SMITHSONIAN INSTITUTION LIBRARY INSTITUTE OF SOCIAL ANTHROPOLOGY PUBLICATION NO. 7 CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA by ROBERT C. WEST SMITHSONIAN INSTITUTION INSTITUTE OF SOCIAL ANTHROPOLOGY PUBLICATION NO.7 ~ CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA by ROBERT C. WEST Prepared in Cooperation with the United States Department of State as a Project of the Interdepartmental Committee on Scientific and Cultural Cooperation One of a series of monographs describing the results of the joint field investi- gations of the Institute of Social Anthropology and the Escuela Nacional de Antropologia of Mexico in the Tarascan area of Michoacan, Mexico, 1945-46 —.————————————————————————————— UNITED STATES GOVERNMENT PRINTING OFFICE e WASHINGTON :1948 For sale by the Superintendent of Documents, U.S. Government Printing Office, Washington 25,D.C. - - - ---+-+-++-+ee28 6 Price 75 cents LETTER OF TRANSMITTAL SMITHSONIAN INSTITUTION, InstiTuTE oF SoctaL ANTHROPOLOGY, Washington 25, D. C., June 13, 1947. Srr: [Ihave the bonor to transmit herewith a manuscript entitled “Cultural Geography of the Modern Tarascan Area,’’? by Robert C. West, and to recom- mend that it be published as Publication Number 7 of the Institute of Social Anthropology. Very respectfully yours, Grorce M. Foster, Director Dr. ALEXANDER WETMORE, Secretary of the Smithsonian Institution. Preface. __-_- Iphoneticmotes.—2 oe =) eee CONTENTS Thesmodern Tarascan. areas -=._---.---2--=-===- Tarascan population—____ The physiographic areas____-__ ~~~ Climateiand vegetation--—~—.=-- _-- --=-.—_ = The recession of mative: evan Modern linguistic distributions______- Tarascan settlements _----___-- ee oe eae IEOUSeHUYIDCS= = 22 = eee eo ea een The land system and the pueblosos2 22 sse225- Tarascanveconomy====-~ == 2222522252822 22 - ee QaQOorwnre SHO AOANOARWN Agricultural systems and associated crop types- Field agriculture and associated crops___- Monbiculnlte saan = aes ee eee PAGE Vv VI Tarascan economy—Continued Bibliography----__-- Stock raising and animal products___-__-___-- Food- patie ae ecuvitles en ee Sigs Fishing... Be Re ee ee ee umbering activities: =_- =. 229) 225) sae andicraftis=--=- So - 2 @Weramics=. 2. 225 2k oe ee chextiles= 22 a5 == ee ee AS Soe ees Wooderafts=—-2---.53 Lacquer work _______- Leathercraft______ 2 Metalcraft ___- Stonecutting_____ Trade and transport __ ILLUSTRATIONS PLATES (All plates at end of book) . Physical landscape. . Water supply and settlement. House types. House types. . Maize culture. Wheat culture. . Horticulture and domestic animals. . Fishing and forest exploitation. . Ceramics. . Ceramics. Pottery making at Cocucho. Pottery making at Cocucho (con- tinued). . Textiles. . Textiles. . Woodwork. . Markets and transport. FIGURES . Decline of Tarasean population, 1500—1940____ . Growth of population in the Sierra, 1750-1940_ aelarascan planting tO0lss=s==-—5— eer a= ase = . The T‘apdératdirakua irrigation device__-____--_ ae Lhedishyspearseandfisqa_ =. see = 2-2 se Srbhegwheellathesea=s a= ee eee eS SS PAGE 22 23 37 48 52 68 . Distribution of MAPS . Topographic map of the modern Tarascan area_ . Geognostic map of the modern Tarascan area__ . Length of frost season in northwest Michoacdn_ Climati¢e map of Michoac4n=_.--_--------=.- Vegetation types in the modern Tarascan area Soil types in the modern Tarascan area_______ . Pre-Conquest and modern boundaries of Taras- Can speecht. == ==. eee {8 . Area of Tarascan speech, ca. 1750________---- . Area of Tarascan speech, ca. 1800____-------- . Area of Tarascan speech, ca. 1850__- ~~ --- oaEe , Area.of Tarascan’ speech, 1940._> -=2=-2222== . Distribution of Tarascan speech by settlements, . Distribution of monolinguals in the Tarascan area 19408250252 so: 3 ee . Distribution of La Cafiada settlements, 1580 and. 19462222. 3232-2 222 eee ePlanvof Uringuitiro,, 194622 = — 3: See . Plan of Ahuiran, =ePlan of irindaro, 04 G2e= see =e ee . Distribution of house types in the Tarasecan 194625. 22. S22 eeee ee e ares sl 78oandel94Gr cee e. = ee eee handicrafts in the modern Tarascan area . Distribution of markets and their local trading territory in the modern Tarascan area------ 1m PREFACE The present study was done under the auspices of the Institute of Social Anthropology, Smith- sonian Institution, Washington, D. C., and in cooperation with the Escuela Nacional de Antro- pologia, Mexico, D. F. The study proposes to serve as a background for the various detailed pueblo monographs executed in the Tarascan area by other members of the Institute. Being a report on the cultural geography of a region, the present paper is chiefly descriptive, although a developmental treatment has been employed wherever the scanty historical materials would permit. Physical background is only briefly considered; emphasis is on material culture, particularly modern Tarascan economy: agricul- ture, handicrafts, and trade. In addition, an attempt is made to describe the areal recession of Tarascan speech since Spanish contact. Field work was done in April, May, and June of 1946. With the exception of Cherandtzicurin, all Tarascan towns were visited. Many neigh- boring mestizo pueblos (formerly Tarascan) were inspected to obtain comparative data. Approxi- mately two-thirds of the field season was spent in the Sierra. Archival research was done in the Archivo del Arzobispado de Michoac&n, Morelia, the Archivo General de la Nacién, Mexico, D. F., and the Museo Nacional de Antropologia, Mexico, D. F. I am especially indebted to Sr. Pablo Valasquez G., a native Tarascan and anthropology student, who accompanied me in the field. His intimate knowledge of the Tarascan Sierra, its language, and many of its customs was an invaluable aid, not only in the field, but also while the report was in preparation. Velasquez read a large part of the manuscript and corrected the use and spell- ing of all Tarascan words employed in the text. Rosert C. West. Mexico, D. F. March 1947. PHONETIC NOTE The phonetic symbols used conform to the Tarascan alphabet approved by the Congreso de Filélogos y Lingitistas of México in 1939 and employed by the Tarascan Project of the Departamento de Asuntos Indigenas. The alphabet is based on standard Spanish usage insofar as possible, with additional symbols added for Tarascan and with some clarification of the Spanish symbols as indicated below. The vowels a, e, 7, 0, u have Spanish values. The vowel a is intermediate between Spanish t and u. The consonants b, d, f, g,j, k,l, m, n, p, 7, s, and t have regular Spanish values. In addition the following symbols are used: is the equivalent of English or Spanish ts. is the equivalent of English ch. is used for the sound of English vg in “‘sing.”’ is the equivalent of French j. is intermediate between Spanish l and r. is the equivalent of Spanish rr. is the equivalent of English sh. is the equivalent of English z. ‘ &, k‘, p‘, and ¢‘ are aspirated forms of the consonants given above. Mm & HS BR Org OD _ —, e tava eae al got ae Wing = vd Willa Jiménez rajomonsaie 3 Be ‘ H 0 ' dae } f ‘ £ Tanganofcuoro / re 1) a % ©.DEEA ALBER a eel \v \ a “La Wontera L-- Ko a : 7 S-—s8000— > yi - ase, gfoptevare eA) aad £3 a a ae San José em j at) ' fa MS ° ~ a Los Ganoas IONACIO. ‘OR Tipidio Gres Sec ae | — y sree soles mie, ) 2 i via 3 S if Wieden hgaw a ’ ‘one n~. pTifguindin } | we f uv Ss ‘y > bat Santo nr Fr Gu j 0, Tocumbo ! Hi ' \ ; ~cherén ee ant ne ‘| (one axAWpana Zipcitos | 2 t 7 . bZsonBenito 1 Aeiees {Rancho Nuevo, i Peicciehs f CELA ALBERGA ‘ & % ra jes ‘ / \ ce 4 = wy ‘ so me Tee Ahuiron s/f . ( sa Sicvichoy | M4 co ‘ Boon ; Fi at | vase Bhardan, - om , s Me Nahuatzen va M5660 Chefatog seRANJUATA oy 4 sabe «) “ 4 o> 1) 2, 4 eed ~ . J gXxuian “* ° Se! (pagotdcuarsy, 7 a %~, ” fe Ae eT . ((/DE SAN MARCOST; CDE LA VARA oo ii Pomacuordn fr j ’ a we A + Me \ ( ~ / Naplzorog- ~ rongérfeuard ve Sli IF ae buSrey A Neen, ek” pio Siago° “VS UATRER! H ‘ ) ‘s~, NG:DESGHIVOIE aroeutin “Pog uare! Nocutzepoo, ed toa ee \ Capacuaro/ AS me 1 lit, Lat (yes whta's. 900 y ( ELA ¢ RONA) Y, we EL REY VALIENTE! SS Ne IN ftom \ a) ie SY *s 19" Tingambato, aw ' \ ’ A aa Huiramangaro\ San Juan Tumbio' 7 ; Sim aa ') 6 9écom “\ ‘ ‘ RINDO . SX Uruapan Coltzontyin cob OO me el FS \ ne SAN LORENZO a / Ea ens \ \ Sox open Oe oy : j dToretan \ ms TARASCAN PUEBLO MESTIZO PUEBLO TARASGAN RANCHO MESTIZO RANCHO sm ALL-WEATHER HIGHWAY —— ORY SEASON AUTO ROAD owm= TRAIL +++ RAILROAD ra f * Toneitaro ~ 2 "i c4 Le, sees o Oe Ario de Ragalés Cosil¥e ) a) 7 sok. — ~~ Nillo Silva 7 [ 2 AREA OF maP 8rco. dees Boncos Contour interval 1000 feet 748988 O - 48 (Face p, 1) Map 1.—Topographie map of the modern Tarascan area. 6 he Janitziog v —Oardeuaro 2 ape 101° 30° '° Iratzio @Cucuchucho *~ @thuotzi a tee Cle Um dampo 1 Aelled leny(SPaNTaKu E27 cuonojo: ertanacou) af ee Sa rf ( cae Frisch — oe er OS Fiseent ¢ vec punto wee oe { ©-DEL Yugo | pYAMEL % H as = BARRA 101°30° Cultural Geography of the Modern Tarascan Area By Rosert C. West THE MODERN TARASCAN AREA The present territory of Tarascan speech con- sists of a relatively small area (about 3,500 sq. km.) in northwestern Michoacan. Approximately, the modern area extends eastward from the Zamora-Los Reyes railroad to the east shore of Lake PAtzcuaro, and southward from the M éxico- Guadalajara highway to a line drawn between Patzcuaro and the peak of Tancitaro (map 1).! A few small islands of Tarascan-speaking folk exist south of the main area. Within the present area nearly 55,000 individuals of indigenous speech live in 66 Tarascan pueblos and 50 ranchos. Four geographical regions comprise the modern Tarascan area. (1) The Sierra (called by the Tarascans Sierra or Siéris) is the largest of the regions, the main portion of which extends west- ward from Lake Patzcuaro to slightly east of the Zamora-Los Reyes railroad.“ The northern ! Map 1 is based on an enlarged portion of sheet 643A (Uruapan) of the AAF Preliminary Base, 1:500,000. This sheet was compiled by the U. 8S. Aeronautical Chart Service in January 1945 from AAF trimetrogon photog- raphy taken in December 1942. Positions and names of topographic fea- tures which appear on the accompanying map were checked on the ground during the spring of 1946. Some errors were encountered on the original map: misnamed localities (e. g. Ajuno), small errors in routes of highways and railroads, mistakes in elevations. Drainage was found to be fairly correct. Onmap1only the more important trails are indicated. Numbered localities refer to the following ranchos: 1. Guarachanillo. 14. San Maros Aracht- 27. Patambicho. 2. Aranza. cuta. 28. Ojo de Agua. 3. Las Trojes. 15. Huancho. 29. Ichupio. 4. Las Cafias. 16. Las Cocinas. 30. Tarerio. 5. El Venado. 17. San Nicolas. 31. Ucasandstacua. 6. Tapan. 18. La Alberca. 32. La Vinata. 7. Tierras Blancas. 19. La Atascada. 33. Las Granadas. 8. La Mesa. 20. El Rosario. 34. Yunuén. chars 21. El Tepemal. 9. La Tinaja. 22. Tepetate 35. Tecuena. 10. Queréndaro. 23. Tejamanil. 36. Urandén Morales. 11. Zarzamora. 24. Pacdpatiro. 37. Urandén Morelos. 12. San Luis Sorena. 25. Chupicuaro. 38. Urandén Carian. 13. La Jolla. 26. Oponguio, 39. E] Padre. The following Tarascan ranchos (listed in the official 1940 census) are not located: Tzintzicha (municipio of Chilchota); Agua Escondida (municipio of Tangancicuaro); Las Encinillas and Los Laureles (municipio of Tanga- mandapio); La Providencia and El] Tropezén (municipio of Los Reyes); El ‘Tejocote (municipio of Paracho); Revolucion (municipio of Erongaricuaro); and Itziparamucu (municipio of Tzintzuntzan). 1a On modern maps the high area west of Lake Patzcuaro is termed “‘Sierra de los Tarascos.’’ In colonial documents the area was usually called ‘‘Sierra de Michoacan.”’ boundary approximates the México-Guadalajara highway, while the steep escarpment that plunges into the Balsas-Tepalcatepec Basin marks its southern limit. An eastward extension lies south and southeast of the lake and joins with the Sierra de Ozumatlan in eastern Michoacan. Containing 60 percent of the present indigenous group, the Sierra west of the lake is the modern center of the Tarascans. (2) The Lake Patzcuaro (Japinda.zu, Inéimecuatu) area contains 19 percent of the Tarascan population distributed in 13 pueblos and 13 ranchos along the lake shore and on the islands. Formerly one of the political centers of the Tarascan Empire, the lake region, in terms of indigenous speech, has declined rapidly since late colonial times. The speech of the entire south shore and the towns of Quiroga, Tzintzuntzan, and Erongaricuaro is predominantly Spanish. North and northeast of the Sierra lie two small areas of indigenous speech, which appear to be remnants of the once large northern Tarascan zone. One of these is (3) La Canada (EréSeman), a small narrow valley located at the northern edge of the Sierra. This valley was the region of the ‘‘onze pueblos” of colonial days. Today nine towns with 9 percent of the total Tarascan population are clustered along a strip of alluvium within the valley. (4) The other remnant of the northern zone lies north and northwest of Lake Patzcuaro and contains seven pueblos and 9.5 percent of the total number of Tarascan-speaking folk.2 Other regions of Tarascan speech consist of “islands” south of the main area. Cuanajo, located southwest of Mo- relia in the western extension of the Sierra, is the Jast fragment of the former indigenous area south- east of Lake Patzcuaro. San Angel Zurumucapio and the newly formed towns (Caltzontzin and Villa Silva) harboring refugees from the stricken 2 These pueblos include Tirindaro, Tarejero, and Naranja on the shore of former Zacapu marsh; Azajo and Comanja on the northeastern edge of the Sierra; Teremendo and Zipiajo at the northern foot of Cerro el Zirate. ry 2 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7 zone around Paricutin Volcano, are the remaining predominantly Tarascan settlements in the tierra templada, the upper part of the plateau escarp- ment (2 percent of Tarascan population in 1940). Formerly an important part of the Tarascan Empire, the hot lands of the Tepalcatepec and Balsas Basins (tierra caliente, Jusio) have lost completely the last vestige of spoken Tarascan. A small number of Tarascan-speaking folk live in some of the larger mestizo towns adjacent to the main Tarascan area: Uruapan, Patzcuaro, Coeneo, Zacapu, Zamora. With the possible exception of a few old households in Uruapan, the presence of aboriginal speech in the large mestizo settlements probably represents a recent influx from rural areas (a desire for urban life, migration from the voleano-devastated areas) rather than linguistic remnants. THE PHYSIOGRAPHIC AREAS The Sierra.—The Tarascan “Sierra” is not a mountain chain; it is rather a volcanic plateau, whose average elevation is some 1,500 feet higher than that of the surrounding areas and whose surface has been roughened by large composite volcanoes, scores of small cinder cones, and ex- tensive lava flows (malpais). Lying within Mex- ico’s transcontinental volcanic axis, the Sierra is the locale of the country’s newest active volcano, Paricutin.’ Within the central part of the area elevations range from 6,900 feet to over 12,660 feet (Cerro de Tancitaro). The altitude of the plateau increases from west to east. Elevations of towns in the western half of the Sierra range from 5,180 feet (Atapan) to 7,800 feet (Pamaté- cuaro);in the eastern half, from 8,040 feet (Sevina) to 8,460 feet (Cumachuén), the highest pueblo in the Sierra west of Lake PAtzcuaro. Even higher settlements (e. g. the rancho of Cruz Gorda, 8,987 feet) exist southeast of the lake, and the highest point in Michoacan, the Cerro de San Andrés (12,840 feet), lies in the Sierra de Ozu- matlin, 62 km. east of Morelia. Tertiary and Quaternary vulcanism has pro- duced the major land forms in the Sierra (map 2). In age the volcanic forms range from probably Eocene to the present time. The oldest are mas- sive composite volcanoes, the highest and most 8 The chief scientific references on the Paricutin Voleano include Ordéiiez (1945), Robles Ramos (1943), Pérez Pefia (1946), Mexico City Universidad Nacional Instituto de Geologia (1945). prominent landmarks in the area: Cerro de Tancitaro (12,660 feet), Cerro de Patamban (12,300 feet), Cerro de Quinseo (10,800 feet), Cerro el Zirate (10,955 feet). The flanks of these mountains are composed mainly of andesite with some pinkish rhyolite near the summits; small veins of mineral-bearing quartz sometimes occur within the andesite. Conical shape and radial drainage characterize these voleanoes, but most craters have been destroyed by erosion. Fre- quently erosion of soft consolidated ash situated between andesite flows has formed caves, which have acquired importance in Tarascan folklore. Cinder cones and lava flows, Pleistocene to Recent in age, represent the younger forms in the Sierra. The entire area is dotted with cones, 250 to 700 feet high, with no apparent alinement. Most are composed of semiconsolidated ash, cinder, and large blocks of explosion remnants. Two types of cones occur: (1) the symmetrical cone with a well-developed, flat-floored crater, and (2) the breached cone, with one side partially destroyed, initially by explosion or lava flow and subsequently by erosion. Some cones are ribbed by radial drainage; others carry scars of surface slips; owing to porous surface materials, a few show little effects of erosion, in spite of high (35°-45°) angle slopes. Basaltic lava flows, originating usually from Pleistocene or Recent fissures in the sides of old volcanoes or occasionally from large cinder cones, have descended slopes in narrow corridors and have fanned out in wide expanses on gentle eradients. Fantastically rough surfaces charac- terize the flows, which form the Sierra’s badlands— agriculturally unproductive and barriers to horse and wheeled traffic. Comparative age of the flows can be roughly determined by the degree of rock decomposition and character of vegetation cover. In some flows, such as that south of Pomacuaran, depressions and crevasses are par- tially filled with alluvium; large areas are covered with a thin soil mantle; sizable pines and oaks cover most of the flow. These features evidence a long period of exposure. In contrast, the rough, blackened, almost treeless malpais north- west of Zacapu at the Sierra’s northern edge, appears to be a much younger flow. Volcanic activity in the Sierra has possibly been continuous from Eocene to the present day. Jorullo (1759) and Parfcutin (1943) represent 102°30 Map 2.—Geognostic 1 (malpais). (4) Le of stream alluviu oe en ae rn ar a 102° 30° id oa he Torecuato wake Patambon Pomatdcuaroo | fo Cocucho ot Urapicho, A e Ms ¢ <= oAhuiran Sicuichog | =® ° Choropaneee @ eo? ae ee s oAngahua “hee e e ©Zirosto e e ° Peribon : A o e A De , Oo f eg Q oO * of 2 mroageifeaera see » ° PGtzcuaro \ go GD) A ) aot Guanajot ow Wd Santa Claraom—" Y 101" 30° (2) Recent cinder cones. Data from aerial photographs and field notes. (3) Recent lava flows (5) Large flattish-floored basins 7148988 O - 48 (face p. 2) CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—WEST 33 historical examples of vulcanism within or ad- jacent to the area. However, vulcanism associ- ated with human ancient settlement in the area, is unquestionably evidenced by the occurrence of charred maize ears embedded in a basaltic lava flow 18 km. northwest of Morelia.* Aside from land forms resulting directly from vulcanism, others caused by depositional processes occur within the Sierra. Between the old com- posite volcanoes and young cinder cones flattish surfaces have been formed first by ash and cinder fall and later by aeolian and alluvial deposition from surrounding slopes. Such surfaces, which compose only a small percentage of total land area, are the agriculturally important sections of the Sierra. Some form saddles or cols between adjacent hills; the larger plains form basins of interior drainage. The largest basins are Llano Grande, southeast of Charapan; the Plan de Nurio; that of Paracho, Aranza, and Cheran; the plain of Nahuatzen; of Sevina; of Paracho; ete. (map 2; pl. 1). Minor forms include dissected aprons of alluvium and semiconsolidated ash at the base of volcanoes and steep-sided arroyos eroded into alluvium in the upper parts of the basin plains. One of the most characteristic physical features of the Sierra is the paucity of perennial streams and lakes. Although this is an area of moderate summer precipitation, the porous volcanic surface quickly absorbs most of the available moisture. A few permanent, spring-fed streams occur on the northern and western flanks of Cerro de Patamban and on the western and southern sides of Cerro de Tancitaro. Small springs occur on the flanks of the old composite volcanoes, whose porous rocks form a reservoir of rain water. Such springs afford the sole water supply for many Sierra villages. Only on the edges of the Sierra plateau, at the contact of porous and impervious rock layers, do large springs occur. The Lake area.—At the eastern edge of the Sierra exists a depression filled by Lake P&tzcuaro. Sierran geomorphology (young and old volcanic forms) almost surrounds the lake, but predomi- nates on its northern, western, and southern shores. Twelve kilometers south of Pétzcuaro small Lake Zirahuén, within the eastern prong of the Sierra, appears to have been formed by a lava-blocked 4 An excellent specimen of charred maize so embedded is in the Museo Regional Michoacano, Morelia, stream.’ Both lakes present similar shore fea- tures—moderately steep banks alternating with wide, flattish delta fans. In other respects the two lakes are distinct. Patzcuaro is shallow (deepest point in the southern arm, 20 feet; in the northern part, 50 feet, in 1941); Zirahuén is relatively deep (148 feet, maxi- mum sounding). Moreover, while the level of Zirahuén (6,953 feet in 1942) is relatively stable, that of Patzcuaro (6,671 feet in 1942) has fluctu- ated frequently in historical times. Since 1939 the lake level has descended nearly 4 feet, exposing large areas of mud flats along the shore and re- vealing one new island (Pastora) near the south- west corner of the lake (pl. 1). In some places the descending waters have uncovered old tree stumps, indicating that formerly the lake level was even lower than at present. On the other hand, the western portion of the large lacustrine plain of Chapultepec in historical times formed an eastward extension of the lake’s southeast arm, denoting a former level higher than the present one.