon involved is a regional change in en-
vironmental conditions.

If the reader will grant that the means of dating the pollen spectra are
adequate and that the shifts which occur in the pollen record are regional
rather than local fluctuations, the following pollen chronology is evi-
denced by the results of this study:

190 PREHISTORY OF EASTERN ARIZONA, I

Four major periods of different environmental conditions can be rec-
ognized in the palynological data recovered from the archaeological sites.
These periods are characterized by differences in the frequencies of pollen
types, rather than by differences in the types of pollen found.

The most recent environmental period is characterized by dominance
of the pollen spectra by high percentages of cheno-am pollen. It is recog-
nizable at the Mineral Creek Site, Rim Valley Pueblo, Hooper Ranch
Pueblo and Table Rock Pueblo in the floor samples; in about 50 per cent
of the samples taken from the modern surface; and in certain levels taken
above the floor at the Tumbleweed Canyon Site, the Promontory Site,
Site LS-34, Site LS-28, and Higgins Flat Pueblo. Since the oldest floor
sample to which high cheno-am pollen percentages may be attributed is
that from the Mineral Creek Site, it appears that this period began about
A.D. 1000+100 and has continued to the present day.

The dating of the change that occurs in the pollen record is crucial
to proper interpretation of the effect an environmental change may have
had upon culture. The change had not occurred when the floor sediment
at Site LS-28 was deposited, some time between A.p. 900 and 1250. It
had also not taken place when the sub-floor sediment was laid down at
Higgins Flat Pueblo, which probably was about a.p. 1000. By the time
the Mineral Creek Site and Rim Valley Pueblo were constructed, how-
ever, the change had taken place. Rim Valley Pueblo and the Mineral
Creek Site date between A.p. 1000 and 1200. The change must be dated
earlier than 1200, since it was in effect when Hooper Ranch Pueblo was
constructed, ca. 1200.

The bulk of evidence seems to indicate that the change took place
about A.p. 1000. For the sake of greater precision, I have added a plus
or minus figure of 100 years, placing the shift at 1000-100.

Within this first period there is sufficient variation in the frequencies
of other pollen types than cheno-am to justify the establishment of sub-
stages. In the earlier part of the period (1000+100-1200) such floral
elements as Typha, Cyperaceae, <ea and arboreal plants are not of par-
ticular importance in the pollen spectra. In the middle part of the period
(1200-1350) pollen of Zea, Typha and Cyperaceae becomes an important
feature of the pollen spectra. Figure 77 shows the increase in hygric and
economic pollen percentages at this horizon. At Hooper Ranch Pueblo,
fluctuations in the frequencies of pollen of hygric and economic plants
seem to be correlative with cultural changes.

The youngest part of this environmental period (ca. 1350-1960) is
rather poorly sampled but can be recognized in samples from upper
levels of stratigraphic sections. A gradual and persistent increase in the

POLLEN ANALYSIS 191

frequency of arboreal pollen may be observed. This is especially marked
at Site 30 and at the Promontory Site, which are today located in the
upper parkland and forest zones.

The second period is characterized by pollen spectra in which sub-
equivalent percentages of cheno-am and Compositae pollen are observed.
The percentage of arboreal pollen in spectra from this period is greater
in the Vernon area (18 to 26 per cent) than in the Pine Lawn area (4 to 5
per cent). The period is in evidence in the floor samples from Higgins
Flat Pueblo, Site LS-28, Site 30, Site LS-4, the Promontory Site and
the Tumbleweed Canyon Site. A radiocarbon date of Aa.p. 360+50
on the Tumbleweed Canyon Site allows the conclusion that this period
extends from A.D. 1000+100 at least as far back as the fourth century.

It is interesting to note that <ea pollen was recovered from the floor
sample of the Tumbleweed Canyon Site. This datum helps to fill in the
chronology of agriculture in the Mogollon area, and bolsters inferences
based on the conclusion that agriculture was an established feature of
early Mogollon culture.

A gap in the chronology exists between the fourth century A.p. and
the fifteenth century B.c. The third environmental period is charac-
terized by the dominance of cheno-am pollen and arboreal pollen fre-
quencies of 15 to 30 per cent. The only samples collected for this period
are taken from the Laguna Salada Site, which is dated at 1420+60 B.c.
by radiocarbon. The terminal date and the beginning date for this en-
vironmental period are as yet undetermined.

The fourth environmental period is as yet undated. This period is
exemplified by the pollen diagram from the Little Ortega Site, and is
characterized by a dominance of Compositae pollen and arboreal pollen
frequencies of 15 to 30 per cent. The only means of dating the Little
Ortega Site, and thereby dating this environmental period, is through
comparison of the artifacts found at Little Ortega with those found at
Laguna Salada. At Little Ortega more tools of chipped stone have been
found and at Laguna Salada more tools of ground stone were recovered.
It is evident from the pollen analyses that the Laguna Salada Site and
the Little Ortega Site belong in two different environmental periods, but
there is little conclusive evidence to prove which is actually the older.
Temporarily, at least, the Little Ortega Site may be considered older
than 1400 B.c. on the evidence available through artifact typology.

INTERPRETATIONS AND INFERENCES
CLIMATIC CHANGE
Have there been major fluctuations in climate over the three and
one-half millennia encompassed by the pollen record from the eastern-

192 PREHISTORY OF EASTERN ARIZONA, I

Arizona—western-New Mexico area? ‘The question is crucial to inter-
pretation of the palynological data, since a basic objective of this study
is the investigation of the relationship of ancient cultures to environment
in that area.

It has been shown that at different time horizons different frequencies
of certain pollen types were being deposited in the sedimentary column,
and reasons have been given to justify the assumption that these changes
were responses of the natural vegetation to existing environmental con-
ditions. This is an insufficient basis for claiming that changes in climate
have occurred, however, for a change in climate involves a transition
from one climatic type to another. Through an investigation of the
present climate of the area, and through comparison of pollen spectra
from the modern surface and the ancient horizons, it can be demonstrated
that no change in climate is evident in the pollen record.

Climates are defined on the basis of long-range patterns of meteoro-
logical phenomena. The length of time necessary for the establishment
of a climate is disputable, and the measurement of the meteorological
phenomena is often far from complete, but classifications have been
proposed which describe characteristic climatic patterns. While it is
impossible to measure the meteorological conditions prevailing at any
time in the past, it is recognized that parallels may be found between
biological phenomena existing under present, known, climatic conditions
and biological phenomena reconstructed for former time periods. It
may be inferred that in situations where the biological phenomena
of the present approximate those of the past, the climatic conditions also
approximate those of the past.

At present, the area discussed in this report lies in a climatic zone
classified as steppe (Trewartha, 1954). The meteorological characteristics
of this climate are described as those of the transition belt between the
desert climate and the more humid climates. In the steppe climatic zone,
the potential evaporation from the soil surface and the vegetation cover
exceeds the annual average precipitation, as in the desert, but not by
so great an amount. ‘Temperatures are rather severe for the latitude,
with relatively extreme seasonal temperatures and consequently large
annual temperature ranges. Marked daily ranges in temperature are
common. Rainfall is meager, variable, and undependable. Average an-
nual precipitation is 10-20 inches, variability from normal averages
25-30 per cent, and precipitation is seasonal. Steppe climates are situated
on the margins of dry settling tropical air masses associated with sub-
tropical high pressure cells; thus, they are encroached upon by rain-
bearing winds and their associated storms only for short periods.

POLLEN ANALYSIS 193

The eastern-Arizona—western-New Mexico area is situated on the
western margin of a settling air mass. In the summer, when the air
mass is farthest north, torrential convectional showers are formed when
heated air rises from the ground surface and meets cooler air settling
from above. In the winter, when the air mass is farthest south, rain or
snow falls from fronts associated with cyclonic storms.

Summer rains contribute the majority of precipitation allowances
(Smith, H. V., 1956) but the pelting rain does not soak the ground to
any great depth before running off the surface, collecting in flash floods
in the arroyos, and rushing downstream, where it cuts and erodes the
flood plains of major and minor drainages. Winter rains are slower,
soak the ground, and raise the water table, but they account for a much
smaller amount of the annual rainfall. Winter rainfall does not con-
stitute a great water resource for plants, since winter rains occur during
the season when most plants are limited in growth by reduced sunlight
and air temperatures. The two dry months preceding the growing season
cause much of the soil moisture reserve to evaporate. The classification
of the eastern-Arizona—western-New Mexico area as steppe climate is
only indirectly a matter of long-term averages of temperature and pre-
cipitation values. Basically, it involves recognition of the atmospheric
physical system which results in the temperature and precipitation values.
If the area undergoes climatic change, then, some change in the physical
system must occur and not merely a change in average values of tem-
perature and precipitation. In addition, this change must be in effect
for a relatively long period of time. For example, the long-term precipita-
tion pattern in this area could change from biseasonal rainfall to rainfall
in all seasons. This would be a climatic change regardless of the amount
of rainfall received, for it could only take place if the area did not lie
on the western edge of a dry, settling air mass associated with a high
pressure cell. On the other hand, one can imagine a shift in precipitation
pattern from predominantly summer rains with few winter rains to pre-
dominantly winter rains with few summer rains. This situation might
occur under the present physical system if the winters were a little cooler
(thus bringing more frontal activity), if the summers were a little hotter
(since moisture condenses more readily from cooler air), or if winters
were cooler and summers were hotter.

Such meteorological changes might be in effect for only one year,
in which case they would have little effect on the biota of the area. If
they were in effect for some decades or centuries they might have a
great effect on the biota; yet, since the physical system which determines

194 PREHISTORY OF EASTERN ARIZONA, I

the climate of the region had not been basically disturbed, a climatic
change could not be said to have taken place. The temperature changes
initiated in this hypothetical model need not constitute a climatic change,
since in the steppe climatic zone extreme seasonal temperatures and
large annual ranges of temperature are normal.

The position taken in this paper is that long-term fluctuations in
meteorological conditions are of at least two types. If the fluctuation
is demonstrably due to a change in the basic physical system which
is expressed as a climatic type, it constitutes a climatic change. If the
fluctuation is due to changes in the relationship of some meteorological
phenomena to others, yet the basic physical system involved is un-
changed, it constitutes an environmental change or environmental shift. Both
climatic changes and environmental changes may affect the biota and/or
the cultures of an area. In terms of vegetation and the pollen record,
it is expected that climatic changes would be much more marked than
environmental changes.

When we return to the palynological data with these distinctions
in mind, it should be noted that the present climate of the area studied
is expressed differentially in the various samples from the modern surface.
At certain locales, arboreal pollen is dominant; at others, cheno-am
or Compositae pollen is dominant. There is no question that all of the
surface samples reflect the same climate, since all come from an area
controlled by the same physical system, which is classified as a single
climatic type. The differences between them, then, must be recognized
as expressions of local conditions, as they operate within the broad
framework of the steppe climatic type.

Similarly, it is clear that the palynological characteristics of the
ancient sediment samples can be essentially duplicated in certain of
the samples from the modern surface. Over the entire time period inves-
tigated, the range of variation in the pollen frequencies in the ancient
samples does not lie outside of the range of variation seen within samples
of the present climate. Thus, no change in climate can be said to be
evident in the period of time represented by the ancient samples.

THe NATuRE OF PRE-ExIsTING ENVIRONMENTAL CONDITIONS

The demonstration that the climate of the eastern-Arizona—western-
New Mexico area has not undergone change over the past 3500 years
proves that the changes in the pollen record are to be relegated to the
position of environmental changes or environmental shifts. There remains
the problem of determining the nature of these shifts in terms of the

POLLEN ANALYSIS 195

ecological changes that occurred and the meteorological changes that
precipitated them.

Through analysis of the pollen spectra of the modern surface samples
and comparison of the plant habitats from which the samples were
obtained, it was concluded that local conditions of both vegetation and
ground moisture affect the pollen rain at any particular site.

It has been mentioned that high frequencies of arboreal pollen reflect
conditions within the upper parkland and forest borders. In terms of
meteorological phenomena, this may be due to the lower air temperatures
of the higher elevations, to the reduction in evapo-transpiration values
that such lower temperatures encourage, or to higher rainfall allowances
due to adiabatic cooling of air masses in the highlands.

Surface samples which contain high frequencies of cheno-am pollen
have usually been collected near streams. It is known that cheno-am
pollen producers are adapted to growth in disturbed sediments and
that they germinate and develop only during the summer rainy season.
The summer storms which cut and erode the flood plains of streams cause
disturbed sediment conditions and create excellent habitats for the pro-
ducers of cheno-am pollen.

Surface samples in which high frequencies of Compositae pollen occur
have been shown to be related to localities where a relative abundance
of ground moisture is found. Perhaps more important, these are localities
where sediments are not disturbed by erosion and where water tables
are relatively high. Along the streams water tables are relatively low,
for dissection of the flood plains brings the water table down.

There are no surface samples in which pollen of the hygric plants,
Typha and Cyperaceae, occurs. From the habitat preferences of these
plants, however, it is evident that where pollen of hygric plants is found
conditions of standing water may be inferred. Standing water is a result
of poor local drainage. At present, since most streams are actively under-
going erosion in the Southwest, conditions of poor local drainage are
rare. There are a few locales where cienagas and ponds are found, however,
and these sometimes are fringed by sedges and cattails.

If these characterizations are applied to the environmental periods
recognized in the pollen record, the following interpretation of ecological
and meteorological conditions may be developed:

Period I-a: A.p. 1350 to the present. The high percentage of cheno-am
pollen reflects sediment disturbance occasioned by the present summer
rain-flash flood pattern. Some increase in arboreal pollen may indicate a
cooling of air temperatures or an increase in effective moisture allowances.

196 PREHISTORY OF EASTERN ARIZONA, I

Period I-b: ca. A.p. 1200-1350. High percentages of cheno-am pollen
reflect the sort of summer rainfall and sediment disturbance conditions
observable at present. Sporadic and fluctuating percentages of Typha
and Cyperaceae pollen, however, reflect local fluctuations in surface
water and drainage conditions. During this period standing water must
have been more common than it is today. Major fluctuations in per-
centages of <ea pollen appear to be correlative with the fluctuations
in surface water and drainage conditions.

Period I-c: ca. A.D. 1000-1200. High percentages of cheno-am pollen
reflect meteorological conditions similar to those of the present. The
low frequencies of arboreal pollen found at many of the archaeological
localities indicate that the sites were located below the parkland border.

Period II: probably before a.p. 350 to ca. A.p. 1000. The sub-
equivalent percentages of cheno-am and Compositae pollen indicate con-
ditions in which sediment disturbance is less pronounced than at present
and ground moisture reserves are essentially greater. Higher arboreal
percentages are noted in the floors of dwellings from the Vernon area
and lower arboreal percentages are noted in the Pine Lawn area. Ap-
parently the sites are located within or just below the parkland border
in the former area, and below the parkland border in the latter area. An
agricultural economy is evidenced at four out of six sites.

