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OPV THE
COASTAL PLAIN OF NEW JERSEY
WITH
Remarks in Reference to Other Regions
and Kindred Subjects
BY
JOHN GIFFORD, D.Ckc.
FROM THE
Annual Report of the State Geologist of
Bes Jersey for 1899.
TRENTON, N. J.:
MacCreciisuH & Quicitey, State Printers, Opposite Post OFFICE
1900,
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GEOLOGICAL SURVEY OF NEW JERSEY
REPORT ON FORESTRY
Plate No. XVII.
e a
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S haae
The Forestal Conditions
AND
Silvicultural Prospects
OF THE
COASTAL PLAIN OF NEW JERSEY
WITH
Remarks in Reference to Other Regions
and Kindred Subjects
BY
JOHN GIFFORD, D.Céc.
FROM THE
Annual Report of the State Geologist of
New Jersey for 1899.
TRENTON. N. J.:
MacCreciisH & QuiGLey, State Prinrers, Opposite Post OFFICE
1900,
Forestal Conditions and Silvicultural Pros-
pects of the Coastal Plain.
I. General Description.
Although small in area, the State of New Jersey is very varied
in nature.* In the north there are rough, wooded mountainous
regions; in the central portions rich farm lands, and in the south
vast stretches of sandy pine-lands. The average value of im-
proved land in New Jersey is higher than that of any other State
in the Union. ‘The State is without a rival in reference to loca-
tion and transportation facilities. If forestry cannot be practised
with profit in this region, there is little hope for it elsewhere in
eastern America.
The region to which this title refers is located in the south-
eastern portion of the State, less than one hour’s ride by train
from New York and Philadelphia.+ It is irregularly triangular
in shape, and is included between latitudes 4o° 20’ and 38° 55’,
and longitudes 74° and 75° 30’.t It is the northern extremity of
the Atlantic Coastal Plain, which extends southward in vast
stretches of sandy pine and swamp-lands, to the cocoanut groves
and pine-apple fields of Florida. The Coastal Plain of New
Jersey is bounded on the southeast by the Atlantic Ocean, on
the southwest by Delaware Bay, and on the northwest by a com-
paratively thickly populated and productive agricultural region.
The area of this territory is about 2,500 square miles, at least
* The area of New Jersey is 8,224 square miles, with a population in 1895 of 1,672,942. ‘The area of the
Grand Duchy of Baden, an important forest state of the German Empire, is 5,821 square miles, with a
population of 1,657,867. It is considerably smaller than the Kingdom of Belgium, which contains 11,373
square miles, with a population of 6,195,355.
+ The combined population of adjacent cities amounts to more than five millions !
{This region lies in about the latitude of Naples, Constantinople and Northern Japan. Although
South Jersey has the temperature of Northwestern Europe, it enjoys the sunshine of Italy.
(235)
236 GEROLOGICAL SURVEY OF NEW JERSEY.
seventy-five per cent. of which is woods.* It is slightly rolling
in nature, seldom exceeding two hundred feet above the level of
the sea, and is traversed by several navigable rivers + besides
many small streams.
The climate of this region, although close to the ocean, is, in
comparison with that of Western Europe and the Pacific coast,
dry. Our prevailing winds which come from the west are dry.
During the hot, dry days of midsummer even wild bushes often
die. On the other hand, the destructive effects of strong winds,
frost and snow press are very slight.
The East American life zones, each characterized by certain
forms of life, extend westward with exceedingly irregular and
broken borders. ‘There is a transition belt in which the North
and the South more or less overlap. ‘This is the true agri-
cultural part of Eastern North America, where apples, white
potatoes, barley and oats attain their highest development. It
is where the oak, hickory, chestnut, liquidamber, white cedar,
etc., of the south, meet the white pine, maple, beech, birch, hem-
lock, tamarack and arbor-vitae of the north. South of this
transition belt begins the first of the true Southern zones, the
Carolinian, to which the Coastal Plain of New Jersey belongs.