® The cause of flucuation in level is not clear. De Buen (1944), judging from meteorological data (1939-43), has suggested a correlation between rainfall and evaporation variation on the one hand and lake surface fluctuation on the other. The excessive evaporation and low rainfall during those years likely affected lake volume, but normal precipitation and evaporation in following years have not halted the gradual decrease in lake level. Moreover, if fluctuation is caused by meteorolog- ical elements, one would expect neighboring lakes to be similarly affected. Periodic clearing and clogging of sublacustrine crevices, often associated with lakes of volcanic origin, is another popular hypothesis applied to Lake Patzcuaro. The lake contains 10 islets on which live some of the most conservative of the Tarascan people— the fishermen. The four islands off the Taafu-k*éri Peninsula (Pacanda, Yunuén, Tecuena, and Janitzio) are old volcanic hilltops with steep banks and, with the exception of flat-topped Pacanda, with little land suitable for cultivation. In the 5 De Buen (1944) assigns the origin of all present and former lakes in the western Portion of the Mesa Central to disruption of normal drainage by vuleanism. He also suggests that Lakes Patzcuaro, Zirahuén, Cuitzeo, and Yuriria were formed from portions of Rio Lerma drainage, since the fish Chirostoma, abundant in Lake Chapala and the Lerma, is found also in these lakes, the number of species decreasing from Chapala (10) to Zirahuén (2). 6 The 16th-century map of Lake PAtzcuaro which accompanies the Relacién de Michoacan (1903) clearly shows the former extent of the southeastern arm. At the time of the Conquest this section included the island of Aputato, now a hill some 300 m, from the water's edge. 4 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7 shallow southern part of the lake lie JarAcuaro, the largest of the group, and the newly formed Pastora. (The former island of Copujo is now attached to the mainland.) Both islands are low, composed of semiconsolidated alluvial materials. Along the southern shore only low marsh now separates the Urandén islets (low voleanic hills) from the mainland (pl. 1). The southern escarpment.—Although geologi- cally similar to the Sierra, the abrupt southern escarpment, which forms part of the Mesa Central’s southern wall, constitutes a distinct physiographic area. Pleistocene and Recent vulcanism continues from the Sierra to the Balsas and Tepalcatepec Rivers, Jorullo having been the most recent volcanic activity on the escarpment. The canyons formed by deeply entrenched spring- fed streams are the escarpment’s salient features. Some barrancas exceed 500 feet in depth. The upper tributaries of the escarpment streams are eroding headwardly into the Sierra, capturing enclosed basins and intermittent water courses.’ Above the barranca area shallow basins occur in the upper portion of the escarpment. Probably of volcanic origin, these flattish-floored valleys are now tapped by escarpment streams. Typical examples are the plains surrounding Uruapan, those below Periban and Los Reyes, the valleys of Tingambato and Tacambaro, all important sites of former Tarascan settlement in the tierra templada. The northern plateau area.—The former Taras- can area north of the Sierra forms part of the interior plateau county of Central Mexico. For the most part physiography is characterized by old volcanic hills and mountains separated by flat to rolling plains country. The part of this region formerly inhabited by Tarascans extends from Lake Chapala east to the Sierra de Ozumatlan and from the Sierra north to the Lerma River. (The low areas near the river and its tributaries are often termed the ‘Bajio.”’) A narrow belt of the hill and plains landscape also extends south from Lake Chapala to include the Cotija-Tin- giiindin area along the western side of the Sierra. Average elevations in the interior plateau decrease from 7,200 feet along the flanks of the Sierra de Ozumatlin to 5,000 feet at Lake Chapala. The 7 For example, this phenomenon has occurred at the southwestern edge of the Sierra, where a tributary of the Tepaleatepee has apparently captured the drainage of the structural basin which runs east-west from Parangaricu- tiro to Periban. higher hills and mountains rise 2,600 to 4,000 feet above the surrounding plains. The young volcanic land forms found in the Sierra are lacking in much of the northern area, where the principal elevations consist of eroded composite Tertiary voleanoes. A few tongues of Recent lava flow from the Sierra into the northern edge of the plains, and cinder cones extend north- ward from El Zirate. Many lakes, some cecupy- ing structural basins, dot the northern area. The extensive sections of old alluvium, which form a good part of the plains, probably represent beds of Pleistocene lakes. At the northern and north- western base of the Sierra many spriag-fed lakes and marshes existed in historical times, e. g., Ciénaga de Zacapu, de Tangancicuaro, de Chapala, ete. The lacustrine basins and the borders of the former lakes and marshes were the major areas of Spanish settlement in the Tarascan North, for both afforded year-round pasture and _ sites for irrigated wheat farms. Some marshy sections still exist, but natural desiccation and artifical drainage have converted much of the wet area to dry farmland. The once extensive chain of lakes in the Cotija graben, west of the Sierra, has almost completely disappeared, and the marshes of Zacapu, around which are grouped a few rem- nant Tarascan pueblos, have been converted into a large farming area. A unique physiographic subarea of the northern zone, called “La Canada,” a narrow east-west depression at the northern base of the Sierra, is still one of the significant Tarascan regions. The valley floor, 10 km. long and 2 km. wide, decreases rapidly in altitude from 6,360 feet at its eastern end to 5,840 feet at Chilchota, near the western extremity (pl. 1). The western end of the valley is marked by an ancient lava flow, which once partially blocked normal drainage. Subsequent deposition of alluvium (possibly lacustrine) behind the lava dam has resulted in the present wide flattish floor of the valley’s western half. Today the stream draining the valley flows subsequently through a deep gorge cut through the northern end of the lava flow. The numerous intermittent streams which descend from the adjacent hills have built up small alluvial fans along the valley sides. Like other areas at the edge of the Sierra, La Canada is favored by numerous large springs issuing from fissures at the southern and eastern borders of the depression. Alluvium and water rn CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—WEST oO have attracted human settlement to the valley since prehistoric times. Sierra Tarascans, who ‘all La Cafiada “ErdéSemen”’ (view from above), probably visited the valley for chile and early maize before the Spanish Conquest. Spaniards immediately seized the well-watered plains near Chilchota for wheat fields. Today La Cafiada is a garden spot of orchards and wheat fields amid recky volcanic hills. CLIMATE AND VEGETATION Meteorological data.—In dealing with meteor- ology, northwestern Michoacan will be treated as a whole; attempts will be made to point out regional differences in temperature and rainfall. Meteorological stations in the area are few; data are entirely lacking for the Sierra. Consequently, only general statements can be made concerning the weather and climate of modern Tarasca. 102°30. Zamora 60 / F ©o Chilchotans [e} ° al eharapane \ S\/ -u OD S072. o Tarecuato fe} 2 Zirosto CDE TANCITARO 102°30' Map 3.—Length of frost season in northwest Michoacsn. Annual temperature ranges throughout the area are small.§ Lowest winter temperatures occur in the Sierra, the Tarascan tierra fria, where noctur- nal freezing and frosts are common from November to March ® (map 3). Winter temperatures in the northern plateau and Lake P&tzcuaro areas are somewhat milder then those of the Sierra (January avereges: Zamora, 16.2° C.; Zinapecuaro, 15.9°; Paétzcuaro, 13.9°), and the number of days with frost is smaller. winters of the upper escarpment (tierra templada) are frost-free (Jan- uary average for Uruapan, 16.0° C.). The Summer § Data from seven stations in the area give annual temperature ranges from 3.9° C. (Hacienda Tequecsran, 10 km. south of Uruapan) to 7.7° C. (Zacapu). The meteorological data given in text are taken from Atlas climatolocvieo de México (Mexico, Servicio meteorlogico mexicano, 1939). ® The mining town of Tlalpujahua (elev. 8,500 feet), on the eastern border of Michoacan, 140 km. east of PAtzeuaro, may afford temperature data similar to that of the Sierra. December and January are the coldest months, with average monthly temperatures of 11.8° and 11.5°, respectively. Maxi- mum temperatures occur in April and May (15.0° and 15.9° C.). whieh are probably somewhat lower than those occurring in the Sierra. 101°30' Coeneo oO ° 5150 2p o Quiroga ° Sonto Juana ° Tacdmboro 101°30' Isopleths indicate the average length of annual period in days, in which frosts oecur. . Data are mainly from reckonings by local inhabitants. 6 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7 temperatures are high over the entire Tarascan area, but less so in the higher Sierra. The warmest months are April and May, the period immediately before the rainy summer (May average temperatures: Zacapu, 19.1° C.; Uruapan, 22.4°; Zamora, 23.2°; Cuitzeo, 23.2°; Pdtzcuaro, 19.9°). Precipitation in the area, as in most parts of Mexico, is seasonal, 80 percent of the annual total falling mainly as convectional thunder- showers in June, July, August, and September. In the Sierra the summer rains often continue as drizzles for a period of 3 to 4 days, suggesting local cyclonic origin. Occasionally during the months of December and January light winter rains, called cabafiuelas, or janingerkua, occur. These rains prevail over most of western Mexico when cyclonic disturbances over the Pacific reach inland, a condition which occurs every 3 or 4 years.'° Such precipitation often falls as snow on the higher volcanoes in the Sierra, such as Tancitaro, Patamban, and Quinseo. Freak snow storms have been recorded in historical times; in September 1887 several inches of snow fell in the vicinity of Charapan and San Felipe, caving roofs and destroying the maize crop.!! Another curious meteorological phenomenon of the Sierra is the prevalence of radiation fog in the low basins from late summer to early winter. Forming in the early morning hours (after 1 a. m.), the fog evap- orates by noon. Its presence lowers average daily temperatures and prevents rapid evapora- tion of surface moisture.” Annual precipitation in the area north and east of the Sierra averages from 750 to 850 mm. A greater amount is recorded around Lake Patz- cuaro (town of Patzcuaro, 1,109 mm.), and even more probably falls in the Sierra, where no records exist. The greatest precipitation in Tarasca is recorded along the southern (windward) side of the Sierra in the upper escarpment zone. (Aver- age annual totals for Uruapan, 1,683 mm.; Ario de Rosales, 1,225 mm.; Tacdimbaro, 1,240 mm.) ‘0 In northwestern Mexico, particularly in Sonora and the Sierra Madre Occidental, the winter cyclonic storms are called equipatas. Although they are part of the same frontal system, the eqguipatas occur more frequently than the cabaviuelas since northwestern Mexico is nearer the North Pacifie center of frontogenesis. '' Lumholtz (1902, vol. 2, p. 365) states that water has been known to freeze in Cherfn and Zacapu on June 10. The Sierra fogs are often mentioned by colonial chroniclers. One, describing the Charapan area in 1789: ‘ . . . continwalmente se ve el terreno cuebierto de neblas, que evaporen y eralala humedad de latierra’’ (AGN Historia, vol. 73, f. 219). Climatic areas and associated vegetation.— Sufficient statistical data are not available to construct accurately a map showing climatic types in the Tarascan area. Using (1) the avail- able statistics from the few existing stations, (2) vegetation boundaries taken from field observa- tions and aerial photographs, and (3) elevations from topographic maps compiled from aerial photography, an attempt has been made to locate climatic areas based on the Koéppen system (map 4). The Sierra.—The Cwb and Cwe climatic types of Képpen"™ correspond to the tierra fria of the Tarascans—the Sierra, its eastern extension (in- cluding the Sierra de Ozumatlan), and the south- eastern part of the northern plateau area. A mixed oak-pine forest forms the dominant vegeta- tion of the Sierra and its eastern extension, and corresponds to the higher and colder phase of the Cwhb climatic zone. (Cf. maps 4 and 5.) Pinus leiophylla (pino chino) and P. michoacana var. cornuta (pino lacio) are the principal pines (p‘ukiri) of the Sierra (Martinez, 1945). (Pl. 1.) The former species is the main turpentine pro- ducer, while the latter, a straight, tall tree, affords the best lumber. Minor species of pines found in the Sierra include P. teocote, P. pseudos- trobus, and in the upper escarpment zone, the subtropical pine P. oocarpa. Even at high altitudes the pines rarely form solid stands, but are mixed with numerous species of oak, the latter dominent at lower altitudes, the former at higher elevations. Some 30 species of oak (urikua, tuktis, Sariri), both deciduous and_ persistent, occur in the Sierra and adjacent areas. Among the more common are Quercus fulva, Q. acuminata, Q. circinata, Q. laxa, Q. crassipes, and Q. pandurata (Trelease, 1924). Often mixed with pine and oak are madrofio (pandnksa; Arbutus sp.); various laurels (Lauraceae); many hydrophytes in bar- ranca bottoms, such as jaboncillo (saépu), palo blanco (udrpit-uku; Alnus sp.), palo colorado (éaraépit-uku). On lower slopes one often sees the Mexican “crab apple” (actually a hawthorne) or tejocote (kaais; Crataegus mexicana) and the “cherry” or capulin (Séngua; Prunus capuli), both of which 13 Mathematical values of Képpen symbols: C, temperature of coldest month between —3° and 18° C.; w, dry winter, rainy summer; b, tempera- ture of warmest month less than 22° C.; c, temperature of coldest month above —38° C., and mean temperature of less than 4 months out of the year is more than 10° C. a Y OF THE MODERN TARASCAN AREA—WEST CULTURAL GEOGRAPH ‘uUpOBOyIW Jo deur onemiyo— fF avyy ft BiBWBTINgY Sos opupsiz | \ NVOVOHOIN 40 ANYONNOS HO33dS NVOSVHVL 03120W JO SLIWIT) LN3S3ud Be NOILVLS 1V9I90T0H03L3W os0n20:09? Ce20dajjoosowe, ojoaiang? (ys@) uobuizjodye Z 62286 ==-. < 9edajo>2\0da) ° / v i i 010) 090. u0}jOWO zee 16 S2)0S0y ap ouy ‘1 u We . (my) oasodnonindg Ne (my) 1 4S@ vosoranba, Opis ) ea ae sakay so79 oanbuobuy? - (om) ay EO 3 iets ubdorine Dee (qm) o10n 20412 [ebuy ves Sf = \ # o 7 : ; (qnq) o10noz100° er ; m9 S e (qm) OB0pIH OHA *, Surpuinbury (qm9o) . anes! Hier coe Pemare: Et e onypindjoj, eS Moyo? (qm9)ndoo07" oe - if . * (qm9) of1y097% q NM 9) (quo) osonredourz® et : s a | (quo) on oros0W® \ = Cs Os Be \ o1edaing? Sy ojwoz0w X a we eae z oazyng TF (om9) o10W07 © --2 (amo) 01/2108 0pH® oe 4 okonyos? (qm9) O10NI 91a ® DM DMO Ruojjownlon — (DM) O1saijoajos® = NN Jj VIVdVHI 30 O97 02409 079 & wy) (O0m9) popaig 07 = sail ecOl Of 8 INSTITUTE OF SOCIAL ANTHROPOLOGY are frequently semicultivated in hedgerows and in house lots. Agave (akimba; A. latissima, A. americana) is also a frequent hedge plant found particularly on the outskirts of settlements, and the tree yucca or izote (¢ambasa; Yucca australis), although more common at lower altitudes, is often seen In Sierra villages. Understory vegetation in the oak-pine zone is sparse, possibly owing to the annual burning of herbaceous plants in the forest to improve summer forage. Some of the more prominent understory plauts are zarzamora (¢ttn; Rubus sp.), a wild blackberry especially abundant along hedgerows, and wild grape vines (Vitis sp.). Various epiphytes, such as orchids of many species, are found on the trunks and branches of pine and oak throughout the Sierra. Although meteorological data are lacking, the climate of elevations above 10,000 feet is possibly Cwe, i. e., cold winters and cool summers (map 4). Such elevations occur on the upper slopes cf the higher volcanoes, where snow occasionally falls and where fir (Abies religvosa) forms the ,dominant vegetation. On slopes above 8,700 feet this tree (pinabete, t*ktimbu) starts to appear among pine and oak. At 10,000 feet solid stands of fir begin and continue to the mountain peaks, where high altitude pine (P. hartwegii) has gained a foothold in eracks and crevices in rocky cliffs. Understory vegetation in the fir forest coasists of various herbaceous plants, including a bunchgrass cailed zacate or j6éin (Muhlenbergia macroura). The green shoots of j6¢in afford the principal forage for sheep and goat herds which are grazed on the high slopes of Cerro de Patamban and (before the eruption of Paricutin) on Cerro de Tancitaro. The type of original vegetation in the basin plains within the Sierra is problematical. Prob- ably cleared and cultivated for more than 300 years, these plains now show little evidence of the original vegetation cover. The dark-colored soil of the plains suggests the former presence of a grass cover, possibly with scattered oaks and pines. The Lake district.-According to temperature figures, the shores of Lake Patzcuaro fall within the tierra fria climate (Cwb). Owing to higher winter temperatures than those experienced in the Sierra, and to absence of fog, the Lake district enjoys a warm phase of Cwh (possibly transitional between Cwb and Cwa). Oak and associated broadleaf trees, such as madrono, jaboncillo, ete., PUBLICATION NO. 7 form the dominant plant complex of a belt 3 km. wide around the lake. Moreover, colorfn (pforén¢a; Hrythrina americana), casahuate (Ipomoea murucoides), and zapote blanco (uriata; Casimiroa edulis), all characteristic of the warmer sections of the northern plateau, are common hedge plants in the Lake area. Along the lake shore, water-loving plants, including a willow (tatimu; Salix bonplandiana), shrubs of ““tepozin”’ (Buddleia sp.), and clumps of bamboolike carrizo (pfatamu; Arundo donar) are not uncommon; while in marshy sections canebrakes (tule or pa¢imu; Cyperus thrysiflorus) abound. Other aguatic plants include various waterlilies and hyacmths (Nymphaea sp.; ichhornia speciosa). Possibly a mixed pine-oak forest once covered the lower slopes bordering the lake, but, if so, the pines have long since been destroyed for firewood and lumber. Occasionally lone specimens of Pinus leiophylla are found on the outskirts of lake villages. The northern plateau.—The Cwbh climate ex- tends northward from the Sierra into the south- eastern part of the northern plateau area. In the middle and lower Rio Lerma Basin (Bajio) and in La Canada, however, the Cwa climate of the tierra templada occurs. In both Cwa and Cwhbh areas of the northern plateau, oak and pine forests occupy only the summits of the higher hills, below which exist stands of oak and madrofo. The lower slopes and plains carry an association of grass and shrub, the latter consisting of casahuate, zapote blanco, tejocote, palo blanco (Lysiloma candida), granjeno (Celtis pallida), jara amarillo (téksten; Senecio salignus), all typical of the more humid portions of the central plateau. Xerophy- tes, such as huisache (Acacia sp.), mesquite (Prosopis juliflora), and various cacti (mainly Opuntieae), are common. In the plains, fresnos (padimu; Fraxinus sp.) form gallery forests along streams, and in draws within the hills hydrophy- tes, such as wild ahuacate and other laurels, pre- dominate. Formerly extensive meadows existed at the edge of swamps and lakes, particularly in the lowlands east of Lake Chapala and the well- watered plains near the northern edge of the Sierra. In the northern plateau pine and oak forests were formerly more extensive than at present. Many of the hilltops north of the present México-Guadalajara highway, which are now barren cf arboreal vegetation, were once DW mw me 4 nw we a, O— »9foeneo 2 ° Capacuaro _. ; : : : Li) RFP a C Be ne fe ee LES o°0 ‘ @Toncitaro | : ‘ Ree FIR FOREST \ V////\ PINE-OAK FOREST (a large port cut over & cleared for cultivation) | “ 0° | OAK & SCRUB OAK FOREST = @ Z inthe TT > Ndi | Bota ; P30). : PRESET Cen Gh [Natit Rep AY cateCh) Jeb nacama Tanabe: dd! ab baqyy noltaysgaV—~.2 tAM © CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—-WEST 9 covered with pine and oak within the memory of living inhabitants. Increased cultivation of slopes and constant cutting for firewood and charcoal will soon destroy the greater part of the pine-oak remnants in the northern plateau. The escarpment zone.—South of the Sierra lies a series of climatic types arranged in altitudinal sequence. The upper part of the escarpment (5,600 to 3,600 ft.) is characterized by a narrow belt of Cwa (tierra templada) climate, which is followed abruptly by the subhumid tierra caliente (below 3,600 feet), or Aw. Below 2,000 feet with- in the Tepaleatepec and Balsas Basins, a semiarid tropical climate (BSh) prevails. The pine-oak association of the Sierra spills over onto the upper escarpment, but the sub- tropical Pinus oocarpus becomes the dominant pine. Between 4,600 and 3,600 feet, pines disap- pear, leaving an open oak forest mixed with sub- tropical and tropical plants of southern Mexico. At lower elevations the latter plants become dominant." SOILS Three soil types, which tend to coincide with climate and vegetation, predominate in the Taras- can area: (1) a yellowish-brown leached soil of the upper mountain slopes (Cwb to Cwe, pine-fir cover); (2) a dark, fine sandy loam (t‘uptiri) of the lower slopes and basins in the Sierra (Cwhb, oak- pine, probably grass vegetation); and (3) the reddish-brown clay soil (¢ar4nda) of the lower altitudes (warm phase of Cwb, Cwa, broadleaf vegetation) around Lake PAatzcuaro, in the lower elevations of the northern plateau, and in the escarpment zone (map 6). Transitional and special soil types also occur; for instance, many of the Sierra soils are termed “charandosas,”’ having a ; gees higher clay content than the t‘uptri loams. Yellowish-brown soil.