Period III: ca. 1420 8.c. High cheno-am percentages and somewhat
high arboreal pollen percentages indicate conditions of sediment dis-
turbance and, possibly, summer flash floods at a locale near the parkland-
grassland border.

Period IV: undated. High Compositae pollen percentages and some-
what high arboreal pollen percentages indicate mesic conditions (prob-
ably a large pool of water) near the parkland-grassland border.

In the interpretation given above, the problems of ground moisture
reserves and conditions which promote sediment disturbance are of crucial
importance. Directly involved is the question of arroyo-cutting, for ero-
sion and down-cutting of streams is a major source of sediment disturbance
in the Southwest, as well as a means by which water tables may be
lowered. As far as such shallow-rooted herbs as the cheno-am and
Compositae pollen producers are concerned, lowering of water tables
reduces ground moisture reserves.

A widely held hypothesis on the cause of arroyo-cutting is that which
has been recently stated by Antevs (1955). This hypothesis maintains
that the Southwest is a region of intense cyclical drought. During droughts
the vegetation cover is reduced, so that when rains do occur there are

POLLEN ANALYSIS 197

few plants to absorb the water. Rain water, therefore, rushes off the
surface, cutting and denuding the flood plains.

Martin, Schoenwetter and Arms (1961) and myself (1960a) have
proposed an alternative hypothesis. We feel that only the summer
rainstorms contain sufficient energy to cause down-cutting of drainage
ways under the present climatic conditions, since winter rains are usually
not from high energy storms. We propose that if climatic conditions have
remained stable, time horizons in which arroyo-cutting is widespread
may be considered periods in which there were more numerous summer
storms.

Our hypothesis is primarily based upon palynological information
gathered from samples of flood-plain alluvium in southern Arizona. In
the stratigraphic sections of alluvium sampled, it was found that high
percentages of cheno-am pollen often accompany strata which reflect
conditions of arroyo-cutting. Since it is known that the disturbed sedi-
ments occasioned by the present summer rain-flash flood pattern are
ideal habitats for cheno-am pollen producers, the inference is made that
arroyo-cutting and disturbed sediments are associated with heavy summer
rainfall. The down-cutting effect would be the same if the storms were
more numerous or more torrential. Since summer storms are usually
convectional downpours, any storm probably contains more than sufh-
cient energy to initiate and continue erosional activity; thus, an increase
in the number of storms seems probable during periods of arroyo-cutting.

In the pollen record from southern Arizona, high percentages of Com-
positae pollen are found at certain time horizons. These are not ex-
plained as due to an increase in the number of winter storms, since it
is not known whether the Compositae are as much affected by winter
precipitation as the cheno-am pollen producers are by the summer pre-
cipitation. High frequencies of Compositae pollen, however, are often
found in spectra correlated with soil zones, cienaga soils, and other indi-
cations of quiet, steady drainage of the flood plains. This suggests the
possibility of higher water tables during periods when Compositae pollen
is deposited in high frequencies. I (1960a) have maintained that higher
water tables would not have formed without a substantial increase in the
amount of winter rainfall to make up the difference in annual precipita-
tion caused by the reduction of summer rainfall.

Table 21 shows the similarity between the results of this study and
the results proffered by Martin, Schoenwetter and Arms from southern
Arizona. A few points of difference exist, the major one being that Period
II is characterized in the study area by a near equivalence of cheno-am

198 PREHISTORY OF EASTERN ARIZONA, I

and Compositae pollen percentages, while the same time period is char-
acterized by a dominance of Compositae pollen on the southern Arizona
flood plains. Two explanations might be given to account for this dis-
crepancy: first, the sites in the north are archaeological localities rather
than flood-plain alluvium and so are not subject to the same immediate
ground-water conditions; second, definite distinctions now exist between
plant communities in the two areas, so that it is not improbable that
such distinctions existed in the past.

Another point of difference involves Period I-b, which is missing
in the sequence from southern Arizona. As it is recognized that Period
I-b involves local fluctuations in drainage, this is not an important
difference. Finally, there is the difference in the dating of the shift
from Period II to Period I-c. Martin’s information allowed an estimate
of A.D. 1200 for this transition but is not as sensitive as that from the
study area, which calls for definitely earlier placement.

Of far more importance is the similarity between the pollen spectra
from the two areas, especially as concerns fluctuations in the record of
cheno-am pollen. If cheno-am pollen is recognized as an indicator of
summer rainfall conditions and sediment disturbance, the periods of
heavy and light summer rainfall in the study area and southern Arizona
are seen to coincide.

Adopting the hypothesis that cheno-am pollen percentages reflect
rainfall conditions, I interpret Periods I and III as periods when a
pattern of numerous summer rainstorms contributed the majority of
available water to plants in the eastern-Arizona—western-New Mexico
area and initiated conditions of sediment disturbance and arroyo-cutting.
During periods II and IV summer rainstorms were not so numerous, water
tables were higher, dissection of flood plains was not widespread and,
possibly, winter rainstorms were more numerous than they are now.

If the similarity between the pollen chronologies is accepted at face
value, it appears that Period IV correlates with an extremely ancient
environmental period. While this may be true, the possibility exists
that the argument of antiquity for Period IV based on artifact typology
is erroneous and that the Little Ortega Site is actually not older than
the Laguna Salada Site. It would be possible, in that case, for the pollen
spectrum of the Little Ortega Site to be indicative of environmental
conditions in effect during the transition from Period III to Period II.

RELATIONSHIP OF PREHISTORIC ENVIRONMENTS TO PREHISTORY

Certain major cultural developments are well known in the eastern-
Arizona—western-New Mexico area. The first inhabitants were hunting-

SOUTHERN ARIZONA

EASTERN WESTERN
ARIZONA NEW MEXICO

POLLEN RAINFALL | POLLEN RAINFALL PERIOD

1960

1350

1200

1000

350

A.D.
0
B.C.

1000

1420
3000

5000

cheno-am heavy
dominant summer
Compositae | light
dominant summer

cheno-am heavy

dominant summer
with

more pine

Compositae | light Compositae | light

dominant summer dominant summer

cheno-am
dominant,
some hygric

heavy summer;
local standing
water

cheno-am
dominant

heavy
summer

cheno-am light
Compositae |summer
= 1.0

cheno-am

dominant heavy | -------------t-------------- --------
with summer cheno-am heavy 111

less pine dominant summer

cheno-am
dominant

with heavy
increase in|summer
arboreal

Taste 21.—COMPARISON OF POLLEN CHRONOLOGIES

199

200 PREHISTORY OF EASTERN ARIZONA, I

gathering peoples who built no permanent dwelling units, but who
may have had some agriculture. At a later time a group of sedentary
pithouse village dwellers occupied the region, presumably practicing
more agriculture than the early inhabitants. Still later, people in the area
began building pueblo dwelling units and were possessed of a more highly
developed agricultural culture. It is believed (Martin, Rinaldo and An-
tevs, 1949) that the sequence of development involves a single culture.

In the eastern Arizona section of the area, a recent site survey (Martin,
Rinaldo and Longacre, 1961, pp. 147-164) has given much information
on settlement patterns through time. The survey indicates that occupation
was continuous from about 2000 B.c. to a.p. 1400 + 50, but population
size was not always consistent. A steady increase in population is recog-
nized for the period between a.p. 900 through 1300; by 1500, however,
the area had been abandoned by pottery-making, pueblo-building peoples.

In addition, changes are evident through time in the location of
sites. Before A.D. 500, sites were located on hills and ridges in the Valley
of the Little Colorado River, or on flat areas on the sides of mesas. Be-
tween A.D. 500 and 1100, location of sites seems equally divided between
the bluffs overlooking the valley, hills on the valley floor, and the river
valley floor. Sites which date between 1100 and the time of abandonment,
however, are generally located on hills on the valley floor.

The change in environment that occurred between Periods IV and
III seems to have had little effect on the unspecialized cultures of that
day. The shift in rainfall pattern and the consequent lowering of water
tables and increased dissection of the flood plains could not have had
much effect on the water requirements of a nomadic hunting and gathering
people. The increased availability of amaranths may have affected their
dietary preferences and perhaps stimulated cultural interest in cultigens
known in other areas. However, there is no evidence of a change in
social habits.

A long gap in chronology separates the cultures of Period III from
those of Period II. Whether or not a genetic relationship existed between
them, it is evident that the people of Period II had an essentially different
relationship to their environment. These people were sedentary and
they grew corn. Many of their pithouse villages were located away from
the large permanent streams that today drain the area through dissected
flood plains. From the pollen record it appears that they lived close
to or below the parkland border, though today the sites are often found
in the open forest zone. During this period water tables were higher
and even minor streams near their villages were probably permanent
sources of supply.

POLLEN ANALYSIS 201

As they were agriculturalists they had taken a major step toward
cultural improvement, but as they became more dependent on crop
plants for the continuance of their way of life they became more directly
limited by the water requirements of their crops. The earlier hunting-
gathering economy could operate with reasonable efficiency regardless
of water sources and resources. The sedentary agriculturalists were far
more committed to their environmental resources than the nomads and
far more vulnerable to environmental change.

In view of the environmental conditions under which they lived,
it seems likely that the pithouse agriculturalists were rain farmers. The
major factors affecting the growth of corn are length of growing season,
available water for germination of the crop, and available moisture
for maintenance of the crop once it has started to grow. The effective
crop season in four years out of five in this area is between 120 and
150 days (Baker, 1936)—about the same as that in the corn belt of the
Midwest—and is not much of a detrimental factor. Under the present
conditions of heavy summer rainfall and low water tables, dry farming
is a precarious livelihood in the steppe climatic zone because in many
years moisture reserves are insufficient by the end of the frost season
to germinate the crop. The summer rains may be sufficient to mature
the crop, but the immature plants are often washed out or beaten down.

Under the environmental conditions postulated for Period II, however,
winter ground moisture reserves would have been greater at the beginning
of the growing season, either because of the greater number of winter
rains or the higher water tables or both, and the fewer summer rains
would have been less destructive.

Near the end of Period II, the construction of pueblo dwelling units
began in the Mogollon area. It is fairly evident that the pueblo dwelling
unit was borrowed from the Anasazi, for it has a longer development
in the north (Roberts, 1939), and the amount of Anasazi trade pottery
and religious ideas very obviously increased in Mogollon culture after
A.D. 700 (Jennings and Reed, 1956). No change in environmental con-
ditions can be demonstrated as having occurred simultaneously with the
shift to pueblo construction, but it can be recognized that as the change
in house form occurred there was a shift in the placement of the sites. In
effect, the culture is seen to move from one environmental niche to
another. After A.p. 900 more and more sites were located near the major
drainage ways, and fewer are found along the bluffs and ridges above the
valley floor.

What could have been the advantage of such a move? One advantage
would have been that irrigation could be practiced on the valley floor

202 PREHISTORY OF EASTERN ARIZONA, I

much more easily than in the highlands. The practice of irrigation could
have been diffused from the Anasazi with the pueblo and other cultural
items. Alluvial flood plains along the permanent streams would have
been good locales for flood-water irrigation or diversion ditch irrigation
during this period, since the streams were not deeply dissected.

With irrigation, a rise in population may have occurred consequent
upon an increase in the food supply. The communal dwelling unit
would have been a practical and effective means of dealing with a larger
number of people.

The advent of the conditions of Period I-c, with a heavy summer
rainfall pattern similar to that of the present, must have made dry farming
an almost impossible practice. Significantly, most sites are located near
permanent drainage ways or permanent springs. As there is no existing
evidence of large scale irrigation works, the crops may have been irrigated
by damming the permanent stream so that its waters flooded the cropland
periodically or by short diversion ditches. In Period I-b there is ample
evidence of local areas of standing water near the sites. This could be
explained very well by the presence of irrigation ditches or dams.

The use of irrigation in the valleys near permanent drainages might
have been a cultural advancement, but it could not have lasted long
under the environmental conditions postulated for Period I. Sooner or
later dissection of the flood plain by high energy summer storms would
have caused the water table to fall to the point where irrigation could not
be practiced. Since dry farming could not be practiced either, the area
would have had to be abandoned if the culture remained committed to
cultigens.

If the interpretation of environmental changes set forth above has
validity, it should be possible to demonstrate that changes occurred
over the entire area of the steppe climatic zone in the Southwest. As
yet other pollen studies from this area are unpublished, and though
environmental shifts may be evident in the pollen records adequate dating
on these shifts is lacking.

One source of confirmation for the interpretation of the environmental
shifts presented is the cultural record. Not a few cultures are known to
have inhabited the steppe climatic zone of the Southwest during the past
3500 years, and certain cultural changes have been determined. If these
cultural changes can be shown to date from the same periods as those in
the eastern-Arizona—western-New Mexico area, and if they can be inter-
preted as due to similar shifts in rainfall pattern, some degree of support
for the hypotheses presented above may be gained.

In that part of the area where Anasazi culture was dominant, there
are some interesting cultural phenomena which cluster about the dates

POLLEN ANALYSIS 203

we have determined for the environmental shifts (Jennings and Reed,
1956). A.p. 1000, the approximate date of the transition from Period II
to Period I, marks the beginning of an intensive period of areal expansion
for Anasazi culture in PII. This period ends about 1200-1250. a.p. 1200-
1350, the time span of Period I-b, marks the apogee of Anasazi culture
(PIII) but also marks a period of contraction, with Anasazi culture mov-
ing back into its nuclear areas and abandoning its new frontiers.

It is known that the Anasazi had irrigation systems at Mesa Verde,
but these are not precisely dated (Stewart and Donnelly, 1943). If we
assume that the Anasazi had methods of water control during PII, the
cultural changes described can be explained on the basis of the environ-
mental shifts postulated.

With the advent of conditions of predominantly summer rainfall about
A.D. 1000 more of the steppe zone would have been open to irrigation
along permanent drainage ways, since less water would have been re-
tained in the upper reaches of the highland watersheds and the perma-
nent streams would have carried the excess. The Anasazi may have
pioneered such newly available territory.

As in the area investigated in this study, erosive action would not have
been long in reaching the permanent streams, which would then have be-
come useless. Abandonment would have resulted. Sites in the nuclear
areas may also have experienced an increase in productivity of agricul-
tural lands as conditions became congenial for irrigation. This might
account for the expansion of population and the high development of
culture at that time.