A very large percentage of the Carolinian life zone is forestal.
Owing to its immense size and to the nature of the agricultural
crops which it produces, and for which there is only a limited
demand, a large proportion of this zone is destined to remain in
forest for many years to come. The Boreal and Austral zones
are forestal, the Transition zone agricultural. The eastern part
of the Transition zone, from the Dakotas to the sea, although at
* The term ‘ forest’? is seldom used by woodmen. Good or bad, big trees or bushes, it is all called
““woods,’’ which is a good generic name for such nondescript lands. The word “forst,”” from which
comes ‘‘ forest,’’ is a pure Germanic word, From the earliest times it has been applied however to woods
which have been protected and regulated.
t It is easy to secure an abundance of water in this region, which is a very important feature from a
cultural standpoint. In addition to many streams, a natural copious flow may be obtained from artesian
wells, so that in places irrigation is easy and practical,
} The Coastal Plain of New Jersey is a northern extension of the Carolinian belt into the Transitiou
Zone. It isin reality a part of the South in the North, and as Prof. Merriam says: ‘‘ When such farms
occupy suitable soils in thickly inhabited regions, so their products may be conveniently marketed, they
are of more than ordinary value, for the greater the distance from its area of principal production a crop
can be made to succeed, the higher price it will command. Hence, farms favorably situated in northern
prolongations or islands of southern zones, or vice versa, should be worth considerably more per acre
than those situated within normal parts of the same zones. The obvious reason is that by growing par-
ticular crops at points remote from the usual sources of supply, and at the same time conveniently near
a market, the cost of transportation is greatly reduced and the profit correspondingly increased ”’
REEORI ON HORES TS: 227
present agricultural, was formerly the great white-pine region
of North America. The white pine of the Transition zone and
the short-leaf pine of the Carolinian zone meet on the edge of
the Coastal Plain of New Jersey.
The Carolinian zone is characterized by the short-leaf pine
(Pinus echinata), sassafras, persimmon, liquidamber, magnolia,
white cedar (Chamecyparis thyoides), cardinal bird, opossum,*
grape, English walnut,t sweet potato, etc. On its southern
borders the long-leaf pine (P. Aalustris), the old-field pine
(P. teda),t the bald cypress (Zaxodium distichum) and the
southern magnolias appear. In this zone§ the white cedar
(C. ¢hyotdes) and short-leaf pine (P. echtnzata) reach their
optimum. ||
Throughout the entire mainland of the Coastal Plain of New
Jersey very light sandy soils predominate, although there are
many beds of heavy clay, and ridges of road-gravel, also sand
and clay loams and vast stretches of mucky swamp-lands. ‘The
higher portions of the upland are usually gravelly, the interme-
diate sandy, and the lower, loamy and clayey. ‘The farther
south the richer the soil and of course the thriftier the forest
growth. The gravel is yellow and consists of small water-worn
quartz pebbles mixed with sand and clay. When of the proper
#The oppossum (Didelphys virginiana), about which so much has been written because of its mar-
supial pouch and peculiar habit of feigning death, is arboreal in habit, with hand-like feet and prehensile
tail, and is fond of the fruits of the persimmon tree, the seeds of which it is instrumental in distributing.
It is highly esteemed as food, especially by the negroes of the South.
+ East of the Rocky mountains the Persian walnut has been most successful in a limited area along
the Atlantic coast from New York southward through New Jersey, southeastern Pennsylvania, central
Virginia, North Carolina and Georgia. Farther south it does not succeed, owing mainty to the depre-
dations of microscopic worms, which cause a disease commonly known as “‘ root-knot.’’
tOne specimen of Pinus t2da was discovered by Mr. Pinchot, and another by Mr. Archur Hollick,
in Southern New Jersey. The region of the Pokomoke river, on the peninsula between the Delaware
and Chesapeake, is, as far as I have been able to observe, the most northern limit of the natural growth
of the bald cypress.