—This soil develops in high altitudes under seasonally humid conditions “The tropical vegetation of the escarpment is characterized by a great variety of genera and species. The most common plants include the milky-sapped trees and shrubs of the family Moraceae—comuchin (Ficus padifolia), siranda (F. petiolaris), saruma (Ceropia mexicana); the pod-bearing Mimoaceae—timbin (Mimosa stipitata), guaje (Leucaena sp.), huisache (Acasia sp.), tepehuaje (Lysiloma sp.), parota (Enterolobium cyclocarpum), timuche (Pithecellobium lanceolatum), guamuchil (Pithecellobium dulce), Calliandra sp.; the pod-bearing Caesalpiniaceae—habilla (Cassia occidentalis), easacalote (Caesalpinia coriaria), etc.; the edible fruit-bearing plants of the Annonaceae—chirimoya (Annona cherimolia); of the Lauraceae—ahuacate (Persea americana); of the Sapotaceae—chicozapote (Achras sapota), mamey (Calocarpum mammosum); of the Anacardiaceae—circuela, cupu (Spondias mombin); of the Mirtaceae—guayaba (Psidiwm quayaba); and the copal- bearing Burseraceae—copal ( Elaphrium jorullense). and fir-pine vegetation. It is the soil of the higher hillside maize plots in the Sierra; leached and infertile, it will produce crops for no longer than 4 or 5 years, after which the field is abandoned. The fine, sandy topsoil, however, is moisture retentive, and is therefore known as “‘tierra de humedad,” in which crops can be p'anted 2 months before the rains. Podzolic soils (uncultivated) probably occur above 10,000 feet in the fir forest. T‘uptri.—The most productive of the highland “humedad” soils is t‘uptri. Like the yellowish- brown soil, the texture of the topsoil is extremely fine. (Analyzed as fine sandy loam: 56 percent fine sand, 23 percent silt, 21 percent clay, 1 per- cent coarse gravel.) The surface drys to a fine powder and acts as an insulator, preventing the evaporation of moisture from the soil beneath. Consequently, in April and May near the end of the dry season the t'uptri soil is well moist 3 inches below the surface. T’uptiri usually occurs between 6,500 and 8,600 feet on both the lower slopes and in the basin plains. Being porous, the soil soaks up moisture rapidly, preventing serious sheet or guily erosion even on the steeper slopes. Generally, the basin t‘uptiri is more fertile than the yellowish-brown, the topsoil of the former having a high humus content (6 percent), a fair content of critical elements (e. g. 0.09 percent N), but a deficiency of lime (0.31 percent). Various subtypes of t‘uptiri occur, differences being based mainly on soil texture. At the base of slopes or on alluvial fans the topsoil is often partially com- posed of coarse voleanic cinder. Such soil is locally called ‘‘cascajo,” or gravel. Other sub- types are characterized by an increase in clay con- tent. These eecur on the lower slopes, and are sometimes referred to as “tierra charandosa.”’ Caranda.—This is a reddish-brown clay soil, which prevails below 6,500 feet and develops trom the spheroidal weathering of volcanic rock under warm summer and mild winter temperatures and a cover of broadleaf plants. (Textural content: 39 perceat sand, 26 percent silt, 35 percent clay.) 15 Surface soil samples (to a depth of 25 em. below surface) were taken by the writer in the Sierra and Lake areas and were analyzed by the Comisién Nacional de Irrigaci6n, Direccién General de Agroeconémica, México, D. F. ‘Texturally the highland yellow-brown soils are sandy loams, (60 percent fine sand, 20 percent clay, 20 percent silt, are highly water-retentive (30 percent), and are low in hummus (4to 10 percent). All soils analyzed (including t‘uptri and ¢aranda types) were low in lime content (0.24 to 0.34 percent), and slightly alkaline to alkaline (pH values: yellow-brown mountain soils, 7.22 to 7.24; t‘upuri, 7.44 to 7.71; ¢aranda, 7.21 to 7.42; uirds, 8.05 to 8.13). Since profiles were not determined, classification according to world soil groups is not possible at this time. ca ‘ PUBLICATION NO. INSTITUTE OF SOCIAL ANTHROPOLOGY: *soj0U plPY WOlj ByVq ‘BvolB UBOSBIBT, ULOpOUL 9} UT sod Ay [TlogS—'9 dV] vi Oe) i E , O;oqwobuly Pas ay fof ° “a oyd0u0 i) oo ‘0. oboing “o> — lp d ———— is opuawasay Y/ Theat ffi fed. ee ghee syuin STI0S 3NI¥LSNOVI : a // voNvyy : Ld Ce / YUV) wiseese 7: osadaing® NMOUS~MOIT3A ws y) Lificf cf Vege papel, / LIU WyOdn.t OF e201 vA oud 7 f / 17 a / o if ° Lf & fad ix! / hie: Vay /.ovonoa1017/ ff ‘7 °20l CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—WEST Tel! Large cracks occur in the soil surface during the months of March and April, and moisture is evap- orated from a depth of many inches. Conse- quently éardnda is a ‘‘temporal”’ soil, i. e., it can be planted only after the rains begin. Because of its clayey texture, it erodes easily once the plant cover is stripped and the soil structure is destroyed. The cultivated slopes around Lake Pitzcuaro, for example, are one of the worst-eroded agricultural areas of Mexico. Wherever éar4nda soils occur, the surface is scarred by gullies, which are becom- ing a characteristic landscape feature in the low areas surrounding the Sierra. Minor soil types——Among the most fertile in the Tarascan area are a few minor soil types. These include the alluvium in La Cafada and the lacustrine deposits around the shores of Lake Patzcuaro and within the recently desiccated Zacapu Basin. Containing abundant organic material and essential chemical elements, most of these soils are cropped annually without fallow. A peculiar soil type, called wirds, occurs near the edge of a lava flow on the southwestern shore of Lake P&atzcuaro, on Jaracuaro Island, and near Thuatzio. The subsoil is a fibery-textured white clay (35.4 percent fine clay), from which the whitish-gray adobe bricks of Jaricuaro and Thuatzio are made; the topsoil, when mixed with lacustrine deposits (as on JarAacuaro Island), forms a fertile loam extremely high in organic matter (nearly 5 percent) and calcium carbonate (7.7 percent). On the other hand, when the parent material lies close to the surface (as around Arécutin), the wirds is one of the poorest soils in the vicinity.'® 16 A similar soil type occurs at the edge of a lava flow along the highway on the outskirts of Zacapu. The relation between vulcanism and the forma- tion of wirds is not clear. TARASCAN POPULATION THE RECESSION OF NATIVE SPEECH One of the outstanding developments in Ta- rascan history has been the drastic areal recession of indigenous speech. Today the territory in which Tarascan (P‘orépeéa) is spoken represents only one-fifteenth of its pre-Conquest extent. The pre-Spanish linguistic area (discussed by Brand, 1944) included most of the present State of Michoacan, except the Pacific slope of the Sierra Madre del Sur between Colima and the lower Balsas (map 7). The political limits of the Tarascan state, however, extended beyond the language boundary: in the west into Jalisco, in the south to the Pacific, and in the north to the Bajfo of Guanajuato (Brand, 1944; cf. Stanislawski, 1947 a). The Tarascan cultural core centered in the north-central part of the Empire, comprising the Lake P&tzcuaro-Cuitzeo area and the pine forests of the Sierra and the upper escarpment zone (Stanislawski, 1947 a). Tarascans extended their speech southward into the tierra caliente (basins of the Tepalcatepec and Balsas) by colo- nization from the highlands during the 14th and early 15th centuries. Likewise, the P‘orépeta settlements around the eastern end of Lake Chapala and south thereof (Mazamitla) appear to have been 15th-century colonies. Within the pre-Conquest area various islands of foreign tongues existed; these represented colonies settled with permission of Tarascan chiefs. There were three inclusions of Matlaltzinca or Pirinda (Otomf stock): (1) the largest, near present Morelia, from Undameo northeast to Charo, (2) at Taimeo, southeast of Lake Cuitzeo, and (3) at Huetamo near the Balsas.” Moreover, a group of Apaneca colonists lived at Guayameo, near Sirandaro on the Balsas, and an islet of Teco occurred between Tancitaro and Uruapan."® Various factors contributed to the areal retro- gression of Tarascans during the Spanish colonial and postcolonial periods. One factor was actual decrease of Indian population caused mainly by European diseases. The population of some areas was further weakened or depleted by migration of Tarascans as laborers to distant mining and agricultural centers. Moreover, Spanish and mulatto settlement within the indig- enous area was a powerful force of hispaniciza- tion; wherever stock-raising estancias or sugar haciendas were established, native speech slowly disappeared. Conversely, in those areas shunned by Spanish settlers, Tarascan has been preserved to this day. The most serious shock which the indigenous cultures suffered from Spanish contact was the frightful toll taken by the contagious European diseases that became epidemic throughout centro’ 1 Data obtained from the following Relaciones Geograficas in Mus leg. 102: Rel. de Necotlin and Rel. de Cuseo; Mus. Nac., leg. 99 Charo Matlalzingo. 18 Mus. Nac., leg. 102, Rel. de Sirandaro y Guayameo; P’ 1872, vol. 1, p. 131; Mus. Nac., Col.de Gomez Orozco, vol. 1, ” 102° INSTITUTE OF SOCIAL ANTHROPOLOGY-—PUBLICATION —— mm = Limits of Torascan Speech, ca.1550 (Brand) Guadalajara ch Inclusions of Foreign Speech, ca 1550 T7 > Area of Tarascan Speech, 1946 ——--— Boundory of Michoacén As aio te X aa = IN cree ge the ay » LAGO DE CHAPALA “ . ‘ ? ‘ 0 iD pene Soe ce a Sa es ‘ f oe ena Puruandiro y a } o Sahuayo =— Os Pe 2o---— ip oC i] ozamora “So Sy Se ( Zp aarti = = —_— es ~~ oe fe} t | Mazamitia? 5) Sy MaravatieN 0 TSN oe Re ) mention scores of villages in the Taras- ‘hich are now nonexistent, the inhabi- » this calculation from figures given in the Suma de Troneoso, 1905, vol. 1). boundaries of Tarasea speech. tants having been wiped out entirely, or the few survivors having migrated later to larger towns. Spanish exploitation and settlement in Mich- oacdn slowly effected the reduction of Tarascan speech. Guzman’s entrada (1530) left a trail of destruction and displacement of population throughout northern Michoacén. Moreover, dur- ing the exploitation of placer gold along the tributaries of the Balsas and Tepaleatepee (1524— 35) Spanish miners destroyed and dislocated many Tarascans through enslavement and overwork.” On the other hand, Franciscan and Augustinian missionaries, who by the end of the 16th century had established themselves in most of the large Tarascan pueblos, were strong agents of accul- turation, replacing many indigenous material and 2 The Indice de Protocolos, vol. 1 (ed. Millares Carlo and Mantecon), gives abundant evidence of the feverish gold panning operations in the Balsas and Tepaleatepee drainage from 1524 to 1528 and cites the wholesale use of Indian slave labor. Such activity probably continued until the enforce- ment (in the 1540’s) of the New Laws, which forbade slave labor and conse- quently deereased the profitableness of gold washing. Furthermore, many Spanish adventurers turned from gold panning to silver mining after the discoveries in the Tasco district during the 1530's. LAGO DE CHAPALA -— | ee The mill settlements (trapiches, ingenios), like the cattle ranches, were centers of acculturation and misce- genation. Large groups of Negro and mulatto slaves, male and female, were imported to operate the trapiches (according to colonial law, Indians were exempt from mill labor), while Tarascan forced and free workers planted and harvested cane in fields nearby. Race mixing and gradual loss of native speech was inevitable. Again, ex- ploitation of the copper mines of the trerra caliente and the establishment of smelting centers in Tzatzio and Santa Clara was another activity which helped acculturation and hastened the loss of the aboriginal language. In 1750 the limits of Tarascan speech still coincided with the 16th century pre-Spanish boundaries, but in some areas, such as the Tepalcatepec Basin, the per- centage of inhabitants speaking Tarascan was only 25 percent of the total. In the tierra tem- plada sugar-growing districts south of Zit&écuaro, in the Peribién Valley, and the upper escarpment zone around Ario and Tacdmbaro, the ratio of 25 In 1540 a sugar mill had been established in Taximaroa, on the plateau above Tuxpan (Paso y Troncoso, 1905, vol. 1, p. 253). LAGO DE CHAPALA Pajacuar( e lo \ Mozomitla i \ Tomatién eTepaicatepec \ ees Probable limit of Tarascan speech, 1800 Areas with 100 % Tarascan speech, Ups 1800 Percentage of indigenous speech in towns 100% S99 75% 74-50% 49-25% 24-0% Map 9.—Area of Tarascan Sty ee O Yurécucro™s ° t. uO: XN XN to. R10 g z 5 ) 59 N i ( ° = eee LAGO DE CHAPALA “= ¢ Cojumotidn ° ‘everécuaro = ~ ca a © Sbenjomillo 25% © Purvéndiro ~ ie e e Sohvoyo @ 7 ~ 1 ey J / { : ee = OKcémbaro / e¢4 ~ Huango s © —)o-20 \o 7, x ~ se Cuitzed XN F ores ) ‘ ‘\ Huoniqueo co) Sea») Nie e en CRapendare ZgsedeuarsN . . * 2a 50% Torecuato to) LSE: = 75% 2 N 5 Potamban » Vo \ Me by e © Teremendo “le \ ©. = Tinguindin oldiimoroa ‘OGocupao Tzintzuntzan a @Eticuara S Tancitoro Tacambaro = ° e e Tomatién \ fo} @ Tepolcotepec \ Lo Huacono ° eee Probable limit of Tarascon speech, 1800 Cutziog / / Va Areos with 100 % Torascan speech, Huetama O pf 1800 sa eo ‘ ~ Percentage of indigenous speech in towns 100% 99-75% 74-50% 49-25% 24-00% oooe @ en locality 748988 O - 48 (Face p. 14) : < F iv! ‘ to total number of inhabitants at any 8! Mar 9.—Area of Tarascan speech, ca. 1800. Isopleths indicate percentage of Tarascan-speaking i Me i ae eee : ie ' .< ep i THUICATION Hos & f * hee Siieieli ¥ hos Ts fascune, F = 2 Pure oh Che western @ ii M catern Lorca R te . ays A ; ap ornrepale iia Sire x as ud its Europesnbcubess * pheay hear! whe ete -- mS [acu ny iene Apatauird the Tepulegtoneg so gma x th, ete aun aged ebriubs! 3 eve less ai it thd north ore niatean, ; ape bs bY abundink 2 ngs .. Sr the norili sie native \ Pere rd ar at nt With the mika ew Y > +" SSS \Viee a a cs aoe \ ‘ = = aie i \ a eel “WW the daythtte.” Moreovery difriie: ot an | pion aw 7 ile i uh contury Syaniantiatie gtinambang \ ‘ i : "4 Lar 33 as bee ans and emit sith ' dea a * oe > — oe fy seh hk 8 ti Libs? va caliente * Th = Ve ot SF : ; trapichal tngeniis), tise tie F ihe; ee ous Aegis of aceulturation privonst, +ef_ ee & 5 ey otwert rnupe ot Negre ASC ; q ie ; Prstighnd foranin, were Mipirtedte oe } i Sy. ao jencording to oolonial law . i ki a ? Aan a8 a fruit maiebor), while, 4 d {eee an do oiree workers phusited ‘and h ‘ube esto ¥ Ps — ' r. + Pinal i sals nearby. ee maine and ae watt H ae: Shce a gresae eecoves ae thm aide } 1 20 COPPET POLS hl et ily cap fray . fea Soois Uinee oN anor Peare" a! a Sah oe eats ids tte wired lanai, o 17 28 eearh ete es i ecidod with sre DAashs Daviniariea, Dui ai fH ns tue ilar CR TERE « ew, a ita: as Taraet ah r ocmaw ara ee : . ; 7 Hats v aley, aud they ‘ ut) ao Hiet ponies temsaha'E te nseqoeag wl il eiicioal 0081 29 viasoga peoganaT i048 >, Tht ~ OF (Puce p. 06) arti) 2] ) iI NO O1DN 0104 Se oe Suonp vos osoqwo20)? Gs a= —_---- oadodg 7 P , 3 F ; 4 al J peta a - } manch) wratahine 1] J iis) r) \° i ] ' RRA’ WOE ae ab | 1, 7B savin leg BS gute rs a ee ' 1 Mis 4 i | ee _ =e Prt ie & = fony %. —-aueae| ° ® weauetinzod t bauenit ane j oy 2 oopn0f % (apre f d ning y 1 oe aw * a) i F o is t A. iat i Ae ” °" wa rin RO rs ong gy r @ au . &) we ones: a ie ad i } 26; | ~ ovum gy 7 & ~@- yoo rs — re bit Pia —\ an cy s 3" in ae e > “\n macy « Pace” ot Wl ele ak OC ota : Y 4 | : | ' 7 ee ; @ onivez noIEVsPOoA ? WF anal ane - YY = | 3 oe o ¢ f ype x the A eo 4 ven _ 4 | = puroyoren AG | becca — =< & pag. ; ; a a) v ef cate oreuotgad om Ka sere g & Lom ‘ om 4 : Ff ~\ % “<4 Gilt ce, (Ge) f Ganetos hoc » ‘ i ore * a) ginedtin9 oh I Mf eTdatieanm coos 0208 005,0f ‘& ooce i cf Vacdmbore t i ar Ze Aue 152 bafolustos eslova to jipoAl He qabeos O = $2 Foon we ts), ‘; 7 OLGI xivRo dotbecaib« | \ Mem atcoaritleyar Wassge: neMHET to notinditad—t aa Nox ca) a sswoli noitplugeg to vigor ‘prnvpé mor sizyfo. to: adivica Aguld yo dsloribai yitosel dope al etnntidodnt pra fe insane : = it nn cmd aaisliconl oxi minal CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—-WEST TABLE 1.—Distribution of Tarascan-speaking folk by localities, 1940—Continued THE SIERRA—Continued 19 TABLE 1.—Distribution of Tarascan-speaking folk by localities, 1940—Continued THE SIERRA—Continued Total Tarascan-speaking Total ‘Tarascan-speaking popula- folk popula- folk Locality tion Locality tion (num- (num- ber) Number | Percent ber) Number | Percent Municipio of Paracho: Municipio of Tangancicuaro—Continued Paracho lv) wet eee es 3, 304 1,005 30.4 Ubas anes (t)e- 5 Ss eas ne ee 51 | 20 39. 2 IMHIran(p) eeeeseee eae oe ee ee 593 593 100.0 Gusrachanillo: (1) =.= = -=---- 2-2. 52-cencc- | 22 9 40.9 Aranza (p) 792 126 17.1 Rancho Nuevo (r) 38 3 | 8.0 Arato (p) 233 0 0 [as Trojes\(r) --- 2125222 sete ces | 14 0 0 Cocucho (p) ------___- - 584 584 100.0 HOT Men uecCho(t) 2-222 2.c- esa nee 1, 735 1, 682 97.0 Ibarra (Patzcuaro Sta.)_.....__--------- 809 12 1.5 Huiramangaro (p) 540 17 3.1 emecorio: (p) Lao eee soos seen =enoee 499 0 0 San Juan Tumbio (p).- 887 0 0 Tzentzenguaro (p) 258 0 0 Ajuno (p) 540 0 0 Lazaro Cardenas (p) 412 0 0 Ajuno Sta. (rr) 719 0 0 Primo Tapia (p) 369 0 0 Municipio of Tancitaro: San Pedro Pareo (p)_-..-...------------- 384 0 0 Tancitaro (v) 1, 858 6 3 Carifin (r)__------- 37 37 100.0 "AON (D) Has=4==-5 876 0 0 Tecuena (r)___.___- 7. 73 100.0 Municipio of Tangamandapio: Urandén Morales (r) _ 2 39 39 100.0 Tangamandapio (p)-_--_.---..---------- 2, 573 12 25 Urandén Morelos (r) -_----------------- 164 164 100. 0 ‘Tarecuato (p) 2, 146 2, 146 100.0 San) Pedrito (r)2-= sees enansconsee 14 14 100.0 La Cantera (r) 962 962 100.0 RV rni6mn (r) =: oe ee ee eee ses 116 116 100.0 Las Encinillas (r) 78 78 100.0 Watretzio (1h) = sos see ces ee eee 170 14 8.2 Los Laureles (r) ____ 8 8 100.0 Municipio of Quiroga: Ucuarés (r) 308 0 0 Quiroga: (y) sees eee wee see sane 3, 009 4 1 Municipio of Tangancicuaro: San Andrés (p)_- 1,179 1, 165 98.8 Ocumicho (p) 1,040 1,018 97.8 San Jeronimo (p)_- 1, 527 1, 513 99. 1 Patamban (p) 2, 333 809 34.6 Santa Fé de la Laguna (p) 2, 036 2, 036 100.0 San José de Gracia (p)-- 170 147 86.4 A tzimbor(r) see on en ee neeeeeaceas 179 0 0 Agua Escondida (r)___ By 32 100.0 Chuptouseour)c-3 see = on. 22s ---e 31 0 0 Aranza (r) 54 21 39. 0 Touscato(h)es- 22222 - ose — oases 249 0 0 Gam écmaro;(f)eeeee P= _ = Sees 8 a2at-3 37 2 5.4 La Tirfmicua (r)___----_------- 88 0 0 Tzirandagatzio (r)--- 24 0 0 2 Locality not listed in 1940 census. Names obtained from local inhabi- tants. 3 Estimated population. 4 Entirely mestizo according to census, but 100 percent Tarascan accord- ing to officials in San Juan Nuevo (Los Conejos) in 1946. 5 Uninhabited in 1940, but estimated population in 1946 around 35, all Tarascan. 6 Inhabited 1944. Official census figures not available. 7In 1946, according to local inhabitants, Napizaro was only 50 percent ‘Tarascan. 8 Owing to loss of original census data, the number of Tarascans in PAtz- cuaro could not be calculated. The percentage would probably be extremely low. 20 TABLE 1.—Distribution of Tarascan-speaking folk by localities, 1940—Continued THE LAKE AREA—Continued INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7 TaBLE 1.—Distribution of Tarascan-speaking folk by localities, 1940—Continued LA CANADA—Continned Total ‘Tarascan-speaking Total ‘Tarascan-speaking : popula- folk A popula- folk Locality tonic __ Locality tion (num- (num- ber) Number | Percent ber) Number | Percent a - ~ | Municipio of Tzintzuntzan: Municipio of Chilchota—Continued zintzuntzeni(¢C)= 22s... 22.2----2--22-2- 1,077 | 35 (9 156) |3. 2(9 12. 7) IheiCofradia(r)i i. .s2 69 0 0 Cucuchucho (p)____--_-_-----_-________- 295 279 94.5 ADzintzichs ((t)t = esnon eas See eee oe 117 48 41.0 Thuatzio (p) 1, 206 1, 206 100.0 Municipio of Tangancfcuaro: La Pacanda (p).---......2-..----.-.---- 247 240 97.1 Tangancicuaro (v)_- 10 2 Woenembo! (rings ao2 2s t= tc 451 0 1) IPH CuarOn (pies. sass a cee ee seed 9 1.0 Whos @orralesi(r)c 82.2 oe = 177 0 0 as Cuevas (r)<. 2 = -222- 2.5 =a... e- 69 0 0 > = Las Granadas (r)_______.__-_-___ 92 92 100.0 CHUIDION(G) see Seen se eee 162 162 100.0 = aces: a ae aa eerie (W) - ----------- 2222 2----- ee ue ee) Municipio of Ziricuaritiro: i made a Restwirr Log > ocak yi hs o a San Angel Zurumueapio (p) - 970 822 84.7 - 30 ES) Aes n08 100.0 Municipio of Tingambato: eee n0/(a} a 0 o Tingambato (p)...----.-------------- 2, 768 204 7.3 as Pilas (r)-.-------------------------- 87 0 9 Municipio of Uruapan: Santa: @ruz:.(r) 2-2 2225-22 ences 178 0 0 Upiapanl(c) ae eee ee 20, 583 1 AE Tarerio (r) 201 194 96,5 mcutacatol(pe. lee 509 5 1.0 El Teeolote (t)..----------------------- 12 0 0 La Rosa de Castilla (r)_.-_-_.....-...-- 60 2 3:3 Hl Tigre (1) ----. -----~-=---2-2--0----= we W) M Toreo Alto (r)_.._...------------------- 240 3 1.2 Wensansstacue:(r)..°-.22--2-22 2 222.- 110 110 100. 0 Galtzontein (p)i tee cho ’ (2) ro) (2) La ae (1) ----------2---2--------- tk | 0 W Municipio of Ario de Rosales: La Vinata (r)-.-------..------..-------- a a 1020 Villa Silva (p)1_.... 2.22... 2. see l@) Orde XO i THE NORTHERN PLATEAU REGION = 10 Inhabited 1943. Official census figures not available. Munieipio of Coeneo: ° . ° b See ee the rt an F A Distribution of monolingual Tarascans.—In AcaiOi(p)sameene es ae Ae 1,097 | 1,088 9.2 spite of continued areal recession of native speech Comanja (p) 806 91 11.3 : sey =e = Bare econ 2 WMG a hens og ond infiltration of mestizos, monolingualism still Bellas Fuentes (h) 876 1 1 exists in many parts of Tarasca. According to HUATOC Ot) een ates Soe keane tee eee 345 | 1 3 paris 2 = (OY. a , Fe Nee te er ; ‘ calculations from 1940 census data, approxi auLeuibirol(t) os eeee fe seeds aaah ee 749 2 2 mately 38 percent of the Tarascan population is Municipio of Zacapu: : é 3 o are ie Se ois a 4 monolingual. Personal field experience, however, Cantabria (p)_---_-----.-----.--------- 1, 132 0 0 would indicate that a smaller proportion (prob- INBYanjai(D) coe oon soo hese ee ses ee 1, 082 763 70.5 2 9 ae by Mareiets (ah se aa a ably 20 percent) speak only Tarascan. The mono Guirindero}(p)smere eee ee 1, 252 686 48 linguals are composed principally of conservative Buenavista (h) ...