Cohonina population movements into the Grand Canyon and its side
canyons are similarly grouped about the dates determined for the en-
vironmental shifts. Schwartz (1956) states that up to A.p. 900 there was
no major use of the canyons as habitation areas, but that after that date
the Cohonina movement into the canyon began. About 1100 non-
Cohonina peoples from the west and south ‘‘who up to this time had
lived more or less permanently on the Plateau”? moved in also. By
A.D. 1200, the Cohonina had abandoned the Plateau entirely.

If the Cohonina and other peoples living in that area of the Plateau
were primarily rain farmers it is understandable why movement into the
Grand Canyon area would not have been advantageous earlier. ‘The
date of A.p. 900 for movement into the canyon is about 100 years earlier
than we would suspect on the basis of the palynological information
from the study area but not so much earlier as to discount the argument.
The a.p. 1000 date is a probable one, as determined in this study, and
Schwartz’ A.p. 900 date seems to be of the same type. It has been estab-

204 PREHISTORY OF EASTERN ARIZONA, I

lished in this study that the environmental shift had been completed by
the year 1200, however, and this would explain the abandonment of the
Plateau by that date. The dating problem is complicated by the avail-
ability of rich farm lands in the Flagstaff area resulting from the eruption
of Sunset Crater in the middle of the eleventh century A.p. By 1160,
however, this resource had been made unavailable because of erosion
(Colton, 1936, 1949)—a result which might be expected under the en-
vironmental conditions postulated.

Schwartz (1957) also considers that population movements of the
Cohonina were due to changes in meteorological conditions. His argu-
ments are developed upon different bases, but he concludes that peoples
living on the Plateau practiced dry farming until the tenth century.
Movement into the Grand Canyon and its side canyons is thought to
have been necessitated by a population increase coincident with a shift
to greater aridity and to have been accompanied by a period of experi-
mentation in architecture and agriculture. A period of erosional activity
is recognized between A.D. 1200 and 1350, perhaps triggered by a stormy
period following a drought around a.p. 1100. The basic difference be-
tween the position of Schwartz and that advanced in this paper is that
the meteorological changes are thought to have been due to different
causes. Schwartz considers that the changes were due to a climatic
trend toward greater aridity which had been going on since ca. A.D. 1.
In this paper, changes in the summer rainfall pattern are thought to
have created erosional activity and lowered water tables. ‘Thus condi-
tions effectively more arid were in effect at certain time horizons, though
climatic change was not involved.

Woodbury’s recent study (1961) of agricultural practices in the Point
of Pines area notes that terracing systems were initiated about A.p. 1000.
Strictly speaking, this area does not lie north of the Mogollon Rim, but
its elevation places it within the steppe climatic zone. Since the Point
of Pines area was inhabited long before a.p. 1000 by agriculturalists
(Martin and Schoenwetter, 1960), why would terracing systems have
been inaugurated only after that date? It seems reasonable to suppose
that it was only after A.p. 1000 that some sort of erosion controls were
necessary. According to the postulated environmental conditions it was
only after that date that erosion controls would have been necessary.

For the Sinagua (Colton, 1946; Schroeder, 1960) a pattern similar
to that recognized for the Cohonina is seen. After the lands produced
by the eruption of Sunset Crater were no longer arable, a retreat to the
valleys where permanent water was available is noted, in this case the

POLLEN ANALYSIS 205

Verde Valley. Irrigation was definitely practiced in the Verde Valley
after A.D. 1250 (Schroeder, 1948).

From the preceding discussion it is clear that the postulated model
of environmental changes may be used rather effectively in explaining
certain cultural changes which have occurred in the steppe climatic
zone. Of course this does not constitute proof of the model, but it does
seem to argue for acceptance of the model as a starting ‘point for future
investigation.

One more major question remains. It is known that a great deal of
territory within the steppe climatic zone was abandoned by agricultural-
ists after about A.p. 1400. While this may be explained as due to erosional
activity which caused a reduction in crop potential during Period I-b,
historical records (Hastings, 1960) and geological stratigraphy (Bryan,
1925) clearly show that the erosional cycle had ceased long before the
nineteenth century. The pollen record of Period I-a gives indication
that the pattern of summer rainfall was not disrupted, but if the river
valleys were not dissected why was irrigation agriculture not once more
highly developed in the steppe climatic zone?

It has been indicated by lexico-statistics (Hoijer, 1956) and archaeol-
ogy (Riley, 1954) that Athapascan-speakers were probably established in
the Southwest before a.p. 1300. Possibly the culture of the Athapascan-
speakers on their arrival was adapted to a boreal forest environment,
like that of the original homeland in the far north. Even today the cul-
ture of the Western Apache (Kaut, pers. comm.) is essentially adapted
to boreal conditions. These people do plant a small crop of corn in
favorable micro-environments in the spring, but the bulk of their eco-
nomic supply comes from hunting and gathering in the pine forests of
higher elevations during the summer. As they return to winter encamp-
ments in the warmer lowlands they stop off to harvest the crop which
was planted earlier. The Chiricahua Apache (Opler, 1941, p. 374) plant
near their summer encampments, leaving most of the cultivation to the
women while the men are hunting.

If people following similar economic patterns were established in the
area after its abandonment by the agriculturalists they might have served
as a barrier to re-occupation when conditions in the river valleys changed.
If aggressiveness and raiding were already established cultural patterns
among the Athapascan-speakers, they might have been formidable op-
ponents to sedentary puebloans.

Some small amount of data on environmental conditions existing after
A.D. 1350 tends to support this tentative hypothesis. Pollen profiles show

206 PREHISTORY OF EASTERN ARIZONA, I

an increase in arboreal pollen in Period I-a. This might indicate that
after its abandonment by agriculturalists the eastern-Arizona—western-
New Mexico area underwent an expansion in the amount of forested
land. Since it is possible that the Athapascan-speakers were culturally
adapted to boreal forest conditions at the time of their entry, the effect
of forest expansion would have been to offer an expansion of territory for
forest-dwelling peoples.

It is recognized that an increase in the frequency of arboreal pollen
may not be due to an increase in the number of trees. It is equally pos-
sible that it reflects a decrease in the output of some other pollen pro-
ducer, such as cheno-ams, due to changes in environmental conditions
which do not affect the trees at all. Noting the apparent invasion of
trees at the Promontory Site and Site 30, however, and Woodbury’s con-
tention that forest movement took place at Point of Pines (Woodbury,
1961, p. 2), I consider it very likely that arboreal expansion has taken
place.

Even an increase in forest need not be explained as a purely natural
phenomenon. It is quite possible that the growth of forest was a re-growth
reflecting the cessation of land clearance measures by the agriculturalists.
It is recognized, though, that dendroclimatic records for the time period
1350-1800 (Schulman, 1956) indicate an environment favorable for tree
growth.

APPENDIX A: SAMPLE COLLECTION TECHNIQUE

The profile or arroyo bank selected for sampling was that which
showed the most stratigraphic detail. The section to be sampled was
measured and mapped on graph paper when ordinary field notes would
not be sufficient for a description. When possible, the section to be sam-
pled was so located that wind-blown pollen and debris blew into the face
of the collector and not into the samples he was collecting.

The section was measured vertically by means of a steel tape. Sam-
pling intervals of 5, 10 or 15 cm. were selected relative to the depth and
stratigraphic detail of the section. The intervals were marked off on the
section by means of marks made with a trowel. The trowel was then
wiped off so that no dirt was visible, and the surface of the face was
scraped away to a depth of one-half or three-fourths of an inch at the
lowest mark. Using the trowel as a scoop, a quarter to a half pound of
sediment was removed from the level indicated by the mark and placed
in a clean vinyl plastic bag. After the bag had been sealed and labeled, the
trowel was wiped clean again and the procedure repeated for the next

POLLEN ANALYSIS 207

lowest mark, then the next, and so on. Sampling the section from the
bottom upward reduces the possibility of contamination from upper levels.

APPENDIX B: POLLEN EXTRACTION TECHNIQUE
STEP 1

A 50 ml. nalgene, round-bottom centrifuge tube is one-half to two-
thirds filled with sediment from a sample and pollen-free water added
(distilled or filtered) to the three-quarter mark; 1 ml. of a solution of
quebracho, 2 ml. of pine oil and 3 ml. of a solution of laboratory deter-
gent are added and the whole is thoroughly stirred. The tube is placed
into a large beaker and an air or gas source is inserted into the tube.
When the gas is added slowly, oily bubbles are formed which carry non-
silicious material out of the tube and into the beaker. Water! is added
to the tube as it is depleted and the mixture stirred often during the proc-
ess. After a half hour the detritus in the tube may be discarded and the
tube cleaned and the material in the beaker put back into the tube and
centrifuged. The supernatant is discarded. The mixture is then given
a water rinse and centrifuged and the supernatant discarded. The que-
bracho acts to depress silica in aqueous solutions so the material bubbled
into the beaker is largely silica-free (Arms, 1960).

STEP 2

A: Conc. HCl is added to the tube slowly with cautious stirring until
evolution of gas ceases. This dissolves carbonates in the mixture, pri-
marily, and makes the mixture acid to facilitate the next procedure. The
mixture is allowed to sit overnight? and is stirred again before centrifuga-
tion and discard of the supernatant.

B: Conc. HF is added to the tube slowly with cautious stirring until
evolution of gas ceases. This dissolves almost all of the remaining sili-
cates. The mixture is allowed to sit overnight and stirred again before
centrifugation and discard of the supernatant.

C: Another rinse is given with conc. HCI to remove fluorides and to
lessen the acidity of the mixture. The tube is centrifuged and the super-
natant discarded.

D: The mixture is rinsed with glacial acetic acid to dehydrate the
organic fraction. The tube is centrifuged and the supernatant discarded.

! All water must be pollen free to avoid contamination. Equipment must be rinsed
with such water before use.

* Whenever the mixture is left the open surface of the tube must be covered to
avoid contamination by modern pollen.

208 PREHISTORY OF EASTERN ARIZONA, I

E: 10 ml. of acetolysis mixture (one part of sulphuric acid to nine parts
of acetic anhydride) are added to the mixture slowly and with cautious
stirring. When the evolution of gas has mostly ceased, the tube is trans-
ferred to a hot water bath for five minutes. This procedure destroys a
considerable portion of the organic fraction of the mixture but does not
act on the pollen if carefully done. The tube is centrifuged and the
supernatant discarded.

F: The mixture is rinsed with glacial acetic acid to stop the preceding
reaction and to make the mixture less acid. The tube is centrifuged and
the supernatant is discarded.

G: The mixture is given two rinses with acetone to remove any ma-
terials that might be soluble in this solvent and to prepare the mixture
for the next step. The supernatants are discarded.

STEP 3

A: 15 ml. of flotation mixture (two parts of tetrabromoethane to one
part of acetone) are added to the tube, a stopper is put into the tube,
and the whole is shaken thoroughly; then the tube is centrifuged at half-
speed for 15 minutes. The flotation mixture has a specific gravity of
about 2.0 and so will separate the lighter fraction containing the pollen
from the heavier fraction of the mixture, which will sink to the bottom
of the tube. The supernatant is decanted into a clean centrifuge tube;
the heavier material is discarded.

B: Acetone is added to the supernatant and the whole thoroughly
stirred. ‘This reduces the specific gravity so that the pollen-bearing debris
can be centrifuged to the bottom of the tube, after which the supernatant
is discarded.

C: The mixture is given another rinse with acetone to insure that all
flotation mixture is removed. The tube is centrifuged and the super-
natant discarded.

D: 10 per cent KOH is added to the mixture and the tube trans-
ferred to a boiling water bath for ten minutes. Frequent stirring aids the
reaction, in which certain of the remaining organic materials are de-
stroyed and the pollen is expanded for better microscopy. The tube is
centrifuged and the supernatant discarded.

E: The mixture is transferred to 10 ml. shell vials with a jet of alcohol
and centrifuged. The supernatant is discarded.

G: Enough glycerin is added to the mixture to cover and keep it
moist. A water solution of basic fuchsin stain is added before viewing the

POLLEN ANALYSIS 209

material. An alternative is to add pre-stained glycerin jelly to the vial
rather than glycerin and stain.

IX. Summary

During the field season of 1960 several projects were undertaken:
1. Archaeological excavations of six sites.

2. Continuation of the archaeological survey of the Upper Little
Colorado River Drainage.

3. <A paleoecological inquiry by means of pollen analysis.

The costs of the palynological research, of the archaeological survey,
and of the excavation of the Tumbleweed Canyon Site were paid for by
means of a grant from the National Science Foundation. We are grate-
ful for their assistance, without which the scope of our archaeological
activities would have been sharply limited.

The sites, briefly summarized, are given in chronological order, with
the earliest first. Then follows a section concerned with Settlement Pat-
terns and various conjectures derived from these; and finally a brief resume
of the results of the other three major projects: the study of pottery de-
signs; the archaeological reconnaissance; and the paleoecological study.

1. TUMBLEWEED CANYON SITE

The earliest excavated site, Tumbleweed Canyon Site, consists of
three pithouses and three circular pits that may have been used for
storage. ‘This site was located on a high mesa-top overlooking Lyman
Dam and the Little Colorado River Valley. Crude, double walls made
of lava boulders span each end of the long, narrow mesa and also span
any possible means of access. It is possible that these “‘walls”’ served as
primitive defense systems to exclude unwanted visitors (see Chap. VII,
‘Conclusions,’ for a notable discussion of this).

The types of stone tools that occurred at this pithouse village include
the following: one-hand manos, basin metates, rubbing stones, cylindrical
pestles, choppers, notched or shouldered projectile points, flake knives,
and scrapers. It should be noted that these types are also found at later
villages. We would be hard pressed then to single out one of these types
of stone artifacts as the type characteristic of an early phase (that is, be-
fore A.D. 500). We can say, however, that the types listed above occur
more abundantly in early sites and tend to decrease in frequency or pop-

210

SUMMARY 211

ularity in sites of later dates. In other words, we do not regard types of
stone tools as sensitive chronological indicators. It is usually conceded
that they are less useful than pottery, for instance, in detecting more exact
chronological divisions.

The study and analysis of stone artifacts, especially from a pre-ceramic
site like Tumbleweed, are important, however, in any functional appli-
cations of archaeological research, the essential purpose of which is to
provide information about man’s past. At best, the archaeologist is
hampered in his attempt to learn of past cultures and societies because
only a portion of the whole culture survives. We must utilize all avail-
able data if we hope to learn anything about the past.

Tools of stone are among the few classes of imperishable objects to
survive in unchanged form. Stone artifacts are diversified and enter into
nearly every aspect of the life of the people. From them we can often
make guesses concerning agriculture, hunting activities, preparation of
food, ornamentation, house building, and even ceremonial activities.
From these data we may be able to create hypotheses concerning the
growth and development of culture, culture change, trade relations, the
specific tradition to which a given site belongs, and perhaps even social
organization. It is the study of minutiae of the material culture of a past
society which makes it possible to interpret archaeological data—specif-
ically, artifacts of stone, of bone, of pottery and of architecture—in terms
of social history.