2 According to the investigations of the U. S. Biological Survey (see ‘‘ Laws of Temperature Control
of the Geographic Distribution of Terrestrial Animals and Plants,’’ National Geographic Magazine, Vol.
VI, December, 1894), the northward distribution of terrestrial animals and plants is governed by the sum
of the positive temperatures for the entire season of growth and reproduction, and that the southward
distribution is governed by the mean temperature of a brief period during the hottest part of the year.
According to Prof. Merriam the species of the Carolinian belt require a total quantity of heat of at least
6,400° C. or 11,500° F., but apparently cannot endure a summer temperature the mean of which for the
six hottest consecutive weeks exceeds 26° C. or 78.89 F, The northern boundary of this zone, therefore,
is marked by the isotherm showing a sum of normal positive temperatures of 6,4-0° C. or 11,500° F.,
while its southern boundary agrees very closely with the isotherm of 26° C. or 78.8° F. for the six hottest
weeks, The minimum temperature was assumed to be 6° C. or 43° F., that is, the point where meta-
bolic processes are just possible.
|| By optimum is meant the combination of conditions that produces the best average result.
238 GEOLOGICAL SURVEY OF NEW JERSEY.
mixture and consistency, it is an excellent and inexpensive road
material. The abundance of such gravel in a country where
the natural roads are bad is a fortunate coincidence. When
sand and gravel are cemented together by compounds of iron, as
is often the case, a durable conglomerate is formed, which is the
principal building-stone of the region.
The sources of the rivers of the Coastal Plain are on its
northwestern edge. The land slopes gradually to the sea, and
is so level that tide-water penetrates far into the interior.
Drainage is therefore good, and stagnation of standing water
only occurs here and there in places which are underlain with
an impermeable hardpan.
The Plains* are extensive, practically treeless regions in the
northern part of the Coastal Plain. The region called the East
Plains contains 6,662 acres, and the West Plains 7,737 acres.
There are other areas of the same nature, so that 20,000 acres
is a conservative estimate of the amount of land of this kind.
These Plains are hilly, about one hundred feet in height, and
with gentle slopes. The surface soil is usually a bleached sand.
Often there is a subsoil of clayey loam and gravel at varying
depths. Often the subsoil is hard-pan, and in places there are
beds of conglomerate and strata of clay. ‘There is practically
no physical difference between the soil of the Plains and the
soil of thousands of acres in the neighborhood on which trees
of good dimensions are growing. Owing to the hilliness of the
region in comparison with the surrounding country, and owing
to the lack of a more extensive cover, the soil has been subjected
to the leaching and beating of rain and the scorching and drying
effects of the sun and wind. One would expect to find it, there-
fore, exceedingly poor in quality, with a dearth of plant food,
which might, at least in part, account for the absence of a more
* The term “ plain ’’ is usually applied to hroad stretches of country which are level or undulating.
Owing to the fact that vast treeless areas in the West are called “‘ The Plains,” treelessness is popularly
associated with the word “ Plain.’’ For this reason, no doubt, certain treeless regions in New Jersey are
called “‘ The Plains,’’ although they are hillier than the surrounding country. Geographers, however,
apply the term to level regions regardless of their cover ; for instance, “ the Atlantic Coastal Plain.’’ It
is worthy of note in this connection that the people of the West distinguish between the ‘‘ Plains ’’ and
“ Prairies.’? The term “ Prairies’’ is applied to the region between the 1o4th meridian and the eastern
base of the Rockies. Their treelessness is mainly due to a lack of moisture. East of this are the
« Plains,’’ a fertile but formerly treeless region. The absence of trees is here due rather to the extreme
fineness of the soil or to fire and grass than to moisture conditions. Wherever a plain is produced by fire
reforestation is possible, but in regions where treelessness is due to a lack of moisture, afforestation is
difficult and often impossible without irrigation,
GEOLOGICAL SURVEY OF NEW JERSEY
REPORT ON FORESTRY
Plate No. XVIII.