--.-...------- 224 7 3.1 F ae 5 . ivine in Caches G isi : 13 women and girls and the older men living in the San Antonio (rn)... 909 0 0 more isolated pueblos and ranchos. Pronounced Se nee ce taie ‘ o7 monolingual centers are scattered through the Teremendo (p)...---------------------- 1,331 379 28.4 Tarasean area and correspond to the islets of TIRES VES) ieee caer 178 : oe purely indigenous speech mentioned above (map = 13). One center includes the ranchos around the LA CANADA eae =e = we Cerro de Patamban and also the majority of Municipio of Chilchota: women in the pueblos of Pamatdcuaro, Sicuicho, CE TOE NG) Zale y ‘4 and Sirfo, nearby. (According to data from the Acachuén (p) 717 712 99.3 9 5 ee Garapanl(p)= =e ee ee ee 1,259} 1,240 98. 5 1940 census, approximately 67 percent of the Pee aa COS eine te Tarascan population of this area is monolingual. eban:(p)cesss-5--2s. 22222 776 776 i ‘ 5 a Santo Tomés (p) 295 292 99.0 Following percentages in this paragraph are MACUCO (Dp) se 22. = ce oe 445 445 100.0 ealeulated from the 1940 census.) Another center Tanaquillo (p)_ 410 184 44.9 ri : ah f ORE E Coe ee ee ea Saree 350 135 36 Includes Tarecuato and the adjacent rancho o Zocopo (Pp) ---------2--2----- eee 539 539 100.0 Still ®’ Number and percentage of Tarascans in Tzintzuntzan, 1945, according to ethnographical census. 1,231 inhabitants in Tzintzuntzan. The percentage was calculated on the basis of La Cantera (66 percent monolingual). another area is situated southwest of Nahuatzen, and consists of the pueblos of Quinceo, Turicuaro, 21 WEST EOGRAPHY OF THE MODERN TARASCAN AREA LTURAL G CU Suryvods-uvosviey, JO JoquUINU [B1O} 0} Spensurpouour jo aFBiWs0Ied yuasardar syyotdosT FOI “eYBp SNSUID OFGI [RIOYJO UO poseg “Bale 9Y} UL S}UBIIGBYUT ofouong, 0s0NIZ10d0 fo} opuawasay oauacg ssa| 10 %G %Ol-b2 %S2-60b %OG- bl 49A0 pud ZG ° 12) 8 o e uanyouiz” osalai0l Gg ee or ‘OFGI ‘Bole UBOSBIB], JT} UL STeEnSurtjouour Jo uoTNqLUslq—'eT IVI 2z0l uodonin?s jabuy uos? ojyoquwobury 2 079407 US, (4 o4ond0d09, es oasuino mM uanysown9 Orr, [ Se” 2 ° Os0;DYIIg Podnioy 9° uodosoy9 o20u0, 0 QDIUOION fe) ndooo0z ° ° osondjuobuo) ovadaung? ,O€ ec0! O¥VLIONVI 30 9 v Surquag 0480117 fo) sakay $o7 oyaINIIS Y Th: orongoiowog A 0 Je fo} uipuinbury \ \ \ uoquinjog Sjuawa|jjas ul jo saquinu Sjudjiqoyu! Bbuiyoads-uodsosoy {040} Of SjonBuljouow jo abojuadsag 22 Inhabitants 200,000 9 299 o90 \ (Mendizabal) \ \ \ \ \ \ \ \ INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7 100,000 \ | | | | \ 22,000 (Mendizabal) | | ~~ | i; 80,000 ar F SS SS i | ~ in | Offical census ~ dota ec,ece LE if T AN, | 55,000" 4,795 (Villasefior & church records) 40,000 20,000 (e) Year 1500 1550 1600 1650 1700 1750 1800 1850 1900 1950 Ficure 1.—Decline of Tarascan population, 1500-1940. The figures for 1500 and 1550 include all aboriginal inhabitants in the diocese of Michoacan. Besides the Tarascans, several thousand Otom{ and some Huastec inhabited the eastern and northeastern sections of the diocese (Guanajuato and San Luis Potosi), and many people of Nahuatl speech lived in the western portion (Colima, southwest Michoacan). and Cumachuén (62 percent monolingual). More- over, the pueblos of La Cafiada, adjacent to mod- ern transportation facilities, are surprisingly mono- lingual (59 percent). Other scattered, ultracon- servative towns, such as Angahuan, Cocucho, and Cherandtzicurin in the Sierra, contain a large number of monolinguals. Effects of Paricutin Voleano.—The eruption of Paricutin Volcano early in 1943 caused the redis- tribution of some of the Tarascan population. The inhabitants of the completely destroyed towns of Paricutin and Parangaricutiro were transferred to new lands near Uruapan. Those of Paricutin were moved to the new settlement of Caltzontzin, 5 km. east of Uruapan, in February 1943. This pueblo now forms a new island of Tarascan speech in the tierra templada. With Government aid the people of Parangaricutiro established a new pueblo near the rancho of Los Conejos, 6 km. west of Uruapan, in March 1944. Another new town, CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—-WEST De Inhabitants 50,000 40,000 30,000 20,000 10,000 Year 1750 1800 1g50 1900 1950 Figure 2.—Growth of population in the Sierra, 1750-1940. The population of the following towns and ranchos was used to calculate totals for the years indicated: Ahuiran, Angahuan, Arantepacua, Aranza, Atapan, La Cantera, Cherdn, Cherandsticurin, Cherato, Cocucho, Corupo, Cumachuén, Charapan, Capacuaro, Huiramangaro, Nahuatzen, Nurfo, Ocumicho, Pamatdcuaro, Paracho, Parangaricutiro, Paricutin, Patamban, Pichdtaro, Pomacuardn, Quinseo, San Felipe, San José, San Lorenzo, Sevina, Sicuicho, Sirfo, Tanaco, Tarecuato, Tenguecho, Turfcuaro, Urapicho, Zacan, Zirosto, San Benito, San Luis, La Tinaja, El Tropezén, Uringuitiro, Zarzamora. Data for 1750 were taken from Villasenor and church records (AAM); for 1800, from church records (AAM); for 1845, from AAM, leg. 707, Memorias estadisticas; for 1900, 1921, 1930, 1940, from official census. called Colonia Dr. Miguel Silva (Villa Silva), was founded by volcano refugees in August 1943, 5 km. southwest of Ario de Rosales, on the upper margins of the tierra caliente. The settlement sheltered families mainly from Zirosto and some from Paricutin, Parangaricutiro, and Zacan.* The highland Tarascans have encountered several difficulties in the subtropical habitat: increased susceptibility to disease, unfamiliarity with sub- tropical clay soils, slow adaptation to new crop types. Consequently, within the last year (1945- 46) the population of Villa Silva has decreased from approximately 600 to 300, owing to high death rate and movement of families back to the highlands; the new settlement may be abandoned within a short time. Besides resettlement in newly formed pueblos, many of the families from the stricken area have moved permanently to less damaged towns, such as Pamatdécuaro, Charapan, Paracho, Uruapan, and Zamora. 80 The continued activity of the voleano may force the complete abandon- ment of the partially ruined towns of Zacan and Zirosto. In the spring of 1946 the authorities of Zirosto were seriously considering the removal of the remnants of their townspeople to the rancho of Barranca Seca, 4 km. to the northwest. = Possible future trends in Tarascan popula- tion.— Judging from the long-range trend in both areal recession and actual numerical decrease in Tarascan-speaking folk, it would appear that the Tarascan language is headed toward extinction. Figure 1 indicates the terrific human toll taken by the European epidemics during the first 50 years of Spanish occupation, and the leveling off of the downward curve * until after 1920, when increases are reported by the 1930 and 1940 censuses. In the period 1930-40 the rate of increase in Tarascan population equaled that of the mestizo element. This period of increase is too short to conclude 31 At the end of the 18th century, decrease in Tarascan population was still outstanding enough to be reported officially to the central government in Mexico City. Commenting on the population increase in the diocese of Michoac&n from 1700 to 1783, an official reports: ‘‘Hay el considerable aumento de 38,449 vecinos . . . pero debe advertirse que este segun las noticias comunicadas por los subdelegados, é informes recevidos en el asunto, es de espanoles, mulatos, y demas castas, pues en la de los Indios se experimenta mucha decadencia o diminucién originada en unos pueblos de la mescla de estos con distintas cali- dades; en otros de las graves y continuas enfermedades, que han padecido; en otras de las pensiones, que cargan insorportables a su felicidad, quando es corto el numero de los obligados a ellos; y en otros finalmente a la exrcasez de tierras para su precisa subsistencia, sobre lo qual para no confundir el estado antecedente se acomparia uno, que manifiesta los Pueblos, a quienes faltan aun de 600 varas, que por cada viento les asigna la ley .. .”. (AGN Historia, vol. 72, exped. 1 (1793)). 24 INSTITUTE OF SOCIAL ANTHROPOLOGY—-PUBLICATION NO. 7 that a new upward trend has been established. On the other hand, there has been a considerable increase in the population of the Sierra and Lake towns since 1750, which probably accounts for the level curve during the 19th century, in spite of drastic areal recession in speech during that period (fig. 2). Today areal recession is still in progress, but actual numbers of Tarascans appear to be increasing. The question is: Can the growth in number of Tarascan-speaking children continue to exceed or equal that of the children (of Tarascan speaking parents) who fail to learn the language or cease to use it in later life? Assuming equal rates of infant mortality and similar health facilities for both groups, it would appear that, owing to cul- tural changes now in progress within the Tarascan area, the indigenous speech will eventually dis- appear. Such cultural changes—improved trans- portation, more frequent contact with modern life, increased educational facilities both within the pueblos and in the large towns outside, the Government alphabetization program—all aid to increase the use of Spanish and to decrease the use of Tarascan. Such factors influence espe- cially the younger generation. Today the young people (5 to 20 years old) of many pueblos have not learned Tarascan, and often those who know the language speak Spanish by preference. More- over, as indicated above, mestizo merchants are still moving into the Tarascan market towns and in such centers intermarriage of Indian and mestizo continues; the offspring of such unions rarely learn the indigenous tongue. TARASCAN SETTLEMENTS The early Spanish adventurers and friars found Tarascans living (like many sedentary Indians of the New World) in agglomerated settlements, the larger of which the Spaniards called pueblos, the smaller, rancherias or estancias. The pueblo and the rancheria (rancho) have remained the basic units of settlement in the Tarascan area, as im most parts of Mexico. In size present Tarascan pueblos range from 200 to 3,400 inhabitants; the ranchos, from 9 to 900. Invariably the modern indigenous ranchos are offspring settlements from a pueblo nearby. For instance, the 11 ranchos on the southern and eastern slopes of Cerro de Patamban were formed by families, which for political or economic (land) reasons, left the mother pueblo, Pamatdcuaro. Sirfo, a former rancho of Pamatdécuaro, was made a pueblo and tenencia ca. 1926, its name being changed to Jestis Diaz. By such a process agglomerated settlements begin and develop. Moreover, the ranchos on the Tarf-uk‘éri Peninsula, Lake P&tz- cuaro, were founded 50 or 60 years ago by fisher- 32 Although in general these two types of settlement are differentiated by size, the terms ‘‘pueblo” and ‘‘rancho”’ have acquired political connotations, From the point of view of State and Federal Governments the basic political unit in Mexico is the municipio, which may contain many pueblos and ranchos. Usually the largest pueblo within this political unit is named the cabecera, or chief administrative town. The affairs of the cabecera and those of the municipio as a whole are administered by a presidente or mayor. The remaining pueblos in the municipio are regarded as tenencias, each headed by a jefe. The ranchos are dependencies of certain pueblos, local authority being vested in the diputado de orden. Upon obtaining sufficient size, prestige, or political influence, a pueblo may be elevated to the rank of villa or even ciudad Because of historical prestige small (1,077 mestizo inhabitants) Tzintzuntzan holds the title of ciudad. Such rank, however, in no way changes the political function of the town. men from adjacent islands of Janitzio and Lo Pacanda. On the other hand, the mestizo ranchos now found in the Sierra are the product of migration of farmers and political refugees from the outside. One of these, Arato, was established soon after the struggle for independence in 1810, and in the 1930’s was given the title of pueblo with tenencia status. Other types of settlement in modern Tarasca include the lumber camp (aserradero), an ephem- eral agglomeration of workmen’s huts around the sawmill. Such settlements disappear after sur- rounding exploitable timber has been depleted. In 1946 there were but three lumber camps in the entire Sierra. In addition, a minor form of dispersed settlement is sometimes found in the Sierra; occasionally a woodcutter and his family live permanently in an isolated house on a forested mountain slope and visit the nearest pueblo only to market products, buy supplies, and attend fiestas. Settlement sites——The few available early descriptions of the Tarascan area indicate the existence of many more Indian settlements during the 16th century than at present.*? This was particularly true in the Sierra, where small agelomerations (estancias or rancherias) were numerous. Such settlements were scattered on 33 The early sources which mention former settlements in the Tarascan area include the available Relaciones Geograficas, 1579-81 (Mus. Nac., leg. 102); various late 16th-century documents concerning labor and associated problems in Zavala and Castello (1939-46); many documents concerning the congregations of 1595-1605 found in AGN Congregaciones and Tierras. CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—WEST wooded mountain slopes (where maize could be easily cultivated with the digging stick) and on elevations difficult of access (chiefly for protection from Chichimec raids). Many of these estancias were likely wiped out by the early epidemics; others the Spaniards probably congregated with larger towns during the last half of the 16th and first years of the 17th centuries (Simpson, 1934; Spain—Law, Statutes, etc., 1681, ley VI, tit. 3), in order to better instruct natives in Christianity and to facilitate the collection of tribute and forced labor. Probably few present Tarascan pueblos possess their pre-Spanish sites. Modern Tarascan settlements occupy a variety of sites, most of which have level, or nearly level, surfaces. Those along Lake P&tzcuaro are on eminences or shelves above the water’s edge; all avoid frequently flooded delta plains. In the Sierra many towns are located on slopes or benches immediately bordering the large basin plains; others occupy level spots in local swales. NS> Tirosto Brarangaricutiro, 2 s Tancitoro : ef ° fon Apotzingdn 102°30' Map 18.—Distribution of house types in the Tarascan area, 1789 and 1946. 748988—48——3 Se pchiTehets eon =eane o o? Te iJ 7 v, . J wt we . J a a ve Cheran Ss Tr Copocuaro Uruapon? } : / f ? } ae \ i jo ys ‘ @ Wooden plank walls predominant © Adobe & stone walls predominant © Wooden plank & adobe or stone walls equally predominant # Wattle-daub walls predominant — Shake roof, 4-, 3-, or 2-shed | Tile roof, usually 2-shed --Approximate limit of wooden plank house Tarejero Coeneo roy io Comonjo TT Zipiojo VALLADOLID LO; Kec & cps ncunse ‘Or zintzuntzon (eis poe ; 7 ROOM ara yu BF Cuonojo Lo} Zirohuen oy Opopeo Sonto CloroO O Tocombaro @ Wooden plank walls © Adobe and stone walls © Wooden plank & adobe walls equally pre- dominant 1] Walls of vertical planks or sticks 4 Stone walls predominant — Shake roof Tile roof thatch roof The 1789 data are from AGN Historia, vol. 73, Calderén report. 32 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7 within or near pine forests. By 1789 most of the buildings in Tarascan towns in the Lake and Sierra regions were roofed with shakes (map 18). Today in the towns bordering the Sierra the red Castilian tile has completely replaced tejamanil and is slowly penetrating into the Sierra towns.* THE LAND SYSTEM AND THE PUEBLO Tarascan settlements are fundamentally agri- cultural villages. They include not only dwellings arranged along streets and in house lots, but also the surrounding farm land. The land is the body of the pueblo, whose political and economic life revolves around land ownership and boundaries, crop planting and harvesting. Few records exist on the ancient Tarascan land system; most lands, however, were probably held in common. Each community owned surround- ing lands, the limits of which were determined by metes and bounds; the record and adjudication of pueblo boundaries were in the hands of the village chief, who apportioned agricultural plots to his subjects.44. As in many modern Indian areas of Mexico, the aboriginal concept of village lands and their established boundaries is indurated in the present political and economic structure of the Tarascan pueblos.® Such holdings in the Sierra include various types of land: monte, or woodland pasture on steep mountain slopes and on lava flows; cropland in basin floors (planes, t'pakua), on lower mountain slopes (/aderas, uandten), and in craters of cinder cones (joyas, t pakua-supiéu). In La Canada often the following lands are held by a given pueblo: irrigable alluvium on the valley floor, temporal lands and monte on the adjacent slopes, and hwmedad lands in the Sierra. In the Lake area types of land vary from pueblo to pueblo. Often small strips of irrigable vegetable plots are held along the lake shore; most towns hold temporal land on the lower slopes; those on 43 Although used in most Spanish towns (except mining centers) in New Spain since the late 16th century, tiles began to appear in the Lake Patzcuaro district only in the late 18th century. In 1789 Patzcuaro was the only town in the vicinity with tile roofs (approximately 50 percent of the houses were roofed with tile, the remainder, with shakes). In the same year one house in Naranja boasted of a tile roof. (AGN Historia, vol. 73, ff. 285, 318.) 44 A copy of an aboriginal land title (1519) of CheranStzicurin is extant in AQN Tierras, vol. 867, exped. 8. 45 In many respects the native land system in central Mexico paralleled that of 16th century Spain. Farticularly was this true in regard to the concept of village holdings, the community. the western and southern shore often have fields in the Sierra. Two systems of land ownership—communal and private—prevail in most of modern Tarasca. Since the land reforms of 1915, the ejido, a third type of holding, has displaced most of the hacien- das around the margins of the Sierra. Since Spanish contact most of the Tarascan agricultural land has become private property of family heads. Even in the few remaining pueblos which claim complete communal ownership of their lands, a strong individualization of property has developed. The historical process of the shift from communal to private ownership is not clear. Late 18th-century documents on land disputes among the Tarascan pueblos indicate that at that time the communal system prevailed at least in the Sierra. The issuance of individual land titles may not have occurred until after the reforms of 1857. In the Sierra private land- holders (propietarios) often possess one or more plots in the plan, and still others on the less fertile laderas. Size of individual holdings varies greatly, since land is purchasable. Normal hold- ings average 2 to 3 hectares per family. Traces of the communal concept exist in the minds of the modern proprietors. Although legally possible, there is little desire to sell land to nonmembers of If such a transaction should arise, it usually must be approved by the town council. Consequently, pueblo lands are kept intact. Moreover, individual holdings, especially those in the plan, are rarely enclosed, for after harvest the fields are used as communal pasture.” Accordingly, the final date for removal of crops and the first date for planting in unenclosed lands of each pueblo is communally regulated. Vestiges of the ancient land system are retained in the special communal holdings found in most modern Tarascan villages. Five pueblos in La Cafiada—Tanaquillo, Acachuén, Ichdén, Tacuro, and Carapan—retain communal ownership of all lands, at least in name. Family heads are allotted one plot of temporal near the pueblo and another of humedad in the Sierra to the south and east. The individual allotments vary from 2 to 4 46 The Tarascan town council is normally composed of the representante del pueblo and his committee of six. The representante deals with most internal affairs of the pueblo. 47 Fences and ditches are used most frequently to divide cultivated lands from pasture and to separate individual holdings on the /aderas, or slope land. CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—-WEST 33 hectares in size,*8 and may be used indefinitely by the recipient, provided they are not left untilled for more than two successive years. They may be inherited by sons, daughters, or in-laws, and may be divided among them. Tocuaro ©) Qa Sa Va Nocutzepo San Pedrow) \_ Pareo © Tzentzénguaro San Bartolo Pareo Santa Ana \ PATZCUARO oO (Coordinates are approximate) ya fo} 101° 40" 101235! Map 19.—Distribution of fishers around Lake Pdtzcuaro, 1940. Data from official census, 1940, 54 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7 Fishing techniques and associated tools.— Fishing with native Tarascan nets predominates in Lakes Patzcuaro and Zirahuén. Both the net and the hook were employed in pre-Conquest times,!! but at present the latter is of secondary impor- tance. The large chinchorros (uatika) and the smaller éerémekuas are the only nets used today. The former is a seine, employed for catching pescado blanco and trucha in midlake, while the latter, a gill net with a fine mesh, is placed along shore to trap the small é‘ara4ri and k‘uerépu 1” (pl. 8). Prior to the introduction of the trucha the picturesque mariposa or butterfly nets (k‘oru- e¢a) were commonly employed for catching t*iru. Owing to the near extinction of this fish, these nets are no longer seen, except in Janitzio, where they are displayed to tourists. The hand net (cuchara, uiripu, ¢itiru) has likewise practically disappeared. All nets used by the P&tzcuaro fisherman are home-woven. Other fishing tools include the spear (arpén, atdérakua), now used to kill trucha in shallow water, and the hook (anzuelo, jupikata-térakua) .!