The stone artifacts from Tumbleweed Canyon Site, then, are not com-
plex when compared with those from sites that were occupied in A.p. 1200,
for example, but they are exceedingly useful, nevertheless.

Diligent search, however, produced not a single sherd of pottery. We
assume, therefore, that the people who built and lived in the crude shelters
that we investigated did not make pottery. ‘This is a curious anomaly
that is not readily explainable, since contemporary peoples some hun-
dred miles to the south did manufacture pottery. Did the dwellers of
Tumbleweed Canyon Site know of pottery-making and refuse to accept
this art, or were they so isolated that knowledge of this art had not yet
reached them?

Charcoal from the roof(?) beams was dated at the Laboratory of the
University of Groningen, The Netherlands, by Dr. H. de Waard at 1685
years before the present, +50 years (GRN 2801). “‘It is possible that the
value found by C-14 method may be in error up to 200 years. The maxi-
mum error, however, is rather improbable.”’ (Letter from Dr. de Waard,
August 13, 1960.)

We date the occupation of this site at about A.p. 275.

212 PREHISTORY OF EASTERN ARIZONA, I

2. GOESLING SITE

Two pithouses were dug out of a possible ten or more. Both had
burned and one had subsequently been used as a trash dump. Nearly
5000 sherds were recovered from this site. Of these, over 25 per cent
were Classified as Red Mesa Black-on-White sherds. Drs. E. B. Danson,
Emil W. Haury, Alan P. Olson, Raymond H. Thompson, William W.
Wasley, and Fred Wendorf, all of whom are familiar with this type of
pottery, would probably classify these sherds as bearing designs in a
Red Mesa Black-on-White style.

The significance of the site lies in the fact that the abundance of large
black-on-white sherds presented us with an excellent opportunity to insti-
tute a comparative study of design elements on the Red-Mesa-style
sherds and on those that we are calling Snowflake Black-on-White (see
Chap. III).

No tree-ring or carbon-14 dates have been obtained from this site.
An estimated date of A.p. 900-950 is placed on it.

3. “CHILCOTT SITES

The three Chilcott sites include several surface rooms with masonry
walls, one pithouse, and several brush shelters. The pithouse and its
antechamber were subsequently remodeled into two rooms. Firepits oc-
curred in several rooms. From these sites, we obtained a total of 2600
sherds. The most popular painted type was Snowflake Black-on-White
(19 per cent of all sherds) with Reserve, Tularosa and Kiatuthlanna
Black-on-White trailing behind.

The date of these sites is placed at about a.p. 1200 (Groningen
GRN 2414) (760+80 before present).

4. THODE SITE

Eleven rooms out of a possible twelve to fifteen were excavated. The
village plan or arrangement of rooms and the primitive masonry were of
special interest to us because they probably represent a step in the develop-
ment of pueblo architecture and arrangement of rooms. The rooms were
of irregular shape, with walls of crude masonry composed of unshaped
cobbles and boulders of varying sizes. Floors were semi-subterranean,
from 10 to 30 cm. below the old ground surface. Interior equipment was
limited to a firepit in one room, possible hearth areas in two other rooms,
and a few milling stones. Under the wall of one of the units two burials,
with mortuary pottery, were located. No kiva was found.

SUMMARY 213

Sherds were small in size and few in number. Only 765 were recov-
ered, of which over 60 per cent were decorated types. The most popular
type was Snowflake Black-on-White (23 per cent of the total). Following
it in decreasing order of popularity were: Tularosa Black-on-White (4 per
cent), Reserve Black-on-White (2.61 per cent), and Kiatuthlanna Black-
on-White (2.10 per cent). There were also three sherds of Wingate
Black-on-Red.

The estimated date for the Thode Site is put at A.p. 1200+-50 years.

5. RIM VALLEY PUEBLO

The plan for this village approaches that found in later villages. The
rooms are grouped in two units on opposite sides of a plaza. Eleven
rooms out of a probable twenty-five were cleared. The rooms are rec-
tangular, with walls of vertical-slab masonry or random rubble composed
of cobbles. The doorways that were found were in partition walls. No
doorways leading outside were discovered. Interior equipment consisted
of firepits, wall ventilators opposite the fireplaces, and flour receptacles.
No subterranean kiva vent was found, but certain features of Room C
suggest that it may have been used for ceremonial as well as secular
functions.

Pottery types arranged in a descending order of occurrence are: Re-
serve Black-on-White (7.59 per cent), Snowflake Black-on-White (6.03
per cent), and Tularosa Black-on-White (4.62 per cent). A sprinkling
of the 2188 sherds found have been classified as Wingate Black-on-Red,
Houck Polychrome, Tularosa White-on-Red and St. Johns Polychrome.

A tentative date of about a.p. 1225+50 years has been assigned to
this site.

6. GREAT KIVA, HOOPER RANCH PUEBLO

The pueblo to which this Great Kiva belongs has been described in
detail (Martin, Rinaldo, and Longacre, 1961; see also p. 220 of this
report).

The Great Kiva is one of the largest rectangular kivas to have been
dug. It measures 15.5 by 14.5 meters (interior dimensions). Entrance
is by means of an easterly-oriented ramp that slopes gently downward
into a vestibule. A large sandstone slab set on edge between the firepit
and the ramp-entrance acted as a deflector—an unusual feature in a
Great Kiva. The interior of the kiva was provided with a bench on all

214 PREHISTORY OF EASTERN ARIZONA, I

sides, and two vaults flanked the central area and the firepit. The vault
on the south side of the building was lined with masonry, whereas the
north one was simpler.

In cleaning the floor west of the south vault, we removed a small slab
of sandstone that may have been “‘sealed”’ in place by a calking of adobe
and that had been placed over the annular opening of a ring slab. A
glance through the opening indicated that little dust had collected in the
box or crypt and that it contained two objects—a human efhgy of sand-
stone, carved and painted, and a miniature jar. In the jar and on the
floor were beads of several colors. The figurine, lacking the right arm,
was face down. The front of the sandstone figure had been carved and
painted to represent, perhaps, a supernatural being. For a detailed de-
scription and a full discussion of its possible significance, see Chapter II.
The crypt appears to duplicate in miniature the Great Kiva itself and the
annular slab may represent the opening to the kiva. Thus the crypt may
be symbolic of a kiva and the entrance to the underworld.

At present, we regard this Great Kiva as a product of converging tra-
ditions, derived in part from Mogollon ceremonial structures and in part
from Anasazi great kivas. The convergence of Tularosa Mogollon and
Chacoan Anasazi traditions is likewise manifested in the ceramics found
at Hooper Ranch Pueblo.

Among the decorated types of pottery the most popular ones, in de-
scending order, were Tularosa Black-on-White (11.00 per cent), Wingate
Black-on-Red (6.77 per cent), St. Johns Polychrome (3.13 per cent),
Heshota-uthla Polychrome (2.08 per cent), Four Mile Polychrome (2.02
per cent), and Kwakina Polychrome (1.88 per cent). There was also a
sprinkling of the Pinnawa series.

When in the lifetime of the Hooper Ranch Pueblo was the Great Kiva
built? Architectural data alone could not answer this important question.

We turned, therefore, to other available evidence.

Schoenwetter (Chap. VIII) suggests, on palynological grounds, that
the Great Kiva was built during the latter days of the pueblo. Freeman
(Chap. IV), in his statistical analysis of the painted pottery from some
of the rooms and from the Great Kiva at Hooper Ranch, likewise places
the Great Kiva as “‘late’’ in his seriation. He states, however, that the
Hooper Ranch Pueblo afforded the most dubious of any analysis that
he constructed in this report.

My colleague, Dr. Rinaldo, and I agree with the supplementary find-
ings of our collaborators, and in the absence of absolute dates or other
evidence to the contrary, we accept the hypothesis that the Great Kiva

SUMMARY 215

was built, or at least used most frequently, in the last days of the occu-
pation of the village.

What conjectural date do we place on the Great Kiva?

In our report on the pueblo itself (Martin, Rinaldo, and Longacre,
1961) we estimated the dates of the pueblo as running from about
A.D. 1200 to 1375.

Charcoal from the floor of the Great Kiva has been dated at Groningen
at 730+60 years before the present or A.D. 1230 (GRN 3006).

SETTLEMENT PATTERNS

Although six sites were excavated, they are somewhat widely sepa-
rated in space and time. Not too many firm conclusions can be based
on this kind of checkered information. A few brief inferences may per-
haps be permitted, especially if they incorporate our other evidence from
the area.

1. ‘TUMBLEWEED CANYON SITE

The pre-pottery pithouse site at Tumbleweed Canyon is presently
unique since it is the only excavated one in our area. In the course of
his survey Longacre found a few pre-pottery sites with one or two de-
pressions (pithouses?) outlined by boulders (LS sites 84 and 86; Martin,
Rinaldo, and Longacre, 1960). These may be sites similar to and coeval
with Tumbleweed Canyon Site.

One can hardly speak of a village “‘plan’’ or “‘organization’’ where
only three houses are involved! We can stress their isolation, located as
they are atop a mesa several hundred feet above the river. Water may
have been available in now dry springs; if not, water had to be carried
up from the Colorado River. Corn was grown or imported, for corn
pollen was found (Chap. VIII). If corn was grown locally, the fields
may have been down on the flats near the river, for it would not have
flourished, in all probability, on the mesa top unless the rainfall pattern
was different. The economy of the group was apparently a combination
of hunting, plant-collecting and some agriculture (corn). The presence
of storage pits must be emphasized. It is probable that the population
was sedentary. Baking ovens were not encountered, but since firepits
were found, it is assumed that cooking, parching or roasting may have
taken place within the house.

It is really impossible to make any guess as to density of population
for this time period of about a.p. 275. Based on available evidence,
I should assume that the regional population was very small.

216 PREHISTORY OF EASTERN ARIZONA, I

Nuclear families may have inhabited the pithouses, perhaps three per-
sons to a house. This random placement of several houses certainly sug-
gests nuclear families rather than an extended family unless an extended
family occupied all three houses. With this kind of village arrangement
I should assume that each village represented a politically independent
and endogamous band.

Favored locations for pre-pottery pithouses include several topographic
categories: on mesa tops; on a bench on the side of a mesa; and on a
ridge in a valley floor.

2. GOESLING SITE

The two pithouses excavated at this site (out of perhaps 10 to 15)
belong to the Anasazi tradition. The village to which they belong was
apparently composed of independent dwelling units arranged in no par-
ticular order. Storage-cists and refuse-areas were probably present but
we did not look for them. One might refer to this site as a multiple-unit
site consisting of several pithouses and additional features typical of a
Pueblo I or Pueblo II village. The village was located on a low terrace
overlooking the valley of the Little Colorado River. Water may have
been drawn from springs, if they existed, or from the not too distant river.
Corn, and perhaps beans and squash, were probably cultivated in the
flood plain—a very short and convenient distance from the village. The
economy of the people of this village was largely based on the cultivation
of crops.

I should guess that nuclear families constituted the social organization
of villages of this type and time period. From the survey, we know that
in our area of study there are probably 60 sites that belong to this period
(about a.p. 900). If one assumes that there are, on the average, five
dwelling units per site and that three people lived in each dwelling, one
finds that there may have been approximately 900 persons living in this
area at this time. While such an estimate of population is perhaps rash,
I should explain that I do not take this or any of these estimates literally.
They merely rank the populations of the villages of differing time periods
in a relative order and give one a sketchy impression of population change.

3. CHttcotTtT SITEs

Although we named three sites ‘Chilcott,’ we feel that only Site 1
was the home village. It is possible that Sites 2 and 3 served as farmhouses
or store rooms, since they appeared to have been brush shelters rather
than permanent dwellings. My remarks, then, will pertain to Site 1.

SUMMARY 217

Two rectangular rooms in this unit were contiguous, but the other
three were close by but separate structures. The walls of the rooms were
composed of masonry of a crude rubble type and may represent some of
the earliest masonry in our area. It should be clear, however, that the
three rooms were not contiguous. Each room was a separate unit and
the units were clustered near to one another. This village probably rep-
resents an early stage in the development of pueblos, but one can hardly
state that the germ of the later village plans lies in a hamlet of this period.
In fact, some of the rooms possess floors that were excavated somewhat
below the old ground surface and, in this characteristic, retain a pithouse
flavor. But the walls, composed of odd boulders, were footed on the sur-
face of the ground and continued upward. In other words, the lower
segment of wall was of native earth with no veneer of masonry.

The source of water for this village is not known. We suspect that
crops were grown and that the economy was agricultural with little de-
pendence on food-gathering. Some animal bones were recovered, and
this fact permits us to assume that hunting and trapping were of mod-
erate importance. Since pottery was present, some cooking was probably
done in pots; but some plant and game may have been roasted.

The social organization may have consisted of one or two extended
families per village, matrilocal residence, matrilineal descent and in-
heritance, and possible exogamous clans.

4. THODE SITE

Most of the foregoing remarks on Chilcott Site 1 would apply here.
The eleven rooms were neither rectangular nor round. The floors were
semi-subterranean, perhaps 20 to 40 cm. below the old ground level; the
base of the masonry walls was on the old ground surface; and the masonry
was composed of unshaped cobbles and boulders set in mud mortar.
(How such walls carried the weight of a roof is a mystery to me!) The
rooms were Clustered near one another but were not contiguous. The ar-
rangement of the rooms makes one think of the informal, unplanned order
of a pithouse village, where each unit is independent of the others. In this
instance, the rooms are closer together, with perhaps only 50 cm. separat-
ing them. The people seem to have drawn closer together. Here one
can sense the beginnings of pueblo architecture in which the rooms
at a later date are arranged in cellular fashion. There was no ‘front’
or ‘‘back”’ to the Thode Site. No ceremonial room was found.

Water for domestic purposes may have been taken from Mineral
Creek. Agriculture may have been practiced although we have no direct
evidence of it. The flood plain would have provided ideal soil and a

218 PREHISTORY OF EASTERN ARIZONA, I

convenient area for fields. Game probably supplemented the vegetable
diet. Food may have been cooked in pottery jars or roasted and broiled
over the fires. Two rooms contained hearth areas and one contained a
firepit.

Sites belonging to this time period (Chilcott and Thode) are fairly
abundant and may represent about one-third (85) of all the sites found on
the survey. A guess as to the population of this period (with a minimum
figure of three people per room and ten dwellings per site) would pro-
duce an estimate of about 2600 persons for the period of A.p. 1200+50
living in approximately 1500 square miles (Springerville—-St. Johns,
Snowflake-Show Low). This estimate is arbitrary, perhaps a bit low.