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REPORT ON FORESLS: 239
extensive growth. A chemical examination disappoints one in
this respect. Very little dependence, however, can be put in
the analysis of a soil. Although the essential ingredients may
be present in sufficient quantity, they may not be in available
form. A soil may be physically and chemically good, but if
moisture is insufficient, the forest will be light and commercially
of little importance.
The Plains are covered with a low bushy growth of several
species. ‘The highest tree (a sassafras) measured in this whole
region was fifteen feet (four and one-half metres). The most
peculiar feature of this area is the fact that a large part of the
growth is a coppice of pine. By the natives these short, stunted
pines are called ‘“‘she-pines.” * They are the stump-shoots of
Pinus rigtda, commonly called the rough-bark or pitch-pine.
When this pine is cut many shoots sprout from the stump, but
since insects soon attack and devour it, the young shoots usually
die in consequence while still small and tender. There is a
strong tendency in the pitch-pine, Peas rigida, to send out
shoots, especially when growing under adverse conditions. Soon
after a fire, with the foliage completely burned, and the bole
girdled, many dormant buds in the crown and on the trunk
develop into shoots, which soon, however, wither and die.
Even logs which have been cut and hauled to the mill send
out similar shoots. These, of course, wither and die just as
soon as the starchy materials and moisture in the trunk are
exhausted. The poorer the soil, and more adverse the condi-
tions, the stronger seems the tendency to sprout from the
stump. Sprouting in this way is rare among the conifers, and,
although of interest botanically, is commercially of no signifi-
cance whatever. Ordinarily a pine coppice is short-lived, but
on the Plains it has persisted for many years. Fire sweeps over
this region frequently and burns the shoots while still only a
few feet high, but the stump, gnarled, charred and full of pitch,
continues to live. Some of the stumps appear to be more than
* The term ‘‘she-pine,’’ or ‘‘ she-pitch-pine,’’ is also applied to Pinxus heterophylla, which grows in
the region of the Gulf of Mexico. In the language of the natives, the prefix ‘“‘she’’ indicates not sex but
inferiority and imperfection. P, heterophylla has been regarded by the lumbermen as a tree of very
inferior quality and of little value in comparison to the true southern pitch-pine, P. palustris. In the
same way the term “she balsam-fir’’ is applied to Adzes fraseri, a small, short-lived tree which inhabits
only the high slopes of the Alleghany Mountains in Carolina and Tennessee. For the same reason the
adjective ‘“‘ bastard’’ is often applied to trees.
242 , GEOLOGICAL SURVEY OF NEW JERSEY.
red cedar ( Juniperus virginiana) and holly (lex opaca) appear
as forerunners, the seeds of which have been dropped by passing
birds. ‘The persimmon and sassafras, hardy oaks, and wild-
cherry (Prunus serotina) also spring up, and near the sites of
old dwellings are clumps of the tree-ofheaven (Az/anthus glan-
dulosus) growing with tropical rankness, root suckers from the
old trees which were once in favor for shade and ornament ;
now and then also an old sycamore with serpent-like limbs ;
here and there pines appear, the edges gradually close in
on the field, the solitary forerunners become surrounded by
their progeny, the gaps are slowly filled by whatever may
chance to fall by the many natural means of seed distribution.
Thus, in time, the whole becomes a mixed forest of many
species and of all age classes: here a thicket, there a pole-wood
consisting of softwood and hardwood, evergreen and deciduous
sorts, many sickly suppressed trees and many much branched,
rough and knotty trees which were the forerunners, holding
their own in the struggle for life even against their own
progeny. Soon come axe and fire; the weaker kinds perish,
the best are used, and a few pines and a coppice of hardy oak
alone remain. Sometimes, if surrounded by pine, these old
fields come up in a growth of pine as thick and green as a field
of orain
The forests of the eastern United States are possessed of
marvelous regenerative power. Among the hundreds of native
species there are many capable of great endurance, and, indeed,
in the regions east of the western prairies there are few spots so
sterile and inhospitable that one or more of these species cannot
survive. There is abundant material for the development of
new and elaborate systems of silviculture suited to the condi-
tions and needs which exist.