¥ Shore traps are occasionally used by a few fishers of Uricho and Pudcuaro. Fish poisons are not employed. To improve habitat conditions of open-water fish, such as pescado blanco, portions of the lake bottom are often cleared of aquatic grasses (zacate, pu¢irini) with the uarématdrakua, a pole 3 m. long with a sickle attached to the end. An indispensible fishing tool and means of water transport is the Tarascan canoe, a flat-bottom dugout hewn from a pine or fir log. Owing to the 121 According to the Relacién de Michoac4n, Tarascan officials oversaw the net fishermen and those who fished with hooks (p. 16). Moreover, “. . . de noche pescan con red y de dia con ansuelo” (p. 149). 122 The chinchorro often measures 100 to 150 m. long and 8 m. wide. In the center is a pocket (bolsa) of fine mesh. Four people are necessary to handle the net in midlake, and it is usually operated from one boat. The net is manipulated by ropes (an¢itatarakueéa), 50 to 60 m. long attached to its twoends. Once the net is cast, it is formed in a semicircle and slowly pulled forward and upward, while the catch setiles into the bolsa. The éerémekua is usually 6 to 8 m. long and 40 cm, wide. This net is used somewhat like a trap. It is fastened to poles in shallow water near the shore and left for 2 or 3 hours. When lifted, the net usually contains several small littoral fish, their heads caught in the fine mesh. This type of éerémekua can be operated by one person. A longer Gerémekua (often 100 m. in length) with a coarser mesh is sometimes used to catch pescado blanco in deep water offshore. Like the smaller variety, it is operated by one person, who attaches the top of the net to log floats and one end to his canoe. The net and boat are permitted to drift in midlake usually through the night, while the attendant gathers in the trapped fish from time to time. 13 The atarakua is composed of a stalk of carrizo 4 m. long, to the end of which is attached a long barbed-iron point (60 cm. long). The spear is hurled either above or beneath the water. Regarding the use of the anzuelo, the cord supporting the hook is usually attached to a piece of carrizo or otate, 1 m. long, a series of which is permitted to float on the water. A strike is indicated by the tilting of the stick, which is hurriedly picked up by the boatman, drying up of lakes in the northern and western sections of Tarasca, the distribution of the dugout has decreased in area during the last 100 years. At the present time the Tarascan boat is used on Lakes Patzcuaro, Zirahuén, Cuitzeo, and Chapala; two old dugouts on the small pond at Tarejero represent the remnants of the once extensive canoe traffic in the Zacapu lagoon.'* Most of the Lake Patzcuaro boats are made in the Sierra settlements of Cumachuén, Capacuaro, and in the highlands to the south, mainly around the rancho of Santa Juana. The boats are dragged to the lake shore, where they sell for 100 to more than 600 pesos each. They are said to last for 3 to 5 years before becoming waterlogged. Two sizes of boats are seen on Lake Pétzcuaro—the small ié4zuta for two to four persons, used for shore fishing, and the larger tep4ri, which carries from four to eight individuals and is employed in midlake fishing and for transport. "The smaller boat is paddled with the pala or 8étakua, which has a round blade of pine (25 & 28 cm.) attached to a handle of oak or tejocote varying in length from 30 cm. (for children) to over 2m. The larger canoes are both paddled and rowed. Sierra folk from Cumachuén and Capacuaro manufacture oars and paddles, which they market in Erongaricuaro and Paétz- cuaro. Fishing methods.—In most parts of the lake, fishing is done in the early morning hours between 5 and 10 o’clock. Fishing is seasonal, most activity occurring during the dry season (Novem- ber to May). Chinchorreros usually operate in groups of four; often blood relations, the group divides the catch equally. An owner of a net and boat often hires peones to help with the chinchorro, paying wages or dividing the catch. The wife and children occasionally help set the éerémekua along the shore, and often women aid with the chinchorro. Midlake fishing is open to all inhabi- tants of the Lake area, who pay a federal license of 1.50 pesos annually. By custom, however, the people of a particular settlement have exclusive fishing rights along the shore of their lands; those from other pueblos may not fish the shores of 14 As late as 1872 heavy canoe traffic is described between TareJero and Zacapu (Pérez Herndéndez, 1872, p. 119). Late in the 16th century small reed balsas were used on Lake Chapala (Ponce Relacion, vol. 2, pp. 18-20). 125 Measurements of the dugouts: The itézuta has a length of 2.5 m. to 6.5 m., width of 60 cm., and depth of 40cm.; the tepari ranges from 6.5 to 11m long, 1 m. wide, and 50 em. deep. CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—-WEST 5D another without permission from the authorities of the latter. Fish preparation.—Pescado blanco, trucha, and aktimaiza are usually taken to market fresh, al- though the latter is sometimes fried on the comal before being sold. The tiny k‘uerépu and @‘arari, however, are invariably sun-dried, the catch being spread on a petate, which is placed near the door of the dwelling where it can be easily watched (pl. 11). Since pre-Conquest days dried é‘arari has been one of the main exports of the Tarascan lakes. It was distributed into the tierra caliente, the Sierra, and as far east as Toluca. LUMBERING ACTIVITIES The Tarascans, possibly more than any other aboriginal group of Mexico, have been exploiters of forest products since pre-Columbian times. During the Empire period one of the important officials of the caltzontzin at Tzintzuntzan was in charge of ‘‘the keepers of the forests,’ who cut beams and made planks for public, and probably private, use.”® Not only were large beams and logs used in the construction of temples, but also in the building of forts against Aztec raids. During the colonial period the pine forests on the northern flanks of the Sierra de Ozumatlin were heavily exploited by Tarascan woodmen for beams, planks, and shakes for the Guanajauto and Zaca- tecas mining districts.” Much of the timber resource of northern Michoacén was depleted by the end of the 18th century. Relatively untouched by colonial exploi- tation, the pine and fir forests of the Sierra de los Tarascos, although constantly diminishing, have remained the principal source of timber for the indigenous population. There are few contem- porary Sierra Tarascan men who cannot handle an ax or lumber saw. When the maize fields do not demand their attention, the family head and his sons are usually in the forest cutting timber or gathering resin. The Sierra Indian is conse- quently both a farmer and a lumberjack. Some are professional woodsmen, who live in the village but seldom engage in agriculture. Little lumber- jim Relacion de Michoacan: p.17: “. . . diputado sobre los que guardaban los montes que tenian cargo de cortar vigas y hacer tablas y otra madera de los mon- ee This exploitation began immediately after the Guanajuato mines were opened ca. 1554, and extended into the post-colonial period. After the ex- haustion of the local wood supply, Zacatecas began to draw on the northern Michoacan lumber reserves during the first part of the 17th century (Basa- lenque, 1886, vol. 1, p. 315). ing is carried on outside the Sierra. Some beams and planks are cut by the people of Zipiajo and Teremendo, who have large tracts of forest on the slopes of El Zirate, and some farmers of the Lake area and La Cafiada cut small amounts of lumber for home use. Beals’ discussion (1946, pp. 15-19) of legal cutting rights, lumber products, and lumber tools for Cherin can be applied to most of the present Sierra pueblos; therefore, only a summary will be given here. As mentioned above, all Sierra pueblos possess varying amounts of forest land held as common property. Since the late 1930’s the Federal Government has attempted to control exploitation by placing all large forest areas under national domain, by encouraging the organization of local lumbering cooperatives, and by periodically inspecting lumbering activities. In most pueblos the Federal tax on lumber prod- ucts is passed on to the individual woodsmen, who pay the town council a given amount for cutting rights. In other towns lumber coopera- tives have been formed to pay the tax, each member contributing dues and having sole cutting rights in the village forest lands. Although much lumber is for local use (house construction, fences, acqueducts, watering troughs, shakes, etc.), most is cut for the outside market. Raw logs, beams (vigas), planks (vigetas, tablas), and railroad ties of pine and fir are cut and pre- pared for lumber contractors, whose heavy trucks visit the larger villages during the dry season to haul the products to the nearest railhead. Wood- cutters of the remote pueblos drag beams and planks to market with the aid of burros and mules. Los Reyes, Tingiindin, Tangamandapio, and Zamora handle the forest products from the western part of the Sierra, while Uruapan, Zacapu, Ajuno Station, and Pitzcuaro serve as lumber points for the eastern section. Formerly a signifi- cant forest industry, shake making (performed by skilled specialists) is slowly declining because of the increasing use of tile roofing.’* Turpentine is no longer distilled locally. (See Beals, 1946, p. 18, for illustration of Tarascan still.) Rather, the resin (resina) is gathered in 5-gallon tins and taken to the village, where they are periodically 138 Although in some pueblos (Pamat&cuaro and ranchos, Angahuan, Capacuaro) shakes are still made for export to Uruapan, most are used locally. During colonial times and even in the last century large quantities of shakes were shipped from the Sierra to the northern mines, where they were the principal roofing material. 56 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7 picked up by trucks from turpentine distilleries in Uruapan and Morelia. Charcoal is a minor commercial forest product made by Tarascans living near mestizo towns. The latter comprise the principal markets for charcoal, which has never entered Tarascan culture.’ Other minor forest products consist of ocote splinters, used for primitive interior illumination; *° softwoods (madroiio, jaboncillo, aile, etc.) for lathe work; pine and fir for cabinet work; etc. Within the last 50 years the commercial saw- mill has penetrated into the Sierra. Lumber companies purchase cutting rights of standing timber from the pueblos and set up a steam- or (when near a power line) electric-powered saw in the midst of the forest.“! When the suitable timber has been depleted (under Federal inspec- tion), the mill closes down, and the remnant of the forest reverts to the pueblo. Although most companies bring in mestizo labor, many Tarascans from villages nearby obtain seasonal work in the sawmills, thereby supplementing their usually low income. Because of their ephemeral character, the number of mills in the area varies. In 1940 there were five mills in the Sierra proper; in 1946 the number had decreased to three. During the last 100 years cutting has exceeded natural timber growth in the Sierra. Clearing of new plowland to sustain increased population and commercial lumbering have been the major factors of forest depletion. Moreover, disease has recently destroyed acres of pine in the vicinity of Tarecuato, and volcanic ash has laid waste the forest within a 3-mile radius of Paricutin. Lum- bering even by the Tarascan woodsmen is often wasteful. Large trees are sometimes cut and left unattended for years until rot renders the wood useless.“ Improper tapping for resin and testing for shakes often kill many trees. The sawmills, operating on a much larger scale than the native lumbermen, are even more destructive, and in former years they depleted large sections of Sierra forest. Approximately 50 years ago the timberland in the eastern part of the Sierra east 129 The main charcoal-producing towns in the area are San Lorenzo (Uruapan market), Opopeo and Cuanajo (PAtzcuaro market). 130 The rancheros around Pamatdcuaro gather much ocote, which the women market in the large mestizo towns bordering the Sierra. 131 In 1944 the pueblo of San Felipe sold its forest to an Uruapan company for two million pesos. The proceeds were deposited in an Uruapan bank, where they remain communal property. 132 Such wasteful exploitation was much in evidence in the forest lands of Pamatdécuaro on the southern slope of Cerro de Patamban, of Nahuatzen, Sevina, and Cumachuén was almost completely stripped by the mills. Today in this area, barren, windswept sheep pastures, supporting occasional remnant clumps of pine, indicate the extent of forest destruction (pl. 8). Throughout the Sierra there is probably not a piece of virgin timber, so long and thorough has been lumber exploitation. HANDICRAFTS Among most people lacking modern transporta- tion facilities and mass production techniques, cottage industries, often termed ‘native crafts,” are characteristic of the local economy. Owing to the presence of particular raw materials nearby and/or to traditional skills, people of one village often tend to specialize in one or more crafts. Cottage industry and village specialization are prevalent in most of indigenous and even mestizo Mexico. It is and has been particularly so among the Tarascans, whom the early Spanish chroniclers described as a skilled and clever people (Beau- mont, 1874, vol. 2, p. 165). Moreover, pro- gressive exhaustion of originally poor soils and population increase have forced many farmers of the Sierra to turn to crafts for additional income. Today five general handicrafts (ceramics, textiles, woodwork, leathercraft, and metalwork) are practiced and over 30 types of articles made among 54 Tarascan towns and ranchos (map 20). Only 10 Tarascan-speaking pueblos lack a cottage industry. In 26 pueblos at least 25 percent of the “working” population! practice various crafts. Some villages specialize in only one industry. For example, over 80 percent of the working population of Santa Fé de la Laguna make pot- tery; nine-tenths of that of Jardcuaro are hat makers. Moreover, many towns which carry on various handicrafts may concentrate on one. Thus, Tarecuaro is famed for agave fiber products, Pamatdcuaro and neighboring ranchos for wooden spoons and bowls. In most pueblos more than one craft is practiced, and in a few as many as eight distinct products are made. Like so many of his material culture elements, the Tarascan’s crafts represent a mixture of 133 The ‘‘working’’ population in Tarascan towns is estimated by dividing the total population by 3.5. The Tarascan family averages about 5 persons, but often the wife devotes her spare time to cottage industry and is sometimes helped by the older children. Boys over 12 years old usually work in the fields as farmers or in the house at the father’s trade. CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—WEST 57 aboriginal and European products and techniques. lost of his modern handicrafts are based on pre-Conquest industries (ceramics; wood prod- ucts; leathercrafts; metal work in copper; weaving of cotton, agave fiber, stalks of tule). Except in a few pueblos, European techniques are now used in making pottery. In modern wood- work the adz and the lathe are probably European and cabinet work is practiced entirely with Old World techniques. Cattle hide and horse hide have replaced deerskin in leathercrafts, but the tanning techniques used are possibly aboriginal. Although the ancient belt loom is used for most cotton and agave weaving, for weaving wool the European hand loom is employed. Sleeping mats (petates) are woven of tule as they were 500 years ago; hat making, on the other nand, is completely European. In regard to metals, European tech- niques have replaced native methods, and iron has of course been introduced. Spanish friars and master craftsmen of the 16th century did in- deed teach Tarascans many new techniques, but in most instances such were applied to long- established native industries. An interesting aspect of cottage industriesjis their ephemeral character. Owing to movement of artisan families from one pueblo to another and changes in markets and fashions, certain crafts disappear in some towns and reappear in others. In the last 160 years 37 Tarascan villages and ranchos have lost old crafts or gained new ones; 27 have retained their characteristic trades (table 2).% The pottery industry in Santa Fé de la Laguna dates only from the last quarter of the 19th century, and in 1910 hat making was brought into Jardcuaro by a few political refugees from Pichétaro. A large number of Tarascan towns were famed for leathercrafts (saddles and shoes) during the 18th and 19th centuries, but now, owing to changes in transportation and the rise of factory production, local leather products have almost disappeared. Again, the iron craft of San Felipe de los Herreros has practically vanished, for factory-made articles can be obtained more cheaply from surrounding mestizo towns. 134 Insufficient data were at hand to determine possible changes in home industries for 20 towns and ranches. TaBLE 2.—WNative crafts in} Tarascan villages ! Pueblo 1946 1841 1822 1789 None. (?) (?) (?) Weaving (cotton): Weaving (cotton): Knitting: Knitting: Rebozos. Mantas. Men's stockings of cotton Men’s cotton stockings. Belts. Belts. thread. Tablecloths. Woodwork: Knitting: Violins. Men's stockings. Turned work. An vahuan=-= -2o-c== neue Weaving (cotton): Woodwork: Woodwork: Woodwork: Rebozos. Shakes, Shakes. Boxes. Belts. Aprons. Tablecloths. Arantepacua- -=-.-=--<.-=-=-= Capotes. (?) (?) Woodwork: Brooms. Saddle frames. Aranza.- === 2222-2282" ---= Weaving (cotton): (?) (?) (Depopulated.) Belts. Tablecloths, Arocutin==.—- sca. sesssese eats None. (2) (2) Petate weaving. Atapansa2.22--- ees Weaving (cotton): (2) (?) Leatherwork: Belts. Tanning. Weaving (wool): Shoes. Blankets. See footnote at end of table. 58 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7 TABLE 2.—WNative crafts in Tarascan villages '|—Continued Pueblo 1946 1841 Caltzontzin (Paricutin) -_____- Capacuaros2- =: =2--2--/---2- Charapanz<2-2-22 2-225. Oherines e252 25.4 A Cheranftzcicutin ___._.____. Ohilchota.22 =~ .2:-222222-.225 Coenchoses2-22 2.22 Gomanjs 2 = et a eee 22 Conejos, Los (Parangari- cutiro). Weaving (cotton): Tablecloths. Weaving (wool): Blankets. Woodwork: Broom handles. Weaving (cotton): Belts. None. Weaving (cotton): Rebozos. Belts. Aprons. Tablecloths. Weaving (wool): Blankets, | Hat making: Palm leaf. Weaving (cotton): Belts. Napkins. Tablecloths, Weaving (wool): Blankets. Hat making: Palm leaf. Embroidery work. None. Weaving (wool): Blankets. Basketry. Pottery. Leatherwork: Shoes. Belts. Saddle leather. Pottery. Pottery. Weaving (wool): Blankets. Woodwork: Cabinetmaking. Weaving (wool): Blankets. Woodwork: Cabinet work: Boxes. See footnote at end of table. Weaving (cotton). Woodwork: Boxes. (?) Weaving (cotton). Woodwork: Rosaries. Chocolate beaters. (?) (?) Pottery. Woodwork: Rosaries. (2) (?) Weaving (wool): Blankets. Weaving (cotton). Woodwork: Boxes. Weaving (cotton). Woodwork: Cabinet work. 1822 1789 (2) Weaving (cotton). (?) Woodwork: Boxes. (?) (2) Woodwork: Weaving (cotton, Rosaries. Woodwork: Malacates. Rosaries. Leatherwork: Leatherwork (1742). Tanning. Shoes, None. Leatherwork: ‘Tanning. Shoes, (?) (?) Woodwork: Pottery. Rosaries, Woodwork: Rosaries. Other turned work. Woodwork (1742): Saddle frames. Pottery (1742). Leatherwork: Leatherwork: Tanning. Tanning. Shoes, Shoes. (2) Leatherwork: Tanning. Shoes, Weaving (wool): Blankets, Woodwork: Piloncillo molds, Boxes. (2) Weaving (cotton). Woodwork: Boxes, Woodwork: Cabinet work. Boxes, CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—-WEST TABLE 2.—Native crafts in Tarascan villages \—Continued Pueblo 1946 1841 1822 1789 Cuanajo—Continued-----_--- Weaving (cotton): Belts. 2 Aprons. Tablecloths. Weaving (wool): Blankets. Cumachuén:--2---------=-.- Woodwork: Woodwork. Woodwork: Woodwork: Bateas. Digging sticks. Digging sticks. Weaving (wool): Oars. Oars, Blankets. Woodwork (1742): Saddle frames. Erongarfcuaro_-_--___--------- Petate weaving (?) Petate weaving. (?) Eu Snsito: -sseese Seth 2S Pottery. (?) (?) (2) Nehante 2220 soe ane sea one Pottery. (?) (?) (?) Mn wAtziove sees se er sso Petate weaving. (?) (2) (2) Basketry. Wanitzio’=2e--- = ess. = 2 Netting. (?) (?) Netting. ‘ Weaving (cotton): Men's belts. WAYACUAYO = ae" Sas ocsastec Hat making. Petate weaving. (?) Petate weaving. Palm leaf. Weaving. Belts. Adobe making. Majbacandass2<2-2-2.-=c=-. 3 None. (2) (2) (2) INahuatzen’=-2-- == + S.2-2--22 Weaving (wool): Leatherwork: Leatherwork: Leatherwork: Blankets. Tanning. Tanning. Shoes. Cloth. Shoes. Shoes, Saddles. Saddles. Weaving (cotton): Belts. Embroidery work. Leatherwork: Saddles. Belts. INaranjarss2-c2=2=2eemee ete None. (?) (2) Leatherwork: Tanning. Shoes. Napizaro:=- s52=2=-~-===55--5" Petate weaving. (2) (2) (?) IN OCULZeDO == = ose nee None. (?) (2?) None, iINurlote et es eo sees. = Weaving (wool): Hat making: Hat making. Hat making: Blankets. Felt. Felt. ‘Ocumicho:=- 22222 --- seen nes Clay toys. (?) Leatherwork: Leatherwork: Tanning. Tanning. Shoes. Shoes. Weaving (cotton), iPamatacnaro.. 2 2-22 snene ss Woodwork: Woodwork: Woodwork: Woodwork: Spoons. Spoons. Spoons. Spoons, Bateas. Digging sticks. Digging sticks. Digging sticks, Hat making: Weaving (cotton). Weaving (cotton). Wheat straw. * Weaving (wool): Blankets. See footnote at end of table. 748988-—4 8——_5 59 60 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7 TABLE 2.—WNative crafts in Tarascan villages \—Continued Pueblo 1946 1841 1822 1789 ParachOsseascces seca ee Woodwork: Woodwork: Woodwork: Woodwork: Musical instrument. Musical instrument. Musicil instrument. Musical instrument. Turned work. Cabinet work. Cabinet work. Cabinet work. Cabinet work. Saddle frames. Toys. Weaving (cotton): Rebozos. Weaving (wool): Blankets. Patamban____- ELE Ste geae le Pottery. (2) Pottery. Pottery. Weaving (wool): Blankets. bichstaro==ar-. see ce nee ee Weaving (wool): Weaving (agave). (?) Woodwork: Blankets. Woodwork: Cabinet work. Weaving (cotton): Cabinet work. Belts. Rebozos. Woodwork: Cabinet work. | Broom handles. Bateas. Hat making: Palm leaf. Petate weaving. Pomacuarfn- ---.--...-.____- None. Weaving (cotton). Knitting: (?) Knitting: Men’s stockings. Woodwork (1742): Men’s stockings. Saddle frames, Pottery (?). Pufcuaro.........