The survey indicates that the people living in this period (during
which time separate, above-ground rooms with masonry walls were being
placed closer together but not yet in contiguous fashion) preferred (by
about 58 per cent) to build their villages on a knoll or the floor of a valley
adjacent to a stream. Others preferred a point of land jutting into a
valley, a bench on the side of a mesa, or the edge of a mesa overlooking
a stream.

The social organization for the Thode Site may have been similar to
the Chilcott Site: several extended families occupying the village; matri-
local residence; matrilineal descent; and possibly exogamous clans.

5. Rim VALLEY PUEBLO

The rooms of this village are rectangular or square, are contiguous,
and are grouped in two units facing each other on opposite sides of a
plaza. This site and another, Mineral Creek Site (Martin, Rinaldo, and
Longacre, 1961), are among the earliest examples we know in this area
of a ‘“‘pueblo” in the sense that the rooms are contiguous and the floors
are at ground level.

At Rim Valley, the pueblo has no “‘front’’; the rooms are linear
agglomerations. ‘The rooms face inward toward the plaza. The ar-
rangement of rooms seems typical of Mogollon architectural development;
that is, a rather unsystematic cluster of square or rectangular rooms.
To put it another way, if one were a person of Paul Bunyan’s stature and
if one were to square up the amoeba-shaped rooms of the Thode Site
(see fig. 21) and were to push them together so that the rooms were con-
tiguous, one would have a graphic representation of Mogollon villages.
In fact, even some of the later sites, such as Jewett Gap Pueblo (personal
visit), Foote Canyon Pueblo (Rinaldo, 1959) and Kinishba (Cummings,
1940), as well as some of the pre-Spanish Zuni towns, are really nothing

SUMMARY 219

but exaggerated counterparts of the earlier Mogollon villages—groups of
rooms pulled together and irregularly disposed. They are simply exten-
sive house blocks or groups of contiguous rooms, in some cases of more
than one story, but now distributed around a plaza and/or kiva.

Thus, Rim Valley Pueblo is an excellent example of one of the earliest
types of Mogollon villages and exhibits characteristics that hint of later
developments, such as one finds at Hooper Ranch Pueblo (see below).
Although I have conjectured that a span of perhaps 20 to 50 years sep-
arates the Thode Site (a.p. 1200+50) from Rim Valley Pueblo (a.p.
1225+50), this is nothing more than a guess and perhaps is mislead-
ing. The seriation of Rim Valley Pueblo sherds was not satisfactory, but
Freeman suggests (Chap. IV) that the site may be slightly later than the
Thode Site.

On the basis of architecture and village plan, I tend to agree with
this position. But the Thode Site and Rim Valley Pueblo may be nearly
of an age. My reason for advancing this paradoxical suggestion is two-
fold: (1) Rim Valley Pueblo is on the Little Colorado River and therefore
may have been in closer contact with more sophisticated developments
that were going on elsewhere. The Little Colorado River Valley was
undoubtedly a route of travel and trade, and peoples living there would
have been, generally speaking, subject to tendencies of urbanization and
more exposed to the latest fashions. (2) At the same time, the folk of the
area in and around the Thode Site lived in a remote, isolated area, cut off
from innovations. For this reason, the architecture of the two sites differs,
Rim Valley being more ‘‘modern”’ while the Thode Site is more anti-
quated or vestigial; but the pottery types are essentially similar.

This interpretation reverses our usual attitude towards pottery, which
generally is regarded as the sensitive diagnostic criterion for defining and
dating minor chronological divisions of prehistory.

I can venture no other explanation for the apparent differences in
two sites that probably were contemporaneous or nearly so; unless, of
course, my chronology is erroneous. The fact remains, however, that the
pottery types that are generally regarded as good time markers—Reserve,
Snowflake and Tularosa Black-on-Whites and Wingate Black-on-Red—
are present at both sites, though in slightly different proportions.

Our investigations at Rim Valley Pueblo reveal no kiva-building that
was detached from the main blocks of rooms. Since the pueblo was built
on bedrock which was everywhere exposed or was, at best, covered with
only a few inches of soil, it is unlikely that we missed it. Separate kiva-
buildings often seem to be absent from pueblos of this period. It is quite
possible, however, that some of the dwelling rooms might have doubled

220 PREHISTORY OF EASTERN ARIZONA, I

as places for small group ceremonies. In Rim Valley Pueblo, for example,
Room C might have been a place in which ceremonial and secular func-
tions could have been carried on. This room is furnished with a firepit,
a ventilator, a ladder-pit(?) flanked by stone slabs, and the kind of vault
or foot-drum in which one often finds a sipapu. These furnishings,
which are more elaborate than those usually found in dwelling rooms,
have been found elsewhere (see Chap. I, ““SSummary of Secular Archi-
tecture’) and persuaded us to wonder if this room might not have
served also as a kiva.

Water for domestic usage for Rim Valley Pueblo could have been
obtained from the Little Colorado River several hundred feet below.
If nearby springs existed, no sign of them remains.

Although we discovered no evidence of cultivated foodstuffs (corn,
beans, and squash), it is assumed that these crops were grown, prob-
ably in the flood plain of the river that flowed below the houses. Animal
bones were found in some quantity, a fact that makes it probable that
hunting supplemented farming. Firepits were probably used for boiling,
stewing, parching, and roasting vegetables and meat, and for heat and
light. These firepits are centrally located in the rooms, are sometimes
associated with ash pits (the need for and meaning of which are not
clear), and are cunningly placed near a ventilator opening set in the walls.

The favored locations for villages of this class and era and an estimate
of the population for the area under study will be stated in the discussion
of Hooper Ranch Pueblo.

6. GREAT Kiva, Hooper RANCH PUEBLO

The village at Hooper Ranch was a “true pueblo,” an agglomeration
of contiguous rooms clustered about three sides of a plaza that contained
the two lesser kivas (Kivas I and II in Martin, Rinaldo, and Longacre,
1961, p. 32). The village arrangement is similar to Kinishba (Cummings,
1940, map) and other plaza-type (Hawikuh-like?) towns.

There were two stories in the pueblo but we have described them as
consisting of two horizontal levels of occupation, not contemporaneous,
each containing perhaps 60 rooms. Our evidence indicates that the upper
story was built and occupied only after the lower one was abandoned
and filled with relatively clean dirt (containing few sherds or artifacts).
This does not preclude the possibility that there were two stories during
the period of first occupation; but we have little or no evidence to sup-
port such an idea.

It is probable that the rooms faced inward toward the plaza. Whether
this orientation of the village reflects a different kind of social organization;

SUMMARY 221

a tighter kind of village control; a more conservative (inward-looking)
village character; a desire to obstruct the view of “‘foreigners”’ or traders,
who might otherwise profane the sanctified enclosure of kivas by their
glances; or whether it was an attempt to make the village defensible or
cozy, cannot say. This ruin exemplifies in miniature the fruit of Mogol-
lon architectural development that required about a thousand years to
germinate.

The dating of the Hooper Ranch Pueblo is conjectural and not too
satisfactory. We have guessed that the pueblo was constructed and occu-
pied from a.p. 1200 to 1375. A carbon-14 date from the Great Kiva is
A.D. 1230+60 (GRN 3006). The earlier portion of the village may be
contemporary with some of the dwelling units in Rim Valley Pueblo.

Water for the use of the village was certainly not a problem. The
Little Colorado River flowed within 25-75 feet of the pueblo and was,
in all likelihood, a perennial stream, as it is today.

The economy of this site is fairly well worked out from the pollen
study conducted by Schoenwetter (Chap. VIII). Pollen from corn and
squash was identified for the earlier or lower level of occupation. The
pollen of cattail was recovered, and this indicates a nearby swamp or
marshy area. In the later stages of the life of the pueblo, the percentage
of corn pollen decreases. This shift plus others (discussed in Chap. VIII)
may indicate a cultural change or a small fluctuation in rainfall pattern.
An unusual quantity of animal bones in the refuse suggests that the diet
was supplemented to a considerable extent by meats. The presence of
firepits implies, as it did in the other sites, cooking of various kinds—
broiling, boiling, parching, roasting—and a source of light and heat.

Sites of the Rim Valley and Hooper Ranch Pueblo class (38 found on
survey) are less numerous than those in the Chilcott-Thode Sites class (85).
On the whole, most of them (32) are found in the Little Colorado River
Valley and the Snowflake-Mesa Redondo areas, probably because perma-
nent streams were present and crops could be grown nearby. If it can be
assumed that each of these villages averaged about 25 rooms (probably a
low average) with probably three people per room, then I should guess
that the population may have been 75 to 100 people per village; and if
this figure were multiplied by the number of known villages of this era
(38), it would indicate that approximately 3800 people were living about
A.D. 1100-1300 near the Little Colorado River and its tributaries near
Snowflake and Mesa Redondo. I have not forgotten that not all ‘‘rooms”’
were dwelling rooms, that some were used for storage purposes; but I
think this fact would be more or less offset by the fact that most villages
of this period (A.p. 1100-1300) may have contained from 50 to 60 rooms

222 PREHISTORY OF EASTERN ARIZONA, I

each. My figure for density of population is probably inexact, but, if
anything, it may be low. As stated earlier, I regard this sort of guessing
concerning population as useful only in ranking the approximate number
of people per century within our study area. It may be relatively correct,
but is not intended to be a census guide.

The social organization of the Rim Valley and Hooper Ranch Pueblos
may be conjectured to have been similar in many aspects to that of the
towns of preceding centuries. In fact, as we approach the contemporary
western pueblos in time, we may be on surer ground in putting forth our
guesses. The “inward-looking” pueblos may not have been very differ-
ent from what we can observe in Zuni and Hopi towns.

It is probable, then, that within the large pueblos we might find sev-
eral matrilocal families, matrilineal descent and inheritance, and a more
complex grouping.

The absence of an arrangement of structures that would indicate
moiety divisions suggests that there existed a single organizational unit
with perhaps several fraternities that controlled the kivas and the cere-
monies held within them. The presence of the Great Kiva might signify
some sort of supra-village organization made up of priests from satellite
towns who were responsible for the major rites held within this eminent
and august structure.

The remainder of my chapter should, perhaps, have preceded the
summary on the dig and the section on settlement patterns. Or, more
logically, the parts that follow should have been interwoven into my
summary, since my statements concerning settlement patterns and the
conjectures stem from the next sections.

In truth, I could not have created many of my statements nor have
derived hypotheses (climate, crops, number of sites per era, density of
population, and the like) without having liberally drawn on the supple-
mentary data provided by my colleagues. I owe them much. But I
feared that the significance of these superlative reports would have been
buried or wasted. For better or worse, I chose to treat them other-
wise.

The results of three other projects remain, then, to be summarized.
Two of these—the Archaeological Survey Program and the Pollen Analy-
sis Program—were part of our original plan for the 1960 season. Both
of these were financed by a generous grant from the National Science
Foundation. I shall deal with these last.

SUMMARY 223

ANALYSIS OF ELEMENTS OF POTTERY DESIGN

A third project was not conceived until the last weeks of the field sea-
son. The black-on-white sherds from the pithouse at the Goesling Site
(Pueblo I or II) were abundant (final total of decorated sherds about
2000). As we slowly perceived a possible relationship between the de-
signs on them (Kiatuthlanna and Red Mesa Black-on-Whites) and what
we had been calling ‘“‘Snowflake Black-on-White’’ during the season, we
decided to institute a comparative study and analysis of the designs on
these three pottery types. It was hoped that if a genetic relationship
existed, we might be able to confirm it.

Miss Constance Cronin, assisted by Mr. Walter Boyer, then artist in
the Department of Anthropology at the Museum, undertook this compre-
hensive undertaking. In the Preface (pp. 5-6) I have described the
preliminary aspects of this study.

Several striking and unexpected consequences flowed from this study.
The principal one is the suggestion that Snowflake Black-on-White pot-
tery designs are genetically closer to those on Kiatuthlanna Black-on-
White than to those on Red Mesa Black-on-White. I had assumed that
since the pottery called Red Mesa Black-on-White was or might be closer
chronologically to Snowflake Black-on-White, a closer relationship would
exist between these types.

Since this study was made, several experts have looked over our sort-
ing of sherds that we classified as either Kiatuthlanna or Red Mesa
Black-on-White. I got two impressions from their remarks: (1) that our
sherds classified as these types were not truly good representatives of
Kiatuthlanna or Red Mesa Black-on-White types; but that one could
say some were in the Red Mesa style and others in the Kiatuthlanna
style (thus, we did not have “pure”? types with which to work); and
(2) that many sherds that we called Kiatuthlanna types, they would
have classed as Red Mesa.

These observations may modify the conclusions of Miss Cronin but
do not destroy them. A relationship between designs on early Chacoan
ceramics and Snowflake Black-on-White is a possible conjecture.

Since Miss Cronin made her study and wrote her report, I have seen
more Snowflake Black-on-White pottery. In addition to the link between
the designs on Snowflake Black-on-White pottery and those on the two
early Chacoan types, I can see the same kind of tie-up between the former
and the early Kayenta pottery types. This is not startling, because I
think most Southwesterners recognize a basic similarity between the de-
sign elements and design layouts of early Kayenta and Chacoan wares.

224 PREHISTORY OF EASTERN ARIZONA, I

At present, then, the origin, affiliation, and lineage of Snowflake Black-
on-White pottery are not precisely known, but it seems reasonable to con-
clude that this type derives from the Chacoan and/or Kayenta wares.

THE ARCHAEOLOGICAL RECONNAISSANCE

Many results may stem from an archaeological reconnaissance. One
may hope for clues as to climate, drainages and terrains, choice of settings
for sites, arable land, and geological and ecological features. The sur-
veys conducted by Rinaldo (unpublished) and by Longacre (Martin,
Rinaldo and Longacre, 1960) have given us invaluable data. Using
these, we can, among other things, intelligently choose sites for extensive
excavation and we can make guesses concerning population density per
unit of time. Without such source information, we should be working
blindly.

Our study encompasses a large geographical area more or less rec-
tangular in shape. The unit embraces the region from Springerville
to St. Johns, to Snowflake to Show Low, Arizona, plus an extensive tract
in the White Mountains. Approximately 1500 square miles are contained
in these areas and 243 occupational components were found. In time,
these range from ca. 1300 B.c. to A.p. 1300.

From the data given, it is possible to make some inferences.

The favorite location of the prehistoric peoples, regardless of time,
was on a knoll or a ridge on the floor of a valley.