A very large part of the Pine-Barren district 1s oak coppice.
The area in pine, however, is constantly decreasing, the area in
oak increasing. Oak of some kind almost invariably follows
* One must not too hastily conclude that the majority of the Jersey pines are pitch or Indian pines
(£. rfgida). A careful census of many districts will show, especially in the southern counties, that the
short-leaf pine predominates. Although the pitch-pine endures fire to a greater extent, the short-leaf
pine is more prolific. From a forestal standpoint, this is, in spite of everything, a hopeful condition of
affairs, because, as I shall endeavor to show later, there is no coniferous forest tree of the dry sandy por-
tions of the Carolinian zone which is silviculturally and commercially the equal of Pizus echinata, the
short-leaf or smooth-bark pine.
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REPORT ON FORESTS. 243
pine. Throughout every pine woods are scattered here and
there suppressed oaks, the seeds of which may have been dropped
by jays or chickarees. Just as soon as the pines are cut, these
oaks, owing to increase of light and room, grow quickly. In
spite of the poverty of the soil and the inroads of insects, and
although burnt and cut again and again, they show remarkable
vigor. *
Even scientific men have advanced the theory that one species
of tree follows another because the first exhausts certain ingre-
dients in the soil which it must have and which another species
may not need. Such statements are rarely founded on facts.
The reason one species follows another may be easily determined
in almost every case with a little observation and study. ‘Trees
do not generally exhaust the soil, but, by bringing inorganic
materials from deep layers of the soil and depositing these in the
form of litter on the surface, and by protecting it from the beat-
ing and leaching of rain and scorching effects of wind and sun,
improve its quality. In moist pine regions which have been burnt
over several times and on which everything 1s killed, birch often
springs up in an almost magical way. This is due to the facts
that the seeds of the birch are quickly distributed by the wind
and quickly germinate, and that the birch is capable of living on
extremely poor soil.
Many dry leaves cling to the small oak trees until the follow-
ing spring ;t the limbs reach close to the ground, and fire, there-
fore, in the late winter or early spring, before there is much sap
in the wood, kills them, although the stumps live on, and with
great persistency produce a fresh growth. In the struggle for
existence the scrub oak and the black jack (Q. marilandica)
usually survive. Although these two oaks are of slight economic
importance, it is due to their pertinacity that in many places
the soil has been prevented from shifting. The species which
form this coppice are, post oak (Q. mezzor), black oak (Q. velu-
tina), white oak (Q. alba), chestnut oak (Q. Arizus), Spanish
oak (Q. digitata), red oak (Q. rubra), black jack (Q. marz-
* It is well known, however, that oaks, chestnuts, and similar trees, lose their vitality when asexually
reproduced for a great length of time,
+It has been suggested by botanists that these clinging leaves indicate a tendency or are a step
toward the evergreen state. The magnolia glauca is almost evergreen in Southern New Jersey. When
leaves cling in this way it is an indication that the species is frost-tender and that the !eaves were injured
by frost before the normal corky layer was formed at the base of the petiole.
244 GEOLOGICAL SURVEY OF NEW JERSEY.
landica), and scarlet oak (Q. coccinea). Hybrids and irregular
forms are common. ‘The coppice is usually cut as pole-wood for
fuel, and has little value. Owing to careless cutting the stumps
are apt to be partly decayed. This decay spreads to the tree.
It also invites the inroads of insects, the number of which
injurious to these oaks is legion.
The wonderful rapidity of tree growth in this sandy soil is
often remarked with surprise. Bleached white as snow, and,
apparently, absolutely destitute of plant food, it is nevertheless
capable of supporting a thrifty arboreal growth. The young tree
starts with the greatest difficulty and languishes throughout the
early part of its life, but as soon as its roots have reached the
deeper and richer layers of the soil it starts afresh and grows
thenceforth with astonishing rapidity. The soil is porous, and
although well drained, is moist a short distance below the surface,
The lay of the land and the nature of the soil is such that the
roots of trees can in the majority of cases penetrate to where
there is constantly sufficient moisture. From the Plains, the
highest part of the Coastal Plain, there are naturally all degrees
of soil-moisture conditions, through the Pine Barrens to the
swamp lands.