___ ____....| Petate weaving. (?) (?) (?) Weaving (wool): Blankets. Quinceo= <== == --2-_ 2-22 <5; | Weaving (wool): Woodwork: Woodwork: Woodwork: Blankets. Saddle frames, Saddle frames, Saddle frames. Weaving (cotton): Belts. Capotes. Quriopas..2<2-22<-soste-ceece Woodwork: (?) Woodwork: Woodwork: Bateas. Bateas, Bateas. Turned work. Boxes. Woodwork (1742): Chairs. Bateas. Boxes. San Andrés_._...._____________] Petate weaving. Petate weaving. Petate weaving. Petate weaving. San Angoel......__......._____] None. (?) (?) None. Bantaulé6! 2-2 2--2)-2--._- "| Pottery. (?) Woodwork. Woodwork: Bateas (painted), Boxes (painted). Petate weaving. San Felipe-_--..___. wiemee: Se Ironwork. Ironwork. Ironwork. Ironwork (also in 1644). Weaving (cotton): Belts. Weaving (wool): Blankets. San Jerénimo....__......-.-- Petate weaving. (?) Petate weaving. Petate weaving. Weaving (wool): Belts. Blankets. See footnote at end of table. Woodwork: Boxes. Pueblo San Jos6_____ San Lorenzo----_- Sz secseesees wRanaquillo: 92) -=2 22.20 2252-2 MarecwAatos 2282 S202. ve se Ss eharejerOve oa. bese oe ee | FRETEMONGO neti s eee eno oe Mrinidaroys2s22-.os 2. mMocuaro-=S4s<_ 5. ee Sk CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—WEST TaBLE 2.—Native crafts in Tarascan villages \—Continued 61 1946 1841 1822 1789 Pottery. (?) Leather work: (?) Tanning. Woodwork: Saddle frames, Weaving (cotton): (?) (?) (?) Belts. Tablecloths. Pottery. (?) (?) (?) Woodwork: Woodwork: Woodwork: Woodwork: Bateas. Shakes. Shakes. Saddle frames. Weaving (cotton): Belts. Weaving (wool): Blankets. None. None. None. Weaving (cotton). Woodwork: (Nonexistent.) (Nonexistent.) (Nonexistent.) Spoons. Bateas. Pottery. (?) (2) (?) Petate weaving. Capote making. Weaving (wool): Blankets. Weaving (agave): Morrales. Ayates. Pottery. Weaving (agave): Morrales, Ayates. Costales. Weaving (cotton): Belts. Embroidery work. Rope making. None. Hat making: Wheat straw. Palm leaf. Weaving (wool): Blankets. Pottery: (Hat making ceased in 1936.) Woodwork: Bateas. Spoons. Masks. Pottery. See footnote at end of table 748988—48——6 Petate weaving. None. (?) (?) (?) (?) (?) (2) (7) Petate weaving. (?) (?) (?) (?) Leatherwork: Shoes. @) () @) Petate weaving. (?) Pottery (1742). Woodworking (1742). Saddle frames. (?) Weaving (agave). Leatherwork: Tanning. Shoes. (?) Leatherwork: Tanning. Shoes. None. 62 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7 TaBLe 2.—Native crafts in Tarascan villages \—Continued Pueblo | 1946, 1841 1822 1789 TPUPCUBTO: 2 o- ane soon a one = | Stonework: Stonework: Stonework: (?) Metates. Metates. Metates. | Woodwork: Bateas. Broom handles. | Weaving (cotton): Belts. Weaving (wool): Blankets. Capote making, Tzintzuntzan ---_- Pottery. Pottery. Pottery. Pottery. Urapicho..._.._..._._._.__..-| Hat making: None. None (?). (?) Palm leaf. Woodwork (1742): Saddle frames. Uricho-=-=--<- __| Petate weaving. (2) Petate weaving. ASCO oneness ates | (2) Weaving (cotton). Weaving (cotton): (?) Mantas, Woodwork (1644): Bateas. Rope making (1664). MALOSLO= sone h cca see _...----| Woodwork: Woodwork: Woodwork: Woodwork: Bateas (disappeared since Bateas. Bateas (painted). Bateas. voleano). Spoons. Piloncillo molds, Weaving (wool): Weaving (cotton)’ Woodwork (1644): Blankets. Bateas. Rope making (1664). ! Sources: 1644, Basalenque (1886); 1742, Villasenor y SAnchez (1746-48): 1789, AGN, Historia, vol. 73; 1822, Martinez de Lejarza (1824); 1841, AAM, siglo XIX, leg. 704, Memorias Estadisticas, 1841; 1946, Field observation. Some industries, important in pre-Conquest times, have completely disappeared. The fine Tarascan featherwork was nearly extinct by the beginning of the 18th century (Escobar, 1924, pp. 149-151). Furthermore, the use of the ground pith of maize stalks, from which various objects (mainly religious) were molded, apparently flared in the 17th and 18th centuries, and then dis- appeared (Escobar, 1924, p. 144). On the other hand, crafts which have persisted in some pueblos for the last 160 years may predate the Conquest. Witness the leatherwork of Nahuatzen, a leather-making center in 1640, where both deer and cow hides were tanned (Zavala and Castello, 1939-46, vol. 7, pp. 361-362); the many towns which still specialize in cotton weaving with the belt loom; the petate-making towns around the shores of Lake Pitzcuaro. CERAMICS Clayware is indispensable in most Mexican kitchens,’ and tile roofing is used extensively in most parts of the country. As in pre-Conquest days, the manufacture of clayware in Mexico is still a cottage industry in which various towns specialize. Including Tzintzuntzan (largely mestizo), there are nine pottery towns in the present Tarascan area: Santa Fé, Comanja, Zipiajo, Hudnsito, Santo Tomas, San José, Patamban, and Cocucho. With the exception of Cocucho, all are located in the Garénda, or clay-soils district north of the Sierra, usually near deposits of suitable firing clay (map 20). The Cocucho potters have always hauled clay from the vicinity of Tangancicuaro and San José, for suitable deposits rarely occur in the Sierra. Other pottery towns, now mestizo, are also located in the northern clay area (Tangan- cicuaro, Capula, Villa Morelos, Penicuaro). More- over, other Tarascan villages in La Canada (Sopoco, Ichaén, Tacuro, Tanaquillo), in the Zacapu 136 The common clay kitchen utensils include various types of pots (ollas) for boiling; the comal, or round, flat piece placed on the hearth for frying, broil- ing, and toasting; small saucers (caswelas) for frying and from which food is sometimes eaten; water jugs (cAntaros); drinking cups (vasos). CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—WEST 63 Basin (Tirindaro), and in the Lake area (San Jerénimo and Erongaricuaro) make pottery on a small scale, mainly for local use. Modern Tarascans use both the hand and the mold techniques. The latter is usually accom- panied by application of lead oxide glaze. The former is still used in only three pueblos—Co- manja, Zipiajo, and Cocucho, where it is per- formed solely by women.'* In Comanja_ the lower part of the vessel is shaped from a single daub of clay. A depression is made in the center and the walls are built up with the hands by press- ing in small daubs of clay. The outer and inner surfaces are smoothed with a corneob. The result is a well-balanced vessel with walls of even thick- ness. The vessels are rough-finished, rarely pol- ished, and litharge glaze is never employed. Firing is accomplished by placing pottery on a pile of dried manure. The pots are covered with dried grass (zacatén), which, when lighted, ignites the manure. The grass ash is permitted to cover the pots, a hole being left in the center of the pile to permit smoke from the smoldering manure to escape. After 3 hours the pottery is fired to sufficient hardness. The chief ceramic products of Comanja are the large water ollas, called “‘coman- jas,’”’ which are marketed in the Sierra, the Lake area, and in some of the mestizo towns to the north. Similar ollas are made by an identical process in Zipiajo, but on a smaller scale. In Cocucho the ceramic process is similar to that of Comanja, except that the base of the vessel is formed on the bottom of a broken olla and part of the wall is built up of rolled pieces of clay (pls. 9 and 10). Firing is also similar, but pine bark and rotten wood, rather than manure, is employed for fuel; this process probably represents the truly aboriginal technique. The Cocucho women make large ollas with thick walls, especially famed as tamale cooking pots throughout the Sierra. This olla, rarely used outside of the Sierra, is called kukiéu, from which the village derives its name. The tunu¢i, a small flat olla used as a tlascal (receptacle for tortillas), is also made. 136 The native hand technique was practiced in other Tarascan towns during the 18th century. In 1729, according to Matias de Escobar, ‘‘ Es cosa que admirar como que los he visto en Tiripitio [southwest of Morelia] como labran cuanto [losa] quieran, sin las ruedas y moldes de los Espanoles. Un pequeno cuero y una mala navaja son todos los instrumentos con que obran”’ (Escobar, 1924, p. 148). Both the hand and mold methods appear to be native in Mexico, although the latter was known to Europeans. See Foster, 1948, for a discussion of native and introduced elements in the modern mold technique. The manufacture of these two Tarascan pots is slowly dying. In 1946 only 10 women were making pottery in Cocucho, whereas in 1841 it was made in practically every household of the village (AAM, siglo XIX, leg. 707). Today by far the greater amount of Tarascan pottery is made with molds by both men and women.” None is manufactured with the potter’s wheel. All who use molds have taken over the European glaze technique and the firing oven. Tarascan mold-made pottery can be differentiated according to finish. The ‘“Patam- ban” type, for instance, carries a beautiful green glaze, known and admired over most of western Mexico." Green glaze is also used in Santo Tomas and Santa Fé de la Laguna, having been recently introduced into the latter pueblo. Pot- tery hand-painted with brilliant floral designs on a background of black glaze is a specialty of Santa Fé de la Laguna. This unusual technique was introduced around 1900, and was readily adopted by the inhabitants, whose former industry was batea painting. As mentioned previously, the inhabitants of Santa Fé de la Laguna began to make pots during the last quarter of the 19th century. Since then their ware has become known throughout Mexico, and some is imported by United States curio shops. In 1936 the technique spread to Tirindaro, when daughters of a Santa Fé potter married into Tuirindaro families. The most common modern household pottery is the Red ware, either glazed or polished, made in Tzintzuntzan, Hudnsito, San José, and Patamban. Before being fired the large pieces, such as ollas and cdntaros, are usually slipped with a red clay solution and then burnished with iron pyrites. A handsomely polished surface, similar to that of the pre-Conquest wares, results after firing. (Such ware is fired only once.) Smaller pieces are often glazed with litharge. Glazed pieces are fired twice, the litharge being applied after the first firing and the glazed surface appearing after the second. Designs are often painted in white (tierra blanca) and black (terra de hormigén). Red ware is carried as far as Guadal- 137 See Foster (1948) for a detailed description of the mold technique used by the potters of Tzintzuntzan. 138 To produce the green color, pulverized copper oxide (cobre quemado) and yellow flinty quartz (pedernal) are added to the lead oxide (litharge) solution, which is applied to the pottery before firing. A black glaze is also made by adding a mineral called tierra de hormiga and pedernal to the litharge. 64 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7 ajara, Morelia, the tierra caliente of Guerrero, and Mexico City. Another type of ceramic industry is represented by the clay toy figurines made by the women of Ocumicho in their spare time. The hollow figures are formed with molds in shapes of diminutive horses, sheep, oxen, and men, each with an open- ing which serves as a whistle. After firmg, they are painted and varnished. Owing to complete lack of water near the town in the dry season, this activity is carried on only during the rains. Ocumicho figurines are seen in markets in many parts of western Mexico and the tierra caliente of Guerrero and Michoacan. Red clay tiles, which are slowly replacing shakes in the Tarascan area, are made in some pueblos within the clay belt on the margins of the Sierra. Tanaco is the sole town within the Sierra proper to make this product. In Nahuatzen the technique of making flat concrete tiles was intro- duced in 1944. Such tiles are replacing the less durable clay ones in some mestizo towns. TEXTILES In 35 modern Tarascan villages spinning and weaving of cotton, wool, or agave fiber are carried on as cottage industries. Both indigenous and European techniques are employed, neither having changed since the 16th century. Since the beginning of the present century, however, factory- made textiles from large Mexican towns have begun to displace some home-woven articles, but indigenous conservatism still supports the native handicraft. Spinning.—Formerly Tarascan weavers spun raw cotton from the tierra caliente, but at present commercial cotton thread, purchased in mestizo markets, is prepared for weaving by twisting five to six strands on the spinning wheel. Today only raw wool and agave fiber are homespun, the latter with the native malacate (uipinu), or hand spindle with round clay wheel, the former with the 16th century spinning wheel (lorno). (See Beals, 1946, p. 36, for illustration of spinning wheel.) Both cotton thread and spun wool are usually colored locally with aniline dyes purchased in mestizo markets. . Weaving.—Tarascans weave all agave and cotton fabrics on the native belt loom (patakua (Paracho); jopdsatakua (Charapan, Tarecuato)), a horizontal loom which has a backstrap and is found in most parts of indigenous America south of the United States (pl. 11). Customarily, only women operate this loom; however, in Tarecuato agave fiber is woven with it by both men and women, and in Tanaco, exclusively by men. Until the 1880’s the most important fabric made with the belt loom was the cotton manta, a simple white cloth used for native clothing since pre- Conquest days. The cheap factory-made cottons of Puebla and Veracruz have completely displaced the indigenous manta, so that today Tarascans weave women’s and men’s belts (fajas), shawls (rebozos), aprons (delanteras), tablecloths and napkins (servilletas). Widths of cloth ranging from 1% inches (women’s belts) to more than a yard (rebozos) can be woven on these looms. Designs are usually woven into the above-named articles, the warp threads being first arranged for large widths on a long stick (Sekudérakua) and for the narrow fajas on the Sekudni, an arrangement of four to five small sticks placed in the ground. Some of the finest examples of cotton weaving are found in the Sierra pueblos: Paracho (whose women make the Tarascan ‘‘rebozo corriente’’), Ahufran (women’s belts), Angahuan (women’s belts, aprons, rebozos), Charapan (belts, aprons, tablecloths), San Lorenzo (tablecloths, belts). In the early colonial period the weaving of agave fiber was apparently widespread in the Sierra (AGN Congregaciones, f. 14), but today it is limited to Tarecuato and Tanaco. In these villages the main agave fiber products are morrales (square bag with shoulder straps), ayates (coarse piece for wrapping articles to be carried on back), and costales (coarsely woven sacks for carrying goods on mules and burros). The fiber of maguey bruto (akaémba t'aaimiti) is used for the finely woven morrales, while that of maguey del toro (torakaémba) is employed for the coarser ayates and costales. Leaves of the agave plant are cut and the fiber extracted and carded. After drying, it is spun by (1) rolling fibers on the thigh with the band, or (2) with the malacate. The fibers are woven on the belt loom in the same fashion as cotton’ (pl. 11). A piece of the agave fabric is doubled over and sewn on the sides to make the morral, and a shoulder cord is added. Other agave fiber products made in Tarecuato include rope and 139 Agave fiber products were manufactured in Pichdtaro during the last century (AAM, siglo XIX, leg. 707). 40 The loom for weaving agave fiber is called u4natakua in Tarecuato. CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—WEST 65 cord; these and the woven articles are marketed in Guanajuato, Jalisco, the tierra caliente, and in all parts of the present Tarascan area. Woolen products are woven mainly on the European loom, which was introduced early in the 16th century." During most of the colonial period this loom was used principally in the obrajes, or cloth mills established by Spaniards in various parts of Mexico near an abundant supply of wool. Indians first learned European weaving techniques in these mills, the labor for which came from surrounding native pueblos. By 1540 an obraje, operated by 26 forced native workers, had been set up in Acdmbaro (Paso y Troncoso, 1905, vol. 1, p. 33), and before the close of the century woolen mills existed in Taximaroa and Valladolid (Zavala and Castello, 1939-46, vol. 6, p. 225). Moreover, Indians quickly learned to spin wool, for tributes of spun wool were exacted from some pueblos, possibly to supply obrajes nearby.” It is not clear when the Tarascans began to use the hand loom in their own villages; possibly some looms were set up in the northern towns in the 16th century.'® A report of 1789 (AGN Historia, vol. 73) on the Tarascan pueblos of Lake Patzcuaro and the Sierra, however, men- tions the use only of the native loom. The first indication of a native wool industry in the Taras- can area comes from the Martinez de Lejarza report of 1822, which cites the obrajeros of San Juan Parangaricutiro (later the most renowned of the Tarascan blanket-weaving towns) and of several northern mestizo towns.'* Tarascan wool weaving on a commercial scale may be post- colonial, having little economic basis until the break-down of the large woolen mills at the close of the colonial period. Today woolen blankets (cobijas, serapes) are made on the European hand loom in 24 Tarascan towns, Nahuatzen and pre- volcano Parangaricutiro being the largest pro- 141 Strands of wool are sometimes mixed with cotton in making women’s belts. Often the warp is of woolen strands, the woof of cotton thread. 142 For example, ea. 1540 the people of Purudndiro (Michoacin) contributed each week two arrobas of spun wool (Paso y Troncoso, 1905, vol. 1, p. 117). 43 The Relacion de Chilchota (Mus. Nac.) states that some natives in the town made clothes of wool, but the type of loom used is not given. More- over, according to the Relacion de Cuitzeo (Mus. Nac.), the Indians living around the lake “‘. . . benden lana a los conmarcanos para hacer ropa para vestirse, y sus mugeres la benefician...’’ Again, the type of loom used to weave wool is not given. “4The northern towns mentioned: Morelia, Zinapécuaro, Zitécuaro, Taximaroa, Jiquilpan, Huarachita, La Piedad, Huaniqueo, and Tanga- mandapio. At that time the latter pueblo was wholly Tarascan; according to Martinez de Lejarza (1824, p. 227), “‘. . . sus habitantes trabajan telares de algodén y lana.’” ducers. In many towns only three of four obrajeros operate full time and produce mainly for local consumption. Raw wool is purchased locally, is washed, carded, dried, and spun by the obrajero. In addition to manufacturing blankets, some weavers in Nahuatzen, Charapan, and Tanaco make woolen cloth for the traditional black skirt, which is still worn by most Tarascan women. Such skirts, however, are being made increasingly from factory-woven woolens pur- chased in mestizo towns. Embroidery and sewing.—In the Sierra villages of San Lorenzo, Tarecuato, Angahuan, Ahuiran, Cuanajo, Nahuatzen, and Charapan some women specialize in cross-stitching and embroidering designs on blouses (huzpiles), napkins, and table- cloths. Many of these articles are for tourist trade in Uruapan, Zamora, and Patzcuaro. During the colonial period and the first half of the 19th century, the men and women of Ahuiran and Pomacuarda knitted men’s stockings of cotton thread, using otate needles (AGN Historia, vol. 73, f. 344; Martinez de Lejarza, 1824, pp. 179-180). Ahuiran stockings were sold to mestizos and Spaniards over a wide area, but this trade declined after the change in styles of men’s clothing in the early 1800’s. Hat making.—Among the Tarascans this indus- try was introduced probably in early colonial days.“ However, the first mention of the in- dustry comes from the report of 1789, which cites it in Nurio (AGN Historia, vol. 73, f. 348). There, hats were made of wool, likely by a felting process, but the industry had disappeared by the end of the last century. None of the colonial sources mentions the manufacture of straw hats in Tarascan towns. Old men from Pichataro remember hat making during their childhood, which fact at least dates the industry in the last half of the 19th century. (Palm-leaf hats were made in Morelia at the end of the colonial period, according to Martinez de Lejarza, 1824, p. 29.) Today hats (principally of palm leaf, some of wheat straw) are made in seven Tarascan towns, Jaracuaro Island being the main center.’ Palm leaf brought up from the tierra caliente is cut in thin sections, which are braided into strips, called 48 According to tradition, hat making was one of the many industries which Don Vasco de Quiroga taught the natives. (Leon, 1904, p. 63.) 448 At least one member (and often three or four) ofevery family on Jaracuaro Island makes hats. Having little tillable land, this pueblo is one of the most specialized home-industry towns in the Tarascan area. 66 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7 trensas. In practically every Tarascan pueblo women, children, and sometimes men weave trensas in their spare time, while walking to and from market, and while herding sheep. Braids are sold in the main markets, where they are purchased by hat makers. Little wheat straw is now braided, palm leaf being more durable and more easily handled.” After they are pressed and straightened with wooden rollers (fashioned like a clothes wringer), the braids are sewed together in spiral form, beginning at the crown. The brim and crown are made separately and sewed together. In JarAécuaro wooden forms are used to block crowns. Most hatters employ a Singer sewing machine, but those of Urapicho, Pamatécuaro, and Zacén sew by hand. In some towns hat making is disappearing, owing largely to factory competition. Pich&taro, formerly an important hat town, now has but four hatters. In 1936 the industry disappeared completely in Tirindaro. Tule weaving.