The density of population for the area studied increased from a prob-
able few hundreds per century in pre-pottery times to perhaps about
3800 to 4000 during the centuries from A.p. 1100 to 1300, and then de-
clined until about A.p. 1500 after which time the area was deserted (unless
the Apaches had moved in by this time).

The sites of the pre-pottery era (before A.p. 300) were found in all
geographic positions except in the White Mountains. By a.p. 900, the
central area was almost vacant, but an increase of sites is noted along
the Little Colorado and Show Low-Silver Creek drainage and in the
White Mountains. It may have been the time when a lot of people were
moving into the Point of Pines region south of the White Mountains; or
it may have been a desire on the part of the people to find a location
where sufficient moisture would permit them to farm.

About A.p. 1100-1300, most of the people were living on the two
drainages of the area, with only a few remaining in the White Mountains,
and soon after A.p. 1300 there were only a few large villages left in the
area (six sites in all); these are all on the Little Colorado River or the
Silver Creek River and a few major tributaries.

SUMMARY 220

Schoenwetter’s palynological inquiry (Chap. VIII) supplies possible
explanations for this ebb and flow and abandonment.

During the period that lasted from about A.p. 300 to 1000, the whole
area under study may have been blessed with light summer rainfalls and
heavier winter precipitation. The reserves of ground moisture were prob-
ably greater at that time; and streams—not only the two large ones still
flowing in the area but also many small ones— flowed the year
around. These stream beds are now only deep-cut, dry arroyos. At
about A.D. 1000 and since, the area has received heavy, destructive, tor-
rential rains such as it has today, and probably little of the gentle winter
precipitation (see Chap. VIII for further explanations).

In a very rough way, a correlation can be seen between the density
of population and location of sites that were worked out in Longacre’s
survey, and a shift in environment. After a.p. 1000 or 1100 much of
our area was inhospitable, and farming was difficult, if not impossible.
The results? The people moved to be near the two remaining streams;
and after a.p. 1400-1500, life became too difficult and the people moved
out. Where they went to is another question and it is being investigated.

The survey, then, provided us with data without which we could
neither function as excavators nor serve as interpreters of the evidence
dug up.

POLLEN ANALYSIS

I have found the interdisciplinary co-operation—the palynological in-
quiry by Schoenwetter (Chap. VIII)—eminently worth while, exciting,
and satisfying. We are continuing this approach and hope to expand
it and to use other interdisciplinary studies. It is immensely profitable,
because data thus provided by our colleagues supplement ours and are
essential for providing us with means to interpret the material culture
we dig up.

I have no intention of trying to summarize the pollen project, for this
would create needless bulk and tiresome repetition. Schoenwetter’s ‘‘Con-
clusions’ and ‘Interpretations and Inferences’”’ are admirably stated.
I have already drawn on his data for some of my conjectures.

I shall content myself with drawing attention to a few points that in-
terested me.

The main one is that a shift in environmental conditions may have
occurred at about A.p. 1000. The ‘“‘shift’? to which reference is made
means a seasonal change in amount of precipitation without altering the
total annual rainfall. For example, at present, the Southwest as a whole

226 PREHISTORY OF EASTERN ARIZONA, I

receives the major amount of its precipitation in the summer months.
Summer rains are dynamic and destructive because they fall in great vol-
ume in a short time and with great intensity. Such heavy torrential rains
(‘‘gully-washers”’ as they are locally called) cause old streams (now dry
arroyos) to run furiously for a few hours. Arroyos are deepened and wid-
ened by such action. In addition to carrying off top soil and dissecting the
lands and mountain sides, most of the water rushes off downstream and is
carried off to the Little Colorado and to Lake Mead so quickly that little
soaks into the ground. Thus, wells are not replenished, the water table
is lowered, springs dry up, and the trees and plants profit very little from
these summer thunderstorms.

Conversely, precipitation that occurs during the fall and winter
months tends to be entirely beneficial. The rains are gentle and often
of several days’ duration; the snows, of course, are better than rains,
even though they may not remain on the ground more than a few hours
or days. The melt therefrom soaks into the ground and is entirely con-
structive. It is believed that winter precipitation replenishes wells and
mountain springs, tends to perpetuate streams, and keeps the water table
high. It is possible, of course, to have the annual precipitation evenly
divided, more or less; but even under this condition winter precipitation
is more useful to plants, animals, and man. Thus a “‘shift’’ in the pattern
of rainfall may mean a change from dominant winter precipitation to
dominant summer precipitation; or vice versa; or from one of these
maxima to rainfall that is more or less evenly divided up throughout
the year.

It is postulated that the shift in the microclimate in the Vernon area
(at least) that occurred about A.p. 1000 was not a favorable one. The
evidence at hand suggests that the rainfall pattern of prevailing winter
precipitation shifted to one of preponderant summer precipitation. ‘This
spelled doom to the farmers, many of whom were in a “‘marginal”’ position.

Here, then, one has a possible explanation of the movement of peoples
and of the abandonment of certain areas previously occupied. A cycle
of preponderant summer rainfall would create an unfavorable environ-
ment for growing crops. Perennial streams probably disappeared and
springs dried up. The explanation of these conditions is clearly given by
Schoenwetter (Chap. VIII, pp. 194-195).

Relinquishment of certain areas has been noted in our archaeological
work in the Pine-Lawn—Reserve, New Mexico, areas and also in our re-
searches in the Vernon area. It is assumed that the people moved to
nearby but more favorable places. To me this is most satisfying because

SUMMARY 227

we now appear to have a possible explanation for such movements of
people—an explanation that is based on observation and good deductions
rather than on wild guesses.

From the evidence at hand, four major periods of differing environ-
mental conditions can be recognized from the pollen data. These periods
are characterized by differing frequencies of pollen types, not by absolute
differences in them. The four periods of different environmental con-
ditions are vividly and briefly shown (Table 21, p. 199), and ample
defense for Schoenwetter’s point of view is given.

In his final section, Schoenwtter bolsters his thesis of environmental
changes by brief references to developments and movements of peoples
in the areas inhabited by the Anasazi, the Cohonina, the Point of Pines
people, and the Sinagua. In this section, he discusses the Athapascan-
speaking peoples, their way of life, their aggressiveness, and the effect
they might have had on the sedentary Pueblo farmers. He does not say
that the Athapascans displaced the Pueblo farmers. He suggests that
the Apaches and Navahos might have served as a cultural barrier to the
Pueblo peoples if the latter had attempted to move back into their old
haunts if and when environmental conditions had improved in their old
home lands. This provides a reasonable answer to a question that has
always bothered me; namely, why did not the Indians of the Hopi and
Zuni refuge areas expand and move back to the Show Low, Snowflake,
Springerville, Pine Lawn and Reserve areas? I like this hypothesis and
shall use it until it is weakened by new and contradictory data.

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234 PREHISTORY OF EASTERN ARIZONA, I

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Index

Abajo Red-on-Orange, 105

Abrading stones, 135; grooved, 132

Acoma kivas, 66

Adobe, 28; calking, 214; clay, 48, 54;
plaster, 46, 62

Agogino, George, 155

Agriculturalists, 201, 204, 205, 206

Agriculture, 200, 215, 217; beginnings of,
164, 165; dry farming, 202; economy,
196; expanding, 166; Mogollon area,
191; see also Irrigation

Alder, 174

Alma Plain, 150, 159

Alnus, 173, 174

Alschuler, William, 4

Altars, Hopi (Marau, Wuwutcim, Tala-
tumsi and Marau-mana ceremonies), 72

Amaranthus, 174, 186, 200

Amargosa II points, 155

Anasazi, 160, 166, 167, 227; Chacoan,
214; culture, 63, 144, 201, 202; Great
Kivas, 60, 66, 67, 68, 214; irrigation
system, 203; lesser kivas, 65, 66, 68;
tradition, 64, 66; traits, 163; see also
Pueblo III sites

*“Antechamber,”’ 36, 37

Antevs, Ernst, 122, 196

Anthropomorphic figure; see Image

Apaches, 224, 227; Western, 205

Arboreal plants, 173; pollen, 179, 181,
183, 185, 186, 188, 189, 191, 194, 195,
196, 206

Archaeological Reconnaissance, 224; re-
search, 4; survey area, 149; survey pro-
gram, 222

Architectural, development, Mogollon,
221; traditions, 69

Arizona W:10:51, 144, 145

Arizona W:10:52, 60, 124

Armillas, Prof. P., 168

Arms, Bernard C., 171, 177, 185, 197

Arrow-shaft, smoother, 132; straightener,
‘352 tools, 132,155; 147

Arroyo-cutting hypothesis, 196, 197, 198

Arroyo bank, 206

Arroyo sites, 177

Artifacts, 115-147; stone, 210, 211

Ash pits, 63, 66

Athapascan-speakers, 205, 206, 227

Awatovi, 66; murals, 73, 74

Awls, bone, 139, 141; bone splinters, 139;
split long-bone type, 139; ulna type,
139, 147

Awl-sharpening stone, 48

Axe-grinding slab, 129, 131

Axes, stone, 115, 127, 129, 130; full-
grooved, 115; three-quarter grooved,
129, 147; tabular, 129

Axis, secondary, of kiva, 66

Aztec Ruin, 145

Babocomari Village, 140

Baker, O. E., 201

Baldwin, Gordon C., 145

Banquettes, 66

Barreras, Wilfred, 4

Bartlett, Katherine, 146

Basalt, boulders, 20, 32, 45, and cobbles,
25, 56

Basket Maker III sites, 60

Beach sites, 116, 122, 155, 156, 163, 164,
178

Beads, 58, 71, 214; olivella, truncate, 144;
stone and shell, 140

Beals, Ralph L., 105

Beams, 50, 59, 64, 65; main, 37

Beans, 68

Bench, 51, 54, 58, 60, 64, 66, 68, 213

Bin, 55, 63; corner, 47, 48

Binne-Ettini Canyon, 174

Black Mesa Black-on-White, 105, 106

Blades, 130, 132, 134, 138; fragments, 158

Blue River, 60, 64

Bluff Site, 61, 116

Bluhm, Elaine A., 64, 106, 164; see also
Sawmill Site

Bodkins, 139, 140; tip, 141

Bone, awls, 139; effigy pendant, 140; frag-
ment, incised, 141

Boreal economy, 205, 206

Boyer, Walter, 5, 106, 223

Bracelets, shell, 140, 144; fragments, 143

Brainerd, George W., 87, 105, 107

Brainerd-Robinson, method, 107; ratios,
114; see also Robinson-Brainerd tech-
nique

Brand, D. D., 126

Brawley, Elizabeth, 5

Breternitz, David A., 60, 62, 63, 64, 124,
125,132, 138; 139, 157

237

238

Brinkerhoff, Mr. and Mrs. Wayne, 5
Brown indented corrugated, 79
Bryan, Kirk, 205

Bunzel, Ruth L., 69, 71, 77

Buttress, 51

Cactaceae, 174

Cactus family, 174

Cahone Canyon sites, 60

Canyon Creek Ruin, 129, 145

Carbon-14 dating, 211, 221; see also
Charcoal

Carter, Mr. and Mrs. J. R., 5

Casa Malpais, 60

Cattail, 177, 195; pollen of, 221

Caywood, Louis R., 140, 146

Cedar, 177

Ceiling, 50; see also Roof

Ceramics, 68; materials, 76; traditions,
69; see also Chacoan ceramics

*“Ceramic Group,” 150; see also Pre-
ceramic site

Ceremonial, objects, 145; use, Room C,
Rim Valley, 51, 53, 220; room, 217

Ceremonies, group, 220

Ceremony, contemporary, 68; hypotheti-
cal, 68

Chaco Canyon, 50, 174; Great Kivas, 66

Chaco district, 115; tradition of Anasazi
culture, 63, 68

Chacoan Anasazi, 214

Chacoan ceramics, early, 223, 224

Charcoal, 178, 211, 215

Chase, Ellen, 4

Cheno-am, 178, 179, 180, 181, 183, 185,
186, 188-191, 194-198, 206; definition
of, 174

Chenopodiaceae, 174, 186

Chilcott, D., 4

Chilcott Site 1, 30, 31, 32-34, 36-37, 62,
7185295, 1072 108. M09 11S s1to> St.
136, 137, 138, 140, 142, 145, 146, 216,
217

Chilcott Site 2, 35, 37, 95, 107, 109, 146,
216

Chilcott Site 3, 35-38, 62, 95, 216

Chilcott Sites, 3, 29-38, 61, 116, 119, 124,
218; intra-site seriation, 95; pottery of,
77, 80, 102; settlement pattern, 216;
summary, 212; totals of sherds, 82;
trends in painted pottery types, 97

Childbirth water house, Tihkuyiki, 67

Chinking, 44, 54

Chiricahua Apache, 205

Chiricahua Stage, Cochise culture, 122

Choppers, 129, 130, 131, 147, 161, 162;
biface type, 130; included with axes,
130; uniface type, 130

Cienaga Site, 116

Cienaga soils, 197

Circle Prairie Phase, 64, 132

PREHISTORY OF EASTERN ARIZONA, I

Cleome, 172, 174, 182, 183, 184; serrulata,
174

Climatic changes, 191-194

Climate, clues to, 224; shift in micro-, 226

Cochise, Wet Leggett, 61; culture, 116,
122, 177; industries, 156

Coefficients of similarity, 90, 107, 108

Cohonina, population movements, 203,
227

Collecting season, 163

Colorado Plateau, 148

Colton, H. S., 71, 105, 150, 204

Compositae, 174, 178-181, 183, 185, 186,
188, 191, 194-198

Concho, Arizona, 29, 138

Concho Complex, 156, 157, 165

Construction of house, tools for, 128

Contamination of soil samples, 171

Cooking, 215, 220, 221

Corn, 68, 165, 177, 215, 216; growing sea-
son, 201; pollen, 215, 221

Cosgrove, H. S. and C. B., 72

Cotton, 177

Counting and identification of pollen, 172

Cox, Mr. and Mrs. Tom, 6

Crooked Ridge Village, 121

Crushing tools, 120

Crypt, 57-58, 59, 64, 67, 71, 73, 74, 214;
wall, 66; double cover, 67; meaning of
aperture, 73

Cucurbita, 174, 182, 183

Cult deity, 71, 74; Alosaka, 72; female
character of, 73; Hopi figurines, 73; re-
lation to underworld, 73, 74; Tuwapong-
tumsi, 73; Talatumsi, 73; concerned
with childbirth, 73

Cultigens, 173, 183, 184, 200

Cultural influences (pottery), 103

Cultural lag, 115

Culture and environment, relationship
between, 169

Cummings, Byron, 73, 218, 220

Curb (or lip), 20, 24

Cylinder stones, 145, 147

Cyperaceae, 173, 174, 183, 185, 190, 195,
196

D-shaped pithouses, 26

“Damper,” 36; slab, 49

Danger Cave, 156

Danson, E. B., 60, 164, 212

Defense systems, 210

Deflector, 34, 56, 57, 58, 64, 65, 68, 115,
21

Deity, cult, 71; see also Cult deity

Desert Culture, 155, 156, 163, 164, 165

Design elements, analysis of, 105-114, 223;
pottery, 75, 105, 163, sorted by, 106,
107; at given sites, 112-113; names and
code numbers of, 110-111; trends in,
109

INDEX

Dimensions of rooms, 32, 43

Di Peso, Charles C., 140, 144, 145

Directional colors, 69

Dockstader, Dr. Frederick J., 6

Dolls, 74; older flat type, 72

Donnelly, Maurice, 203

Doors (at Kintiel), 67

Doorways, 46

Drainages, clues to, 224

Drift, general, in pottery design changes,
77, 108; linguistic, 108

Drills, 135, 138, 139, 147; in very early
levels, 139

Dry farming, 202, 204

Dry Prong Site, Great Kiva, 65, 66, 68

Dwelling rooms, 53

Economic plants, 173, 181, 182, 185, 190

Economy, Tumbleweed Canyon Site, 215;
Chilcott Sites, 217; Thode Site, 217-218;
Rim Valley Pueblo, 220; Hooper Ranch
Pueblo, 221

Effigy pendant, bone, 140

Effigy; see Image

Eggan, Dr. Fred, 6, 74

Elden Pueblo, 145

Entrance, 20, 25, 28, 66; spirit’s, 67; type
of, 64, 65

Entryways, lateral, 65, 67, 68; ramp, 57,
58, 213

Environmental, change, definition of, 194;
conditions, pre-existing, 194; periods,
190, 191; shifts, 202, 203, 204, 225, 227

Environments, prehistoric, 198-206

Ephedra, 174, 185

Erdtman, Gunnar, 171

Erosion controls, 204

Exogamous clans, 217, 218

Extended families, 218

Extraction techniques (pollen analysis),
171

Faegri, Knut, 171

Female symbol, yellow, 22

Fennell, Agnes McNary, 6

Fewkes, J. Walter, 67, 71, 72, 73, 146

Field, President Stanley, 6

Figurine; see Image, 214

Fireboxes, 62, 63

Firepits, 19, 20, 22, 24, 25, 28, 34, 37, 38,
40, 46, 48, 49, 51, 55, 57, 62, 66, 68,
126, 220, 221; area, 65; circular, 60,
62; small, 68

Fireplace, 60

Fire screen, 68

Flagstaff area, 140, 145, 146, 204

Flakes, utilized, 135

Flattop Site, 157

Floor plan, shape of, 64, 68

Floors, 19, 22, 23, 28, 32, 33, 37, 40, 48,
54, 61

Flour receptacles, 47, 48, 63, 122

Food preparation, tools, 115-126

Foot drums, 68; see also Vaults

Foote Canyon Pueblo, 126, 129, 218;
plaza, 65

Forest, 174, 188, 189, 191, 195, 200, 205,
206; re-growth, 206

Forestdale Phase, 138

Forestdale Site, 116, 138

Forslev, Dr. Albert, 6

Four Mile Polychrome, 214; bowls with
anthropomorphic figures, 73

Four Mile Ruin, 67

Frazier, Vernon, 5

Furnishings, interior, 62

Geochronology Laboratories, 168, 171

Gila River, upper, 134

Gillespie, Mr. and Mrs. Charles, 6

Gillespie, Mr. and Mrs. Leon, 6

Gillespie, Mr. and Mrs. Milton, 6

Girders, 37, 65; see also Beams

Gladwin, Harold S., 65, 105, 140, 144,
145

Globe mallow, 177

Goesling, Al. H., 4

Goesling Site, 3, 26-29, 131, 137-143,
146, 223; intra-site seriation, 94; pot-
tery of, 77, 78, 80, 102, 107, 108, 109,
120, 122, 125, 128, types by levels, 92,
totals of sherds, 81; settlement pattern,
216; summary, 212

Goodman, Mr. and Mrs. Donald, 6

Goodman, Joe, 4

Goosefoot family, 174

Gramineae, 177

Grand Canyon area, 203, 204

Grass family, 177

Grasslands, 173, 188, 196

Great Kiva, Higgins Flat, early, 65;
Hooper Ranch Pueblo, 3, 52, 53-60,
64-68, 115, pottery of, 77, 80, totals of
sherds, 85-86, stone discs, 125, west
wall, 71; see also Hooper Ranch Pueblo

Great Kivas, 161, 162; comparisons of, 60;
Mogollon, 67; Village of the, 60

Gregg, Dr. Clifford C., 7

Grinding stones, small metate-like, 124

Groningen Laboratory, 178, 211, 212,
2155221

Gurley, C. E., 6

Haas, Dr. Fritz, 6

Hahn, Mr. and Mrs. Maxwell, 6

Hammer, grooved, 129; see also Maul

Hammerstones, 48, 126

Hargrave, L. L., 145

Harvest cycle, 163

Harvey, Byron, III, 6

Hastings, James R., 205

Hatchways (at Kintiel), 67

Haury, Emil W., 61, 64, 65, 76, 116, 122,
129, 130, 138, 140, 145, 155, 178, 212

240

Hawikuh, 65, 145

Hawley, F. M., 126

Hearth, 68; area, 65, 66; raised, 60

Herod, David, 4

Heshota-uthla Polychrome, 80, 214

Hester, E. D., 155

Hibben, F. C., 126

Higgins Flat Pueblo, 60, 65, 124, 181, 186;
Great Kiva, 65, 68, 169, 185, 188, 190,
119i

Hilltop Phase, 61, 122

Hodge, F. W., 65, 145

Hohokam, 65, 145

Hoijer, Harry, 205

Hooper Ranch Pueblo, 3, 52, 60, 63, 103,
119) 120) 125-131e 134-1445 146.82;
184-190, 219, 221; intra-site seriation,
99; trends in painted pottery types, 101;
Great Kiva, 65-68, 125, 132, 136, 138,
140, 145, 182, 183, 187; settlement pat-
tern, 220-222; summary, 213-215

Hooper, Rob., 4

Hopi, culture, 167; Indians, 227; cult deity
figurines, contemporary, 73; kivas, lesser,
66; similarities, image, 69, 71; towns,
222

Horizon markers (pottery), 88

‘‘Horizon styles’? (pottery), 75

Houck Polychrome, 80, 213

Hough, Walter, 60, 64, 130

Household utility tools, 135-139

pores see Construction of Houses, tools
or

Human effigy; see Image

Hunting, and gathering, 198, 200, 201,
215; and warfare, tools, 130-139

Hygric plants, 173, 181, 182, 183, 185,
190, 195

Image, stone, 57—58, 59, 67, 69-74, 145-—
146, 214; description of, 69; female
character, 72

Interdisciplinary co-operation, 225

Irrigation, 201, 202, 203, 205

Iverson, Johannes, 171

Jacal construction, 62

Jar, miniature; see Miniature jar
Jeddito area, 119, 146

Jelinek, Arthur J., 90, 106
Jennings, Jesse D., 155, 156, 201, 203
Jewett Gap Pueblo, 218

Judd, Neil M., 115, 132, 146
Juglans, 173, 177, 184

Juniper, 177, 179

Juniperus, 173, 177, 178, 179, 180

Kachina-kihu, 66

**Kachina”’ niche, 51

Kachina, proto-, 71, 73, 74

Kachinas, mother of, 67; Citulilu, 72;
Patun (Squash), 72; Rainbow, 72

PREHISTORY OF EASTERN ARIZONA, I

Kana-a Black-on-White, 105, 106

Kayenta pottery types, early, 223, 224

Keney, Dr. Charles W., 6

Kent, Kate Peck, 139

Kiatuthlanna Black-on-White, 102, 105-
109, 150, 212, 213, 2235 design ‘ele-
ments, 109

Kidder, A. V., 66, 119, 146

Kinishba, 60, 73, 144, 218, 220

Kintiel, 67

Kittle, Mr. and Mrs. Jake, 5

Kiva, 51, 220; -building, 219; entrance,
73; lesser, Anasazi, 65; Zuni, 66

Kivas, Anasazi type, 51, 60; circular, 162,
163; Western Pueblo type, 53, 60, 64

Knives, 132; flake, 135, 137, 147, 158

Kwakina Polychrome, 85, 214

Ladder pits(?), 48, 49, 51, 62, 63, 220

Laguna Salada, 61, 155, 178, 186, 191,
198

Lambert, Marjorie F., 6, 146

Lane, Gardner, 4

La Plata Black-on-Orange, 105

Lehmer, Donald J., 87

Leverton, Mr. and Mrs. John D., 5

Lexico-statistics, 205

Lino Gray, 150, 159

Lintel, 36, 46

Little Colorado River, drainage, 50, 51,
105, 145, 147; upper, 63, 115, 120, 130,
157, 184;"Valley;, 195265 40,5355:
134, 148, 151, 161, 162, 164, 182, 210,
219, 221, 224

Little Ortega Lake, 116, 155, 178, 186,
LOT 9s

Los Muertos Site, 140, 145

Lyman Dam, 210

Lyman Reservoir, 19

Malde, H. E., 60

Mallow family, 177

Malpais rocks, 22

Malvaceae, 177

Manos, 20, 48, 116-119, 122, 126, 147;
beveled, 147, 177; grinding surface,
119; flat-tabular, 117; loaf-shaped, 117;
on earlier sites, 116; one-hand, 116,
117, 118, 146; two-hand, 116, 117, 147

Marau ceremony, 72

Marau-mana ceremony, 72

Martin, Paul S. (Arizona), 4, 168, 174,
177, 185, 197, 204

Masauwu, 67

Mask, 71

Masonry, 32, 43, 50, 56, 67, 68, 210, 212;
banded, 50, 115; composite construc-
tion, 33; jacal construction, 62; rubble,
61, crude, 36, 61, random type, 32, 37,
44, 54, regularly coursed, 54; through
stones, 33, 40, 43; Type I, 44, 45, 46;
Type II, 44, 45; veneer, 59, 66, 68;
vertical slab, 44, 54, 60

INDEX

Matrilineal descent, 217, 218, 222

Matrilocal families, 222; residence, 217,
218

Maul, 127, 129, 147; full grooved, 129;
tabular, 129; three quarters grooved, 129

McDonald Corrugated, 78, 79

McGregor, John C., 140, 145, 146

Medicine cylinders, 128

Mesa Redondo, 148, 162

Mesa Verde, 203

Metate, 48; fragments, 20

Metates, 122-124, 126, 147; troughed,
116; 1185 122)123,1475 basin, 116,122,
123, 147; slab, 118, 124; flat, 122

Microclimate, shift in, 226

Migrations, 224-227

Milling area, 20, 24, 25, 62

Milling stones, 62, 126

Mimbres Polychrome, bowl, female fig-
ures in yellow, 72

Mindeleff, Victor, 65, 66, 67

Mineer, Mrs. Leola, 5

Mineral Creek, 40, 217

Mineral Creek Pueblo, 60, 62, 63, 67, 162,
182, 186, 187, 190, 218

Miniature jar, 58, 59, 71, 142, 214

Modified Basket Maker period, 124

Mogollon, agriculture, 191; architectural
development, 221; area, 126, 130, 132;
culture, 129, 144, 163, 166, 167, 191;
Great Kivas, 65, 67, 68, 214; ideas, 166;
migration, 160; pithouses, 65; pithouse
kivas, 66; San Simon Branch, 120;
techniques, 164; tradition, 64, 161;
Tularosa, 214; villages, 218, 219

Mogollon Rim, 169, 204

Mormon tea, 174

Morris, E. H., 60, 66, 144, 145

Mortars, 26, 33, 37, 40, 45, 124-125, 126

Movement of peoples, 227; see also Mi-
grations

Muriyinmana, 67

Muriyinwu, 67

Naegle, Mr. and Mrs. Cecil, 6

Nantack Phase, 64

Nantack Village, Great Kiva, 60; Ruin B,
62, 65, 124

National Science Foundation, 3, 5, 148,
210, 222,

Navahos, 227

Navaho sand paintings, 72

Nesbitt, Paul H., 73, 132, 144

Niches, 46, 48, 54, 55, 64, 66, 67, 68;
-cache, 67, 73; “‘Kachina,”’ 51; phallic,
67; wall, 68

Novak, Lillian, 6

Nuarez, Genaro, 4

Nuclear families, 216

Oak, 177, 179
Olson, Alan P., 63, 64, 65, 66, 67, 212
Open house, 5

241

Opler, Morris E., 205

Orientation, eastward, 67, 68, 213; north-
south, 66, 67; primary, of Great Kiva,
64, 65, 68; village, 220

Ornaments, 140

Padilla, Gilbert, 4

Paint grinding, 126; red, 51

Palynological laboratory, 168; inquiry, 225

Parklands, 173, 188, 189, 191, 195, 196,
200

Parsons, Elsie C., 67, 69, 71, 72

Passageway, 37

Peckham, Stewart, 62

Pecos, 146; Classification, 150

Penasco Phase, 122

Pendant, bone, 143, effigy, 140; bone and
shell, 140; clam shell, 143; limestone,
white, 143; turquoise, 143

Pendants, tinkler, conus, 147; unfinished,
140, 143

Penrod, Mr. and Mrs. Floyd, 6

Penrod, Kenneth, 4, 6

Penrod, Mr. and Mrs. Leonard, 6

Pepper, George H., 144

Percussion flaking, 126; chipping, 130, 136

Perry, Martha, 4

Pestles, 120-122, 126; cylindrical, 120;
multiface, 120, 122; pear-shaped, 120,
122

Phipps, Mr. and Mrs. Claude, 6

Pictographs, 54, 69, 73

Pigments, grinding of, 126

Pigweeds, 174, 200

Pillars, 65

Pinedale, 145

Pinedale Black-on-White, 151

Pinedale Polychrome, 151

Pine Lawn, area, 164, 169, 180, 181, 185,
186, 188, 191, 196, 227; Phase, 61, 122,
132; Valley, 161

Pinnawa series, 214

Pinto Basin, 156

Pinto Point, 155

Pinus, 173, 177-180; edulis, 173; ponderosa,
173

Pinyon, 173

Pithouses, 212; D-shaped, 26

Pithouse village sites, 178, 200

Pits, 19, 22, 29, 34, 54, 58; resonator, 67;
storage, 25, 26; sub-floor, 180

Plaiting, 140

Plants, common names, 174

Plaster, 26, 33, 45, 54, 62; adobe, 46, 62

Plateau, 203, 204

Platform, 51, 66

Platyopuntia, 174

Plaza, 43, 65, 218, 220

Point of Pines, 60, 61, 63, 64, 122, 124,
125, 132, 139, 204, 206; people, 227;
region, 224

Polishing stones, 126

242

Pollen analysis, 3, 168-208, 221, 225; pro-
gram, 222; chronology, 169, 189, 190,
198; extraction technique of, 207-208;
types, common names, 173, frequencies
On 227

Population, 200, 201, 215, 216, 218, 221;
density of, 224, 225; increase, 204;
movements, Cohonina, 203, 227

Postholes; 20; 22;°25,295 33534, 37459) 675
double, 59

Posts, 37, 65; recessed, 54, 59

Pot covers, 125, 127, 147

Pot rest stone, 48

Pot rests, 126, 147

Pottery, black-on-white, 115; hachured,
115; lack of, 116

Pottery-making, tools, 126

Pottery, design elements, 75, changes in,
76, 77; “horizon styles,’ 75, 77; ‘‘intru-
sive,’ 76; methodological considerations
(statistics), 88; miniature jar, 58, 59;
painted, statistical analysis of, 75; petro-
graphic analysis, 76; relationships be-
tween types, 107, 108; relative positions
of samples, 90; seriation, 80, 87, 88, 93,
94; size of sample, 89; stylistic changes,
77, drift in, 77; temporal sequence of
sites, 88, 89; ‘‘trade,” 76; trade, Ana-
sazi, 201; trends in design elements,
109, in painted pottery types, 97;
whole (or restorable ), 78; see also
Design Elements

Pottery types, Abajo Red-on-Orange, 105;
Alma Plain, 150, 159; Black Mesa
Black-on-White, 105, 106; brown in-
dented corrugated, 79; Four Mile Poly-
chrome, 73, 214; Heshota-uthla Poly-
chrome, 80, 214; Houck Polychrome,
80, 213; Kana-a Black-on-White, 105,
106; Kiatuthlanna Black-on-White,
102, 105-109, 150, 212, 213, 223; Kwa-
kina Polychrome, 85, 214; La Plata
Black-on-Orange, 105; Lino Gray, 150,
159; McDonald Corrugated, 78, 79;
Mimbres Polychrome, 72; Pinedale
Black-on-White, 151; Pinedale Poly-
chrome, 151; Red Mesa _ Black-on-
White, 78, 102, 105-110, 150, 212, 223,
later, 110; Reserve Black-on-White,
LOZ OS Of WSO. 212. 215 AOaSt:
Johns Polychrome, 80, 151, 213, 214;
Snowflake Black-on-White, 5, 75, 78,
LOZ, VOS-MO NSO N 2125 20S 2195 225°
design elements, 110, lineage of, 75,
224; Sosi Black-on-White, 105; Tula-
rosa Black-on-White, 102, 103, 105,
LO7,, 151, 2125 213-214. 219 ularosa
White-on-Red, 213; Tusayan White
Ware, 163; White Mound Black-on-
White, 102, 150; Wingate Black-on-
Red, 103, 150, 213, 214, 219; Woodruff
Smudged, 78

PREHISTORY OF EASTERN ARIZONA, I

Powamu, ancestral to, 68

Prayer sticks, 134

Pre-ceramic site, 211

Precipitation pattern, 193; winter, 225,
226; see also Rains

Procedure, field, 151; statistical pottery
analysis, basic, 90

Projectile points, 130-132, 133, 147, 158;
diagonal notched, 132; barbed, 147;
triangular, small, 147

Promontory Site, 61, 169, 179, 180, 181,
185, 186, 188-191, 206

Proto-kachina, 71, 73, 74

Pueblo, dwelling units, 200, 201; early
example of, 218; farmers, 227; sites,
181-185; true, 220

Pueblo I sites, 60; III sites, 60, 119, 174;
IV sites, 119

Pueblo Bonito, 68, 144, 146

Pueblo Indians, contemporary, 72

Punches, 135, 138

Quemado area, 68
Quercus, 173, 177, 179
Quiburi, 144

Rafters, 20; see also Roof supports

Rain farmers, 201, 203

Rains, summer, 193, 196, 197, 198, 201-
205, 226; winter, 193, 197, 198, 201;
see also Precipitation

Rands, Robert L., 77

Red Mesa Black-on-White, 78, 102, 105—
109, 150, 212, 223; design elements,
109, 110; later, 110

Red paint, grinding, 51

Reed, Erik K., 201, 203

Reiter, Paul, 66, 67, 68

Relative chronological order of sites and
rooms, 89

Reserve area, 51, 60, 61, 63, 64, 119, 120,
1225 1245 1125513251385 1395227

Reserve Black-on-White, 102, 105, 107,
150,212 213219

Reserve Phase, 61; late, 50

Reserve-Tularosa series, pottery, 163

Resonators, 67

Rhoton site, intra-site seriation, 94; pot-
tery of, 77, 102

Rhoton, Verl, 5

Richey, Leigh, 5

Riley, Carroll L., 205

Rim Valley Pueblo, 3, 40-53, 62, 63, 117—
122, 124-131, 136, 138-141, 143, 146,
182, 190, 213, 218, 221; intra-site seria-
tion, 98; pottery of, 77, 78, 80, 102, 103,
106, 108, 109; Room C, 51, 220; settle-
ment pattern, 218; summary, 213; totals
of sherds, 84; trends in painted pottery
types, 97

Rinaldo, Mrs. John B., 4, 106

INDEX

Ring, bone and shell, 144, 147; fragment,
143; material, 141; slab, 47, 57, 214

Rio Grande area, 119, 134

Ritual circuit, directional colors, 69

Robbins, Wilfred William, 174

Roberts, F. H. H., Jr., 60, 66, 67, 124,
129° 152.203

Robinson, W. S., 87, 107

Robinson-Brainerd seriation technique,
87; criticism of, 87; choice of, 87; co-
efficient of similarity, 90; basic pro-
cedure, 90

Romane, Pat, 4

Roof, 20, 22, 25, 29, 37, 40, 59; crib-like,
61; supports, 64, 65, 68; timber, 130

Room shape, 62

Rubbing stones, 119-120, 147

Rubble; see Masonry

Sackheim, Judd, 6

Sacred stone image; see Image

St. Johns, 19, 148, 224

St. Johns Polychrome, 80, 151, 213, 214

St. Johns-Salt Lake Highway, 26

Salix, 173, 177

San Cayetano, 144, 145

San Francisco levels, Tularosa Cave, 140

San Francisco Phase, 138

San Francisco River, 181, 186

San José, 156

San José Point, 155

San Simon Branch, 120; Village, 144

Sapir, Edward, 108

Saul, John, 4

Sawmill Site, 60, 65, 68

Saws, 135, 136-139; smooth, 138

Sayles, E. B., 61, 65, 116, 120, 122, 144

Schroeder, A. H., 204, 205

Schulman, Edmond, 206

Schwartz, Douglas W., 203, 204

Scraper-planes, 136

Scrapers, 131, 132, 135, 136, 147, 158-
161; gourd, 126; large, 136; oval biface,
130; small, 136, 137

Secular structures, 60; use, Room C, Rim
Valley, 51, 220

Sedge family, 174, 195

Sediment samples, 170

Seriation, pottery, 80; inter-site, 93; intra-
site, 94; technique, 87

Settlement patterns, 69, 164, 200, 215-222

Shell, beads, 140; bracelets, 140; pendant
(with bone), 140; ring, 140, 147

Shells, Pacific Coast, 115

Shelter, light brush, 61

Shipaulovi, kivas, 65

Show Low, 29, 148, 224, 227; area, 152

Show Low Black-on-Red, 150

Show Low-Silver Creek drainage, 224

Sichomovi, 67

Sills, 46

243

Silver Creek, 166; see also Show Low-
Silver Creek

Similarity; see Coefficients of Similarity

Sinagua, 204, 227

Sipapu, 51, 220

Site 481, 68; Site LS-4, 180, 187, 191;
Site LS-24, 185; Site LS-28, 181, 190,
191; Site LS-34, 185, 187, 190; Site
LS-50, 180; Site 30, 62, 169, 180, 186,
188, 191, 206; Site 30-31 arroyo, 186;
Site 31, 61

Site locations, 152, 164, 200, 201, 216,
218, 220; favorite, 224; pre-pottery, 224

Slabs, 54, 55, 59, 65, 122; image, 58; per-
forated, 67; ring, 47, 57, 67; sandstone,
455,55; 215; stone, 51, 5, 02,.0550240.
worked, 67

Smiley, Terah L., 4, 60, 168

Smith, Watson, 66, 68, 71, 72, 73, 105,
146

Snaketown, 140, 144, 145

Snowflake, 148, 162; region, 163, 227

Snowflake Black-on-White, 5, 75, 78, 102,
105-110, 150, 212, 213, 219, 223; de-
sign elements, 110; lineage of, 75, 224

Snowflake-Mesa Redondo, 152, 221

Social history, 211; organization, 216,
217, 218, 220, 222

Soil zones, 197

Sosi Black-on-White, 105

Southern Illinois University, 168

South Leggett Site, 181

Spicer, Edward H., 140, 146

Spindles, 134

Spindle whorls, 139, 140, 142, 147; of
Mexican derivation, 140

Springerville, 19, 40, 53, 60, 148, 224, 227

Squash, 174; kachina, 72; pollen of, 221

Statistics, lexico-, 205

Stephen, Alexander M., 67

Steppe zone, 192, 194, 202-205

Stevenson, Matilda C., 71

Stewart, G. R., 203

Stone, bowls, 125; discs, 125 (see Pot cov-
ers); tools at pithouse village, 210, 211

Storage pits(?), 25, 26, 62, 215; tech-
niques, 164

Stradling, Frank, 4

Strassburger, Roland, 4

Sudatories, 68

Summer rains, 193, 196-198, 201, 203,
204, 205, 226

Sunflower family, 174

Sunset Crater, 204

Supra-village organization, 222

SU Site, 116, 121, 146, 169, 179, 185, 188

Table Rock Pueblo, 60, 63, 67, 124, 126,
145, 169, 184, 185, 190

‘Talatumsi ceremony, 72

Taylor, Dr. Walter W., 168

244

Technique, of pollen extraction, 207—208;
of sample collection, 206

Te’ewi, 146

Temporal sequence of sites (pottery), 88

Terracing systems, 204

Thode, Earl, 4

Thode Site, 3, 38, 39, 40, 61, 62, 118, 120,
125; 13051356, 139, 140, 1415 1455219;
pottery of, 77, 78, 80, 102; settlement
pattern, 217; summary, 212-213; totals
of sherds, 83

Thomas, Tully H., 156, 157

Thompson, Raymond H., 212

Three Circle Phase, 64

Three Pines Pueblo, 62, 124

Tihkuyi, 67

Tihkuyiki, Childbirth water house, 67

Tinkler, conical, 145, 147

Titiev, Mischa, 71, 73

Trade, evidence of, 115; pottery, Anasazi,
201

Trait unit intrusions, 115

Trewartha, G. T., 192

**Triangle,”’ 151, 166

Tseh Tso, 126

Tularosa Black-on-White, 102, 103, 105,
107, Tote 212 1s 214209

Tularosa Cave, 140, 155

Tularosa Mogollon, 214

Tularosa Phase, 63, 132; early, 50; end of,
51; tradition of the Mogollon, 68

Tularosa White-on-Red, 213

Tumbleweed Canyon Site, 3, 19-26, 61,
ji Ws es eo is Ws nd 2 es hae is ps ls Ye ley
136, 137, 157, 164, 165, 166, 178, 188,
190, 191; settlement pattern, 215-216;
summary, 210-211

Turkey Foot Ridge, 65, 180, 185

Tusayan White Ware, 163

Tuwabontumsi, sand altar woman, 67

Tuwabontumsiki, phallic niche-cache, 67

Tuwapongtumsi (a cult deity), 73

Tuzigoot Ruin, 140, 146

Twin Butte site, 124

Typha, 173, 177, 183, 184, 185, 190, 195,
196

Underworld; see Cult deity
Urbanization, 219

Vaults, 48, 51, 56, 57, 60, 64, 66, 67; foot-
drum type, 51, 220; masonry-lined, 115,
214; north (yellow pigment), 71; south-
ern, 67, 68; use of, 68; western, 67

Ventana Cave, 116, 156, 178

Ventilator, 36, 37, 46, 48, 49, 51, 59, 62,
63, 66, 220

PREHISTORY OF EASTERN ARIZONA, I

Verde Valley, 205

Vernon, 61; area, 5, 169, 178, 180, 186,
189, 191, 196; project, 6

Vestigial architecture, 219

Village control, 221

Villages, form of, 61, 212

Vivian, Gordon, 66, 67, 68

Voth, H. R., 66, 69, 71

Waard, Dr. H. de, 211

Walnut, 177, 182

Walls, 19, 20, 23, 26, 32, 37, 40, 45746;
53, 217; defense systems, 210; exten-
sions of jacal construction, 62

Warfare and hunting, tools, 130-139

Wasley, William W., 212

Water, standing, 195, 196, 202; tables,
197, 198, 200, 201, 204, 226

Weaving tools, 139-140

Weed, tolerated, 174

Welch, Dr. Walter B., 168

Wells, John, 4

Wendorf, Fred, 63, 124, 125, 132, 139,
144, 145, 146, 157, 158, 212

Western Pueblo kivas; see Kivas

Wetherill Mesa, 174

Wet Leggett arroyo, 169, 177

Wet Leggett Cochise, dwelling area, 61

Wet Leggett site, 116

Wheat, Joe Ben, 64, 121, 122, 132, 139

White Mound Black-on-White, 102, 150

White Mountains, 148, 152, 224

Whiting, A. F., 174

Whiting, Mr. and Mrs. Eben, 6

Wikwalobi kiva, 67

Willey, Gordon, 77

Willis, Mr. and Mrs. Ira, 5

Willis, Kelley, 5

Willow, 177

Wilson, Ozie, 5

Wilson, Mr. and Mrs. Richard, 5

Wiltbank, Pacer, 4

Wingate Black-on-Red, 103, 150, 213,
214, 219

Wodehouse, R. D., 171

Woodbury, Richard, 119, 146, 204, 206

Woodland, Bertram J., 6

Woodruff Smudged, 78

Wuwutcim ceremony, 72

Wuya, clan, 71

Wyman, Leland C., 72

Kea, 173, 177, 179-184, 190; 191, 196

Zoogamous pollen type, 174

Zuni area, 145; culture, 167; Indians, 227;
kiva, 66; similarities, image, 69, 71;
towns, 22, pre-Spanish, 218

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