A swamp is usually defined as a tract of land with or without
trees, lower than the surrounding country, and so saturated with
water as to be unfit for cultivation.
This definition, however, is insufficient. When one speaks of
a swamp in Southern New Jersey, or in any part of the South-
eastern States, a wooded region is usually meant. A swamp,
also, is not always unfit for cultivation. Some of the best farm
land in America ison swamp bottom. Neither is it always lower
than the surrounding country. Elevated swamps are common,
and the Dismal Swamp of Virginia and North Carolina, which
is like a Jersey swamp in many respects, is several feet higher
than the surrounding country, with a lake in the center from
which water runs in all directions.
The amount of water in a swamp is an important matter, also
the temperature of the water. It variesin amount from a degree
of mere moistness to the condition of the Cypress swamps of the
south, which are at times navigable for canoes, bateaux and often
good-sized scows. Along the Mississippi river there is a vast
REPORT ON FORESTS. 245
region called the River-swamp, which is seldom completely
flooded. Here, several of the trees which grow in southern New
Jersey reach their optimum. Many trees which thrive in water
in the south cannot live in the swamp-lands in the north, because
of their coldness, but thrive on the upland. By the term swamp
is merely meant a wet, muddy region, covered with a wild growth
of trees and bushes.
To wet, almost treeless or treeless areas, the terms savanna,
morass, bog, slough and marsh are applicable. The term
savanna is usually applied to lowlands covered with grasses and
other herbaceous plants ; the terms morass and bog, to extremely,
spongy, sphagnaceous lands; and the term marsh, to the soft,
muddy deposits around and along bodies of both salt and fresh
water. Some are inclined to restrict the term marsh to those
areas formed in salt water. There is little reason for this, since
salt and fresh marshes are essentially alike in formation. All
these terms are, unfortunately, exceedingly elastic in meaning.
A cedar swamp, for instance, is a swamp while covered with
trees, but when cut over, cleared and planted with cranberries,
it becomes a bog.
Much of the Swamp-land in the Coastal Plain of New Jersey,
although merely moist and extremely fertile, will probably
remain in woods for many years to come, because of the diff-
culty in clearing it. A swamp bottom consists of the forest
detritus of ages, and is a matted mass of roots, stumps and tree
trunks.
The swamp-land may, for the sake of convenience, be divided
into cedar swamps and deciduous or hardwood swamps.
The white cedar (Chamecyparis thyotdes),* the finest soft
wood of the region, grows in dense pure forests. The tree is
tall, straight and sharp-pointed. The bases of the crowns meet
to form a solid canopy. The trees grow so close that one sup-
ports another, and when a few are cut, or felled by storm, others
in the neighborhood, deprived of their support, fall in every
direction. The limbs are often festooned with a gray lichen
(Usnea barbata), the pendant tufts of which are favorite nesting
places of the Parula warbler (Compsothlypsis americana). ‘These
* This tree should not be confounded with the white cedar or arbor vite of the north (7/uya occt-
dentalis).
246 GEOLOGICAL SURVEY OF NEW JERSEY.
swainps are warm and protected in winter, and harbor, there-
fore, many birds. They are cool in summer and fragrant with
the odor of clethra (C. alzzfolia) and magnolia (AZ. glauca). A
cedar-swamp bottom seldom freezes. This may be partly due to
the fact that cedar swamps are usually located in regions of
springs.
The forest floor is usually covered with a thick mat of spongy
sphagnum moss. ‘The streaims in passing through the swamps
often separate into several streamlets, which meander through
the mass of moss and submerged tree trunks and roots. The
water of these in dark places is black as ink, but in the light
and in shallows is the color of mahogany or amber, owing to
impregnations from the humus. Nothing is more characteristic