—The indigenous sleeping mat or petate (k‘uirakua) is found in most of highland Mexico. Also, the fire fan or soplador (p‘unita- tardkua), an indispensable kitchen utensil, is woven of tule. Mats and fire fans are made wherever tule is available—along the shores of shallow lakes, marshy areas, and river banks. Consequently, the villagers living around Lake Patzcuaro are the chief tule weavers in the present Tarascan area (map 20; pl. 12). In San Andrés 90 percent of the werking population make petates. Even a few families in the Sierra towns of Pichaétaro and Cherdn fabricate mats from tule reeds imported from Erongaricuaro. Formerly the towns near the northern march districts were important petate producers, but there the industry has greatly declined with the desiccation of wet areas and disappearance of the tule brakes.“8 Tule is likewise being depleted along the shores of Lake Pitzcuaro. The peta- teros of Pudcuaro, Napizaro, and Uricho import reeds from Jardcuaro Island, the local supply having been exhausted years ago. Tule reeds are cut with the sickle, semidried, and bundled for transport or storage (pl. 8). In 447 Hats of wheat straw are now made only in Pamataécuaro, Teremedo, and Apo (mestizo). 148 A few petates are still made in Tarascan Tarejero, on the border of the former Zacapu marshes; in mestizo Ettcuaro (Tangancicuaro Basin); and in TacAtzcuaro (near the Cotija graben lakes). Moreover, the industry is still carried on in some of the Lerma Delta towns east of Lake Chapala, and in a few villages around Lake Cuitzeo. the Lake area a twilled technique is used in mat making, which is performed on the ground, the only tools being a knife or sharp stone to cut tule stalks and a wooden mallet to flatten the reeds as they are twilled. Several sizes of mats are made; the largest, called simply k‘ufrakua-k‘éri, meas- ures 1.5 by 1 m.“° Both mats and fire fans are taken to the Lake markets (Patzcuaro, Erongari- cuaro, Quiroga), where they are purchased by the Sierra people and buyers from the tierra caliente. Basketry.—Ihuatzio and San Jerénimo in the Lake area are the only modern Tarascan towns in which baskets are made. The former Tarascan towns of Tangamandapio (west of Zamora) and Panindicuaro (north of Zacapu) are the main basket centers in the general area, supplying the Sierra people with the Sindiéa, or harvest baskets for maize. The Ihuatzio baskets are made of split carrizo stalks, which grow in abundance in local house lots. Both wicker and twilling tech- niques are used (pl. 12). Netting.—In all fishing villages around Lake P&tzcuaro nets are made by men, women, and children in their spare time. On Janitzio and the Urandén Islands a few professional rederos fabri- cate nets to sell to fishers in other pueblos. Cotton thread purchased in P&tzcuaro is wound on the hilador (Soréranskua) and five to six strands are twisted with the native malacate or with the European spinning wheel. The twisted strands are water-soaked and sun-dried. Nets are made with the éurikua, a large wooden needle (20 cm. long, 2 em. wide). Capote making.—In many parts of indigenous Mexico the palm-leaf raincape (capote), similar to those worn in the Orient, is a common outdoor apparel during the wet season. Capotes are made by women in three Tarascan towns—Quinceo, Arantepacua, and Turicuaro—using leaves of the palma pimu (Acoelorraphe pimo), which are im- ported from the tierra caliente below Ario de Rosales..° The capes are fabricated by tying soaked strips of palm leaf onto braided cords, two of which are stretched parallel and one foot apart on pegs driven into the ground. The strips of 140 Other types: The k‘amériéa (1.3 m.X80 em.) and the ¢im4nitepémueta (1 m.X50 em.), both used for sleeping; the jatapetakua, a small knee mat; idstitan, a long, narrow mat sold to mestizos as a sort of rug. Many more sizes and varieties occur, the names and types varying from place to place. The terms and types given above were observed in Ihuatzio and some of the ranchos along the shore of the Taasfu-k‘éri Peninsula. 180 Most of the palm leaves used in Arantepacua are said to come from the localities of Rosario, La Playa, Charapendo, and San Marcos, south of Ario, 102°30' 102° 30' fal torecvoto aA Patamban & co} a) Sirf W106 a © Tingiiindin af Lon Pamatdcuaro Sicuicho,, Charapan a> Corupo 0% ites Reyes poi Se ie ) oZirosto ©Peribdn Pottery Clay Figurines Cotton fabrics (belt loom) Woolen blankets (hand loom) 102° 30! @angahuan Etdcuaro Santo Tomas Chilchota BSS 2-0, O° 5°@O Huansito @san José G ©0cumicho io) Tanaco Cocucho @ Gheranasticurin Urapicho, 2 BI ae } ba a ge aI Aa OAranza @O,Nahuatzen no" AC uapon Nurio, Giga 40 iA gesen Felipe (8 sevina er i Arantepacua al dk we . 0 é Turicuaro nal Gumachuén Britis San Lone Tingambato,, oan Angel bo Conejos “° Guet 6 © Ziracuaretiro 2 Hats Mf Capotes a Agave fiber articles Pare Fish nets 4 Petates 8 Baskets A | ? i Turned woodwork Furniture Ironwork Map 20.—Distribution of handicrafts in the Modern Tarascan area. of” Ave whnann bateas) GF musica instruments Leather products CoenevO) olarejero od Teremendo 0 ° Zipiajo Santo Fé San Jerénimol® Ne San André = ves *o ory Forlowios Le a a 5 filg Teinizunfzon Puscuarolt) Erongoricuoro®— OB ea B° JanitzioxA \ 5 Cucuchucho ° \ A WA Jordcuar eel So ( ae Patzcuaro ‘o Zirahuén Ch. eee Santa Clora® 0 96 over CTF Copper products Stonework (metates, etc:) Settlement in wi 20% sy of k opulation eng wong eapaoted (large symbols) Settlement in which less than 20% of working pe engages 10 { Brooms ki atts = 71°30) 748988 O - 48 (Face p. 66) tw ¢ the ofounasol a iy f Mani on azul NOC gy, | * ny —~ : Y oie &, nodmopt = _f | " iba ca Tend sents ‘ 0 gee oe Ol ahh My i ‘4 von i, ¢ Da iv a. Pie : J f 4 ' t Ds i “ 5 | : coctpareanaia ) APLC OeAaudeo orned noe au | | 7 ; ed * y bid 4" hel \ hy onviqant ony cen Oieoeromed || Wek Wi Let Peseak ro) Garr pie 1} dishes eT a ? os F ) oy : ee. by BOhoriuna 0 AGH Dy 6 he ; a tel hy Letslusia D3ne% ol bie é cen : Ho a) bal Gyan? . So jokes *h \ .- eA hud 6 af \ © Page i ‘ Pil y On DOF i i qi “a meet sug? | a ‘be 8 aes ongatnai a Rt = On na brsas 4 Weta _ = # 4 Ps eS ea ; noso5 Se Ii ee (a ude x 4 ; 0% ada leicht 40" bxerai m OMA acne SaaS ~ bis , nourtogan' OOK DDGay i "s eB! Ge atari Se ff} Je < ard pay me * 4 qanvate, Fe nan Seyi * \ f ka 0) amt } ;° Sibodiieds aistnosNo SOnBtatt 7 ” finn . 7s ied eu ts we fi ie ee af j ne { et rere ee | ENT SRO eal ee NEN, vectra Sule sige rece nuc ? “a 4 dat pide Sans po aera 9407 ‘evop A, ad WO wats OF eatogod) (Mes uinierts ator nerd imamaparh Leet eine, afer zeaiwuel fold as : etil He that peat BO OF ! diowbbow ibeatut- 4 ees zatbted Gi pote tion oe ayia OF / er Sai Gan ies fotee La jas re POD eres aes Oe uprated, es uprated, NE th et ees wile ale Psat Senin Same repcan nee armen nN calendar cy Sane Be MO @auittawai (, , Broom elgden dy. @s os Ties — ‘wih mi SMewibaedbde coitudinieiG— oe aAM Mea ihthal pid caiadiie 1 be Oinee oben Xf Sy eateath CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—-WEST 67 palm are tied on one cord, half-hitched to the second one, and then tied back to the first; the loose end of the strip is permitted to hang over the second cord, thus forming a drainage surface similar to thatch (pl. 12). The process is re- peated, adding a new row of tied strips to the prev- ious one until the garment (4 ft. long and 3 ft. wide) is completed. Arantepacua capotes are marketed as far north as Guanajuato. No men- tion is made of these raincapes in the colonial sources, nor is there a Tarascan word for the gar- ment. It is not improbable that the capote is an introduced trait. Broommaking.—This is another minor industry now practiced by a few men in Arantepacua. Pimu palm leaves are symmetrically arranged around the end of a finished pine stick and then tied with agave fiber or a braided strip of palm. The result is a common broom found in all parts of central Mexico. WOODCRAFT According to the early Spanish chroniclers, the Tarascans were clever craftsmen in wood, and under the instruction of Spanish masters the natives became among the best carpenters in New Spain (La Rea, 1945, p. 20; Escobar, 1924, p. 147). By 1580 Indian carpenters in at least four towns—Pitzcuaro, Necotlin (Undameo), Tiripitio, and Tingiiindin—were turning out European-styled tables, chairs, and writing desks, which found ready sale among Spanish colonists in all parts of Michoacén.%= At that time lathework was established in Paitzcuaro, and probably before 1540 Tarascans had begun to carve saddle frames for Spanish horsemen (Molotinia, 1903, p. 183). Like other Tarascan industries, woodwork was probably a rudimentary pre-Conquest craft greatly modified and improved by European techniques. However, the present commercial types of Taras- can woodwork—cabinet work, lathe work, and adz work—all appear to have been developed in the 16th century. Specialized woodwork (apart from lumbering and shake making) was formerly more widespread among Tarascans than at present. At the end of the 18th century wood objects were manufactured in 21 pueblos (AGN Historia, vol. 73), today in only 13 towns. In but eight of the latter is the “tia Rel. de PAtzcuaro, 1581 (Martinez, 1889, p. 47); Mus. Nac., leg. 102: Rel. de Chocandiran, Rel. de Necotlin; Rel. de Tiripitio, ms. (in Garcia Library, Univ. of Texas). industry more than 150 years old; in only five of the present towns do more than 25 percent of the working population engage in woodwork. Adz work.—This is the simplest of the wood techniques now practiced by Tarascans (and by other Indian groups, as well as by mestizos in many parts of Mexico). Before the Conquest the Indians shaped boats from a single log and carved delicate figures on throwing sticks and tom-toms, possibly using obsidian and copper cutting tools. With the introduction of the European steel adz and gouge early in the 16th century, native wood carving was greatly facili- tated. One of the earliest European objects which the Tarascans carved with the adz was the saddle frame (fuste), an industry which disap- peared 100 years ago. Today wooden spoons and bowls (bateas) of softwoods are the principal adz and gouge products, Pamatdcuaro and its offspring settlements Sirio and San Benito being the chief producers.! These objects are also made in the Tarascan villages of Turicuaro, Cumachuén, Pichataro, Zirosto (formerly impor- tant) and Sevina (where the industry was intro- duced a few years ago), and in the mestizo towns of Patzcuaro, Técuaro, Zirahuén, Uruapan, Qui- roga. Spoons and bowls are made from softwoods: jaboneillo (Sa4pu), palo blano (urapit-tku), and aile (pamu). Occasionally bateas are made of pine. Tools include the common adz and vari- ously shaped gouges, which are driven with a wooden mallet (pl. 13). The products of Pama- tacuaro and surrounding settlements are marketed in all parts of Michoacan and sometimes are taken as far as Guadalajara and Mexico City. Lathe work.—This represents one of the most characteristic forms of modern Tarascan wood- craft, Paracho being the center of the torneros. Formerly the simple bow lathe was employed to make bowls, vases, candlesticks, chocolate beaters (molinillos), chessmen, toys (tops, yoyos), darning eggs, etc. (See Beals, 1946, p. 43, for illustration of bow lathe.) Since 1942, however, when a power line was constructed near the town, most of the bows have been replaced by electrically powered lathes. About six torneros in Paracho and five in neighboring Ahuiran still use the bow. Formerly turned objects, chiefly rosaries, choco- 151 It is doubtful that wooden bateas were carved before the Spanish Con- quest. Gourds of Crescentia alata probably functioned for the modern batea. The “‘bateas’’? employed in early Spanish gold placering in the téerra caliente were likely fashioned from Crescentia gourds. 68 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7 late beaters, and malacates, were made in Charapan and Cocucho, but this activity has now disap- peared. Most of the turned objects are shaped from madrofo wood (pandyksa). Carving is done by pressing variously shaped steel chisels and gouges against the whirling block of wood. In Paracho, designs are painted and burned into objects, and the surface lacquered or varnished. The wheel lathe, an early Spanish introduction, is used by most cabinetmakers in the area for turning wood. Cabinet work.—As mentioned earlier, cabinet work was rapidly adopted by Tarascan craftsmen in the early colonial period. In the 17th and 18th centuries inventories of miners’ and merchants’ household goods in west-central and northern Mexico rarely fail to mention chairs, tables, boxes “de Mechoacan.”’ The majority of present Taras- can towns has at least one cabinetmaker who partially satisfies local demand for furniture. In Paracho, Corupo, and Cuanajo—the Tarascan furniture centers—carpenters make chairs, tables, bed frames. Cuanajo is famed for its wooden chests, which are marketed in all parts of Michoa- cin. Most furniture is made from pine wood with simple tools (saw, mallet, plane, chisel, gouge). As mentioned above, chair and table legs are turned on the wheel lathe (fig. 6). The more common jointing techniques used include mor- fp. ES Figure 6.—The wheel lathe, used by most Tarascan cabinetmakers for turning wood. ticing and tenoning, housing, and dovetailing. Some pieces are joined with wooden pegs; metallic nails and screws are never employed. Musical instruments.—The most sophisticated of Tarascan woodwork is the manufacture of stringed instruments in Paracho. This pueblo has been the guitar towr of Mexico since colonial times. In 1940 Paracho claimed 49 guitar makers and three individuals who made violins (including base viols). The art has spread to neighboring Ahufran, where three men made violins in 1946. Local woods—¢irimu, qaile, and palo blanco—are used for the top and base of the guitars; for sides and handles and inlaid designs walnut and cedar are imported from Mexico. Some guitarreros utilize local pine and fir for the tops of violins and base viols. The wood is cut with a small saw and planed to desired thinness. The top and base are cut from a pattern; the side bands are soaked and bent into place, being glued to the top and bottom pieces and held in place with braces. Strings and metal parts are assembled, and the instrument is varnished and waxed, ready for the ultimate consumer. Most guitarreros work on a contract basis for Mexico City or Guadalajara buyers, and many Tarascans have moved their trade to the larger towns, mainly Mexico City, where their products bring higher prices. The age of the Paracho guitar work is not known. The wheel ranges from 2% to 4 feet in diameter and is usually turned by a small boy. CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—-WEST 69 1s first mentioned as an established industry in the report of 1789 (AGN Historia, vol. 73, f. 344), indicating that it had been introduced for some time. LACQUER WORK Modern lacquerwork in Michoacén is closely associated with wood carved with the adz and lathe. Before the Spanish Conquest various gourds (Lagenaria, Cucurbita, and Crescentia) were lacquered with a varnish made from the insect axin (Coccus axin) and chia (Salvia sp.) This industry probably centered in the Balsas and Tepalcatepec Basins (Brand, 1944, p. 60) and was extended into the towns near the southern edge of the Sierra, e. g., Peribin and Uruapan. After the introduction of Spanish adz work during the co- lonial period, lacquer was applied to wooden bateas im Peribin, Zirosto, Zacin, Uruapan, and Patz- cuaro. Bateas were painted, but not lacquered, in Cucupao (Quiroga) and Santa Fé de la Laguna. Today few Tarascans practice the art, the famous bateas of Uruapan being lacquered by mestizos. Some of the turned vases and bowls of Paracho are finished with tung oil and synthetic lacquer purchased in mestizo markets. LEATHERCRAFT Probably one of the first native Tarascan crafts stimulated and expanded by the early Spaniards was leatherwork. With the introduction of cattle, Tarascan tanners were able to multiply leather production, which formerly had been based on deerskin, to meet the heavy Spanish demand for saddles, halters, shoes (the famous ‘‘zapatos de baqueta de mechoacdn’’).** Tanning was done with local oak bark, as it is today (AGN Tierras, vol. 83, exped. 13). During the colonial period leather- crafts were centered in the northern Tarascan towns near the pastures and hide supply, and in a few pueblos of the Sierra. The latter included Cheran, Cherandtzicurin, Ocumicho, and Nahuat- zen, which was one of the largest tanning centers 182 Fray Toribio de Molotin{a’s statement of 1540 on the Tarascan leather industry is revealing: ‘‘Han deprendido a cutir corambres . . . son buenos zapateros, que hacen zapatos y servillas [slippers], borceguias [high shoes], pantaflos, chapines [wooden shoes with leather straps] de mugeres; . . . este oficio comenzdé en Michoacan, porque alli se curten los buenos cueros de venados. Hacen todo lo que es menester para una silla ginete bastos y fuste, coraza y sobre- corazas. . .” (Motolinfa, 1903, p. 183). According to the Relacién de Micho- acdn (p. 16) “‘cotares de cuero,”’ or leather sandals, were made for the caltzontzin in pre-Conquest times. in the Tarascan area.’ By the latter part of the 19th century leathererafts began to decline, and today within the Tarascan area only Nahuatzen (largely mestizo) continues to tan hides and make saddles and other riding equipment. Some Tarascan towns now boast of one or two zapateros who make huaraches of imported leather for local consumption. The principal huarache-making centers are now the surrounding mestizo towns: Coeneo, Zacapu, Tinguindin, Los Reyes, Uruapan, Ario de Rosales. METALCRAFT Copper work.—The Tarascans were probably the foremost metallurgists in pre-Columbian Mexico. They worked gold, silver, and copper. The precious metals were formed into ornaments and disks, which the caitzontzin stored on the islands in Lake Patzcuaro; useful objects, such as axes, coas, and spearheads, were made of copper (Relacién de Michoacdén, pp. 104-109, 122-123). Although definite archeological evi- dence is not yet at hand, it is probable that the Tarascans purified native copper and extracted metal from simple oxide ores by smelting (Hend- richs, 1940, p. 327). From cursory inspection of copper artifacts extant in the Museo Regional Michoacano, Morelia, it appears that Tarascans cast copper objects (axheads) in stone molds. After casting, the axes seem to have been further shaped and possibly hardened by hammering.'*® Accidental, rather than deliberate, alloying with tin and zine probably occurred. The Tepalcatepec and Balsas Basins contained the ancient copper mines and metallurgical sites. Hendrichs (1940, 1945-46) has described several probable ancient copper mines sites in both the 18 AGN Tierras, vol. 83, exped. 13; Zavala and Castello, 1939-46, vol. 7, pp. 361-362; AGN Historia, vol. 73, ff. 178-179. The present northern Taras- can towns of Zipiajo, Azajo, Companja, Tatejero, Tirindaro, Naranja, and Teremendo were all producers of shoes and saddles in the latter part of the 18th and in the 19th century. 184 Beals (1946, p. 44) states that in 1940 one person from Aranza was tanning hides in Cherin. The old men of Ocumicho remember the manufacture of the black “‘zapatos de raquetas’”’ in their town during the last century. These were sold throughout the Sierra as well as in surrounding mestizo towns. 185 The Lienzo de Jucutacato, a 16th-century representation of the migra- tion of a people from the Gulf of Mexico into the Tarascan country (where they learned metallurgy) clearly depicts smelting of ore or metal (probably copper) apparently with the aid of charcoal and forced air draft (blowpipes) at the ancient copper center of Jicalén (Jicalin Viejo), 20 km. south of Urua- pan. 18 Microanalysis of Tarascan copperware has not yet been undertaken. Until the results of such analyses are known, it is impossible to make definite statements as to ancient metallurgical methods. Interestingly, the flange shape of the modern Tarascan steel axhead is identical with that of the copper axes found in archeological sites in the Balsas Basin. 70 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO. 7 southern and northern drainages of the lower Balsas (Guerrero). However, the mines of Inguardn in the northern drainage of the lower Balsas in Michoacdin were the main source of the metal. Smaller deposits, such as those of Sinagua, were gophered over a wide area. The villages of La Huacana, Jicalin, Sinagua, and possibly Tzatzio appear to have been the chief pre-Colum- bian copper refining centers.'” Needing copper for the manufacture of brass cannon, the Spaniards quickly levied tribute in copper bars on various pueblos in the Balsas and Tepalcatepec Basins. Later, adventurers (in the name of the Crown) took over the native mines at Inguard4n, probably introducing European smelting techniques. The main 16th-century Spanish smelting and refining center was Tzatzio, 10 miles each of Ario. This center was located within pine and oak forests, which afforded raw materials for charcoal, and was near the chief highway from P&tzcuaro to the tierra caliente. Copper ore and probably native copper was car- ried by Indians to Tzatzio from the Inguardn mines, which lay 15 miles to the south (AGN General de Parte, vol. 5, ff. 311-313, 1601). Tzatzio was probably an ancient copper center, and the experienced Tarascan metallurgists were retained by the Spaniards to continue with Euro- pean methods. Before the end of the 16th century the Spanish Crown had established an asiento in the Michoacéin copper industry, in order to insure a steady supply of metal for the foun- daries in Mexico City.! Between 1607 and 1614 187 The Suma de Visitas, ca. 1540, state that the Spaniards exacted tribute of copper bars from La Huacana and Jicalén (Paso y Troncoso, 1905, vol. 1, pp. 123, 294). Moreover, every 20 days 20 Indians of Coyuca carried copper bars to Mexico (ibid., p. 80). Coyuca, located near the confluence of the Balsas and Cutzamala Rivers, may have been a collecting point for small lots of copper refined in various pueblos of the middle Balsas drainage. At the end of the 16th century copper was still being mined, refined, and made into tools at Sinagua (Mus. Nac., leg. 102, Rel. de Cinguacingo). Tzatzio was one of the first Spanish copper smelting centers in the area, and was probably an old Tarascan center as well (AGI Aud. de México, leg. 258). In passing, it should be noted that the old La Huacana was located near the Inguar4n mines. In 1759 the town was destroyed by the eruption of Jorullo, and a new settlement, the La Huacana seen on modern maps, was established near Tamacuaro 15 miles west of the old site (AGN Historia, vol. 73, ff. 392-394) 188 Under the asiento, or contract, system, control of various industries was farmed out to private individuals. In the ease of the copper industry of Michoacin, administrative control was purchased from the Crown for 6-year periods. The administrator was obliged to furnish the Government a stipu- lated amount of copper annually at a fixed price. In 1599 an official survey was made of the copper industry in Michoacin. The surveyor recommended that owing to forest depletion around Tzatzio and the consequent difficulty in charcoal supply, refining operations should be moved to Ario, near abun- dant pine forests (AGI Aud. de Mexico, leg. 258). It is doubtful that this move was made, since in 1607 copper was still being refined at Tzatzio (Zavala and Castello, 1939-46, vol. 6, p. 166). official copper refining operations had shifted 20 miles northward to Santa Clara (Villa Escalante), which has remained the copper center of Michoa- cin to this day (AGN Mineria, vol. 22, exped. 3). In addition to copper bars for the royal artillery, the colonial administrators established the manu- facture of caldrons and other copper vessels, which they sold to all parts of New Spain (AGN Historia, vol. 73, ff. 389).1 Colonial copper production, however, was not limited to the royal refineries at Santa Clara, for as late as 1789 braziers were still being made by native copper- smiths at Jicalén (AGN Historia, vol. 73, f. 366). Moreover, some copperwork was done in Pa&tz- cuaro throughout the colonial period.! Today the sole survivors of the former Tarascan copper industry are some 30 mestizo copper- smiths in Santa Clara, where the renowned casos (caldrons), vases, and bowls are still manufac- tured. Ore or native copper is no longer refined; instead, scrap copper is purchased, melted down, and cast in earthen molds. Sixteenth-century hand bellows are still used to force an air draft; charcoal is employed for fuel. The cast vessel is finished and hardened by alternate annealing and hammering. Ironworking.—With its concomitant tools (bel- lows, hammers, anvils, tongs, etc.), ironworking was introduced into Tarascan economy early in the 16th century. Curiously, one Sierra village, San Felipe de los Herreros, became the foremost ironworking center of Michoacén during the colonial period and the early 19th century. In 1644 bridle bits, spurs, locks and keys were fashioned and marketed in surrounding Spanish and mestizo towns (Basalenque, 1886, vol. 1, p. 467). As late as 1851, 68 families (practically the entire town) were professional smiths, supply- ing the countryside with plow tips, hoe blades, axheads, woodworking tools, etc. In 1946 three 169 During the 17th century Tarascans from all parts of Michoacin were forced to work in the Inguara4n mines and the fwndiciones at Santa Clara. Most of the fundidores came from the tierra caliente and from the tierra fria towns of Zirosto and Patzcuaro (Zavala and Castello, 1939-46, vol. 6, p. 166; vol. 7, p. 240). In 1789 there were 8 copper refineries at Santa Clara, each operated by 30 to 40 men (AGN Historia, vol. 73, f. 389). 160 The Relacién de Patzcuaro of 1581 (p. 47) mentions “‘herreros y calderos.”” Basalenque (1886, vol. 1, p. 451), writing in 1644, states that copper bells were made in Patzcuaro. As late as 1862 (Romero (1862, p. 7) writes of PAtzcuaro coppersmiths, who were refining ore from Inguarén and Churumuco. Several new copper deposits in Michoacan were exploited during the last quarter of the 18th century, e. g., the mines of Apupato, near the old site of Urecho (AGN Historia, vol. 73, f. 888) and those of Chirangangueo, near Tusantla, south of Zitacuaro (AGN Mineria, vol. 62, exped. 1; Martinez de Lejarza, 1824, p. 92). CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—-WEST al old smiths, who work at their trade only part time, represented the remnant of a once thriving home industry. The former source of metal for the San Felipe smiths is problematical. According to a local informant, during the 1880’s ‘“‘planchas de hierro”’ were brought in from Cotija, a muleteer and trade center having close connections with the tierra caliente and the Sierra of Guerrero. This infor- mation points to Coalcomén in the Sierra Madre del Sur of Guerrero as the principal source of iron. Other ironworking towns of Michoacan include Irimbo and Nahuatzen. Mestizos in the latter pueblo fashion knives and machetes. STONECUTTING Stonework among modern Tarascans is limited to approximately 12 metate makers in Turfcuaro. Formerly this village was noted throughout Michoacdn for the high-quality metates (iaudn), manos (poaékua), and molcajetes (Stiimatakua) carved from a fine-grained andesite (¢akaépu amiakiti, or “good stone”), found near the summit of the composite voleano Kandkuarani (Cerro de la Corona) nearby. Since the introduction (ca. 1925) of the engine-powered nixtamal mills in mestizo and larger indigenous towns, demand tor new metates has sharply declined.!® Metates and molcajetes are roughly shaped at the quarry on Kandkuardni and are carried down to the pueblo on burro for finishing in the stone- cutter’s house. Stone is worked with steel tools, e. g. the pick (pikua) and sledge hammer (pikua- k‘éri), and is finished with a polishing stone (jand- mu). Several sizes of metates are made and sold to traveling merchants who pass through the town. TRADE AND TRANSPORT The structure of trade among the Tarascans is not dissimilar to that of most Indian groups of central Mexico. Although every settlement has at least one store where general merchandise can be purchased, most trading is done at the tianguis, or market, held regularly in the larger towns. Throughout the area professional traders—huaca- leros (who carry merchandise on their backs), arrieros (who haul products on the backs of burros), and lately, wholesale buyers from the 16t According to local informants, in 1912 practically every family in the village made metates. Since that time most of the villagers have turned to woodwork (mainly bateas). large mestizo towns (who ride in trucks and busses) —all serve as distributing agents. The market (uasajpikuagu, or ‘‘the place where people sit’’).—Sunday is the most important market day for the Tarascans.'” Large groups of Indians from neighboring pueblos flock to the regular markets held in the large mestizo towns within or on the edge of the Tarascan area. Since colonial times Paracho has been the largest Indian commercial center of the Sierra. To the south Los Reyes and Uruapan are the exchange centers for tierra caliente and tierra fria mer- chandise."* A lesser number of Indians attend the northern market towns: Zamora, Tingiiindin, Purépero, Zacapu, and Chilchota (the commercial center for the La Cafada pueblos). Generally speaking, each large Sunday market draws upon a certain Indian area defined by a walking or riding distance of one day or less (map 21). On occasion, however, the Pétzcuaro or Uruapan tianguis is visited by Indians who live more than 1 day’s travel away. In the Sierra often the entire family attends the regular market, leaving Saturday with handicrafts or farm products (usually fruit, chickens, or eggs) packed on burros, and arriving at the plaza at night.!* Sunday morning is a time of brisk trading. By afternoon most of the traders have sold their wares, purchased supplies, and have departed for their respective pueblos. The Lake Patzcuaro fishers got to market in boats, carrying fish and vegetables to Patzcuaro, Erongaricuaro, and Quiroga to trade for maize, wheat, and firewood. Lesser markets are regularly held in a few smaller Indian towns. For example, there is a Sunday market at Charapan, attended by people from Cocucho, Urapicho, Corupo, San Felipe, and Nurio. On Saturdays and Mondays there is some commercial activity in Cheran, as professional traders pass tbrough the town going to and coming from the Sunday Uruapan market (Beals, 1946, p. 80). Again, on Thursdays 182 An important exception is the Pétzcuaro market held on Fridays and Sundays. A minor fish market occurs also on Tuesdays. 163 Formerly Peribin was one of the largest tierra caliente—tierra fria markets in Michoacan, but since the close of the colonial era it has ceded most of its trade to Los Reyesnearby. Important fiesta markets are still held in Periban however. 164 Within the last 8 years the pueblos along the Uruapan highway have ridden busses or taxis to market. Since 1943 similar transport has been extended to Charapan, Zirosto, and intermediate pueblos. Moreover, during the dry season lumber trucks haul loads of men and women from some Sierra towns to mestizo markets. 7 INSTITUTE OF SOCIAL ANTHROPOLOGY—PUBLICATION NO 72 *po}BOIPUL JOU OIB SJoyIVU UTBUL dy} 07 ATE{NqIIy SUMO} UBOSIBT,-UOT Auvpy ‘sjoyIBw Juasoidas souty}NO UMOY PUB SopOIIO Yul “BoB UBOSLAV, ULOpOUT oY} UL A1O}PI19} SUIpCIy [BOO] Ifoy} pus syoxIVU Jo UOTNGIIySIG—'[Z AVI TAG a eee Ss ae SSS SS ETE wy 02 o1 s ° u0jas044 Ww O2 ol Ss ° ze) s “01019 oyUDS oadodo? ¢ Sy oujasono0s17 O oO. 0 0/809 507 ‘ 1 ne uUlzZUOZ OD | eet Updoniq ={ ody Q\. : vanyouz Oy jabuy us? \\ ! \ \ ! \ . olounng ! 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Se / th : ae T o03ua0c9 ovalasoy ; ua SOx., il y ' , OyONras0) ! oyoyr|iug ‘/ P II [fe ; DIOWDZ vm ermeeere pboung -—-— t 1 ; oupnoiogupbuo, ——--— OLONDZ1O dl sercesoc— ise .--- DJOYD|!4D OLDNDIZOB VOID evvsesseraeeee ouono1ouobuoy Ousdaing Oyd0J0g —----- ouadaung ndDIDZ --..- cues uodonsy) ———— 0aua0d0 —=|j—— sokay SOF —-—-— seme O “Sjuawaljjas o1dopuowobuo, | Aaoyngis4y puo sidjuad jyaxsow yoeuu0d saulq \ o10wo 10? “oe 10) = 7201 CULTURAL GEOGRAPHY OF THE MODERN TARASCAN AREA—WEST 13 professional traders gather at Patamban to buy pottery for the various Sunday markets. Besides the regular weekly markets, in practi- eally every village lively trading accompanies the annual religious or semi-religious celebrations. In some instances such markets are large enough to be termed fairs. Commercially, the most im- portant of the annual fiestas is the pueblo’s saint’s day, attended by traders and villagers from miles around. Other fiesta markets occur during the Corpus Christi, Easter, and Christmas celebra- tions. Often a particular village, such as San Juan Parangaricutiro, holds special religious (and commercial) festivals to honor a special saint or miraculous event.!® Trading in the market is done mainly on a monetary basis. Little outright bartering takes place. An interesting exception occurs at Erong- aricuaro, where wives of fishermen exchange baskets of fresh or dried fish for piles of firewood carried in from the Sierra. Another instance of barter takes place at the Patamban market; there, women from the Pamatdcuaro ranchos trade tamales for pottery and fruit. The market takes place in the town plaza, and when the number of traders is exceptionally large, some sellers are crowded off into adjoining streets. Each vendor pays the municipal authorities the piso de plaza, or tax for the use of a small selling space on the sidewalk. By custom, stalls are segregated according to the type of article sold, pottery being dispensed in one section of the plaza, foods in another, etc. (pl. 14). (See illustration of Chilchota market in Beals, 1946, p. 84.) Ex- cept in special markets, such as Patamban, the number of merchants of fruit and vegetables ex- ceeds all others. (See Beals, 1946, p.82.) More- over, in the large towns professional mestizo vendors of factory-made clothing, hardware, ete. are numerous, while the Indians selling handicrafts are relatively few. The P&tzcuaro, Erongarf- cuaro, and Paracho markets, on the other hand, are composed of a much larger percentage of native traders. The village stores.—Almost without exception every Tarascan village boasts of at least one store 165 Of interest are the Palm Sunday (Ramos) fairs held in Periban, Zamora, Uruapan, and Patzcuaro. Exchange of tierra caliente and tierra fria products is particularly significant at these markets. 166 At the Ramos fair at Periban (April 14, 1946) at least three-quarters of the selling space was occupied by tropical fruit vendors and sellers of factory- which handles mainly staple food imports (salted dried beef, dried fish, salt, piloncillo, lard, beans, and wheat flour) and beverages (soft drinks, beer, and hard liquors). A small assortment of canned goods can be purchased in the stores of the larger towns. Often other items, such as cigarettes, kerosene, and metal household ware, are carried. In the small villages stores are customarily oper- ated by well-to-do Tarascan families, often by the wife and children, while the man farms.'*” In the large pueblos the storekeepers are usually mestizos who have moved in from neighboring towns.!® Significantly, the infiltration of Spanish-speaking storekeepers into indigenous towns often repre- sents one of the initial steps toward hispaniciza- tion of the native population.!” The professional traders.—The huacalero (in- spikuuiri, or ‘‘one who trades”) represents the last vestige of the ancient Indian carriers (tamemes), formerly important agents of distribution throvgh- out Mexico. Few such traveling merchants, each of whom carries his wares in a wooden crate (huacal, képartakua) tied to his back, remain; the majority have been displaced by burro and motor transportation. As late as 1900 large numbers of Tarascan huacaleros from many Sierra villages carried handicrafts into the Balsas Basin, the coast of Guerrero, and Colima and returned with tropical fruit, salt, and cheese. Today about 15 huacaleros operate out of Pama- tacuaro, carrying locally made wooden spoons and bateas, Patamban pottery, morrales from made goods from Zamora, Guadalajara, Morelia, and México. Regional handicrafts were represented as follows: Article: Origin Vendors (number) Blankets 222-2 2222 --5-- Gharapan=<_ 27 - ssssae- 10 walking vendors. BlanketSis-ss-------=- PAQUIN SNe se aeeaeeeee a= 1 stall. Rebosos: ss. sass 4235 Paracho 1 stall Women’s belts__--_---- Nahuatzen_--- 1 stall Strew. hats: 2-:__=-.-<:- IADOs -222c8-s5- Cr ne ge ere 4 fie FE igi et, wae eee OT gaa Pr . - Wich ite 7 ' ea ‘a 7 == ': rte" Sire Wie o> Hi MPs ey ot?) 1 ay an ' 7 = Pp - STi soe ae it i Rs ve Pay an Nie : . Irby ST bya tema ase | \ SO ‘ a : 7 | . - 2 POO TGATR Fire! zy witee'l rit rue a | rm Ws ieee ay st yy a LP er ee en ed . int poe « idle AL the Ah: Brat . : : a. iyi | : 7 yr mm? Hi ayy aS = »* oe iatA~ - - z ; 7! < = "liar a + eins eh oF ; a . i a : ’ ee se 6.) pea ; Mari ib a4 = ary ea See, hi ’ lad L > ate ( . - oad : 7 = 7 x jy} ; rs ra Lys a e y j ae ne any, Weer me 7 , iy fj it f *) gh Bs a 4 7 . : Lé é ‘i ; i a eh 3 ty aN SG! ea ‘ , 7 le ah? ve tb Mts ; oa ea 2 ~ o ‘ a : ' 7 : i : Aare = | ee i ¢ x ; § ey pe rr : : —— a om - « 2 ian = oe Ue his _ 2 Py. i! = 7 7 . = ss Te > mie 7 e ay = ’ > io ; ta 7 ; ans Oe - i! im - § = - ; ; : F) oft ty if a : : on: - ¥ ' . — \ : 2 ~ - i 4 a : ; : ' we i ‘ SPT Sere Rie PLATE 1.—Physical landscape. a, Portion of a Sierra basin near Arantepacua. 6, Southwestern part of Lake Patzcuaro; Jaracuaro Island and newly formed Pastora Island, upper center. c, Cultivated floor of cinder cone crater near Charapan. d, Lake Patzcuaro, looking northward; note voleanic islands in middle of lake and the Urandén Islets immediately off shore. e, Mixed pine-oak forest at edge of maize field, Char apan. f, La Canada, looking westward, or down valley. PLATE 2.—Water supply and settlement. a, Wooden aqueduct at Pamatacuaro, which brings water from the local spring (center) to the outskirts of town. », Hoisting water from one ofthe public wellsin Charapan. c, Street in Ihuatzio, Lake Patzcuaro. d, Panorama of San Jeronimo on Lake Patzcuaro, show- ing compact assemblage of adobe structures. e, Partial view of Zacdn near Paricutin Voleano (background), showing grid street pattern, scattered dwellings, and large lots. f, Los Conejos (San Juan Nuevo), founded in 1944 to house refugees from destroyed San Juan Parangaricutiro. Nearly all trojes were trans- ported from old San Juan and reassembled on the new site. g, Street scene, Charapan (Sierra). h, Street scene, Tirindaro, Zacapu Basin. i, Plaza at Charapan PLATE 3.—House types. a, Front view of troje from inside house lot, Quinceo. b, Back view of troje from the street, Sicuicho. Notethe plank wall (¢ar¢éakata) to left of house. c, Elaborately carved door, Charapan. d, Planks housed in L-shaped cornerpiece, Cuanajo. e, Notched plank ladder leading to lofto troje, Charapan. f, Roofed gate, Sicuicho. g, Trojes at Pamatacuaro. Note rail fences. =~ PLATE 4.—House types. a, Old log struc ture, Zacin. 6, Old wooden troje, Tirindaro. c, Adobe house at Apo. The floor plan and roof are similar to those of the plank troje. d, Wooden house at Caltzontzin, the refugee pueblo east of Uruapan. These new structures are North American n appearance, e, Abandoned adobe two-shed house, San Jeronimo, f, Street scene, San Jeronimo. The house at left with the high verandalike front is often seen in Lake Patzcuaro towns. —Maize culture. a, The Egyptian plow, still widely used in Mexico (Nurio). Note straight steel tip (reja) which slips over endpiece of plow yoke and goad near end of tongue; leather strap used to fasten yoke to horns of oxen. 6, Planting maize near Caltzontzin. The first plow, which opens the furrow, is followed by two small boys, who drop seeds at regular intervals. The second plow covers the seeds. c, Contour plowing near Cuanajo. Field of youngmaize. d, Hillof maize and beansin hoe land near Chilchota. Plants are about 1 week old. Newly burned desmonte near Apo. Note wood ash, which will be mixed with underlying soil. f, Platform on which maize fodder (rastrojo) is stored, An PLATE 6.—Wheat culture. a, Irrigated wheat fields near Chilcota, La Cafiada. 6, Temporal wheat fields on the northern edge of the Sierra, near Tirindaro. ec, Method of hauling wheat bundles to the threshing floor, Apo. d, Cutting wheat with the sickle, near Pichataro. ¢, Threshing wheat with flails, Sirio. f, Threshing wheat in the era with horses, at Comanja. The carreta (right) is used in many parts of Tarasca to haul wheat bundles and maize fodder. Se 2 Peas. ET PLATE 7.—Horticulture and domestic animals. a, Large plowed ekudiu, San Felipe. Note anima]pen adjoining froje. b, Small patch of cabbage in house lot, San Felipe. c, Vines of chayoteineckuaiu, Tanaquillo, La Canada. d, Irrigated vegetable plotsalong west shore of Lake Patzcuaro, near Arocutin. e, Ditch well and palas (t‘aparatarakueca) used to lift water from ditch to irrigate fields. Near Uricho. /, Sheep grazing in harvested maize field, near Tanaco. g,Herding sheep near summit of Cerro de Patamban. The flock is from the rancho of Uringuitiro. h, Bee hivesin house lot, Azajo. cay jnosnp eynregt [[wUs oy ‘G IZ oyeT = 24 ke See E i aed PLATE 9.—Ceramics: Pottery making at Cocucho. a, Vessel being started from’a single daub of clay. The vessel is worked on top of the mouth of a broken olla. 5, and c, Bottom portion of vessel being shaped. d, Piece of clay being rolled out on board. e¢ and f, Sides of vessel are built up by adding pieces of rolled clay. PLATE 10.— Ceramics: Pottery making at Cocucho (continued) gand h, Rolled pieces of clay are worked into sides of vessel. i, Sides of vessel are smoothed with corncob. jand k, Lip of vessel being shaped. /, The finished olla. The vessel was made in about 25 minutes. PLATE 11.—Textiles. a, Weaving cotton cloth for aprons on the native belt loom, Charapan. 6, Weaving women’s belts (fajas), Azajo. The belts vary in width from 114 to3 inches, carry various designs, and each is of several brilliant colors. c, Weaving men’s sashes of white cotton thread, Janitzio, C ari is drying on the petate, lower right. d, Weaving a mor of agave fiber, Tarecuato. e, Stretching woven pieces of agave fiber, Tarecuato. Each piece is doubled over to make a morral. /, Weaving agave fiber on the belt loom, Tarecuato. g, Spinning agave fiber witb the malacate, Tarecuato. 7) Pe A 4 Pisgh en oe i Rie FR Bg aks aia PLATE 12.—Textiles. a, A milpa of tule along the shore of Lake Patzcuaro, between San Jer6énimo and San Andrés. Many petate makers own their own milpas, but sometimes portions of the brakes are leased to tule sellers, who harvest the reeds and distribute them to various villages around the lake. b, Harvesting tule, Jaracuaro Island, Lake Patzeuaro. After partially drying in the sun, the reeds are bundled into manojas and stz 1in shocks. c, Weaving petates, Thuatzio. Note the wooden mallet on the mat near the man’s hands. d, Making capotes, Arantepacua. Work is done je the kichen. Note the hearth, lower left. Palm leaves are kept moist by dipping them in the batea of water at left. e, Embroidering a huipil, or blouse, Tarecuato. f, Baskets woven at Ihuatzio. The large one (left), called @uite, is used to carry bread and fruit. It is usually transported on the back in the ayate. The flat round basket is called ¢‘Akiata and is used to carry fish and tamales. The twilled basket is a tlascal (the Tarascans call it ‘‘tascile’’) for tortillas. The handled basket at the right (simply named ‘‘canasta’’) is for carrying eggs, piloncillo, and often fish. 3.—Woodwork. a, Gouging tools, Pamatacuaro. 6, Wooden spoons and ladles, Pamatacuaro. c, Modern electrically powered lathe shop, Paracho. urned objects made at Paracho. e, Cabinetmaker’s shop in house lot, Corupo. f, Making molinillos with the bow lathe, Paracho. g, Nest of wooden boxes, Cuanajo. h, Small (2 feet high) folding chair commonly made in Cuanajo. i, Bateas made at Sirio. 1 ey wears ao plainer *LATE 14.—Markets and transport. a, The Sunday firewood and fish market, Erongaricuaro. The wood vendor at left has already bartered a pile of pinesticks for a few fish in the basket of burros bringing pimu palm leaves from the tierra , Pottery section of the Sunday market at Uruapan. caliente to Ario de Rosales c, The bread section of the Erongaricuaro market on the plaza. d, A train e, Boats from Janitzio landing on the mud flats at Erongaricuaro for the Sunday market. /, Hauling disassembled chairs and tables from Corupo to the Uruapan market \\ + ' i : ii ' i i ' i i { 1 : i i ' } 1 i — 2 i ' ' : i ’ { ‘ j : ' i i ' i i i ‘ i i a i iy i ' i i ‘ i ‘ * i I : i a i ae : 7 ‘ ya a WT Ta Ina a Sheik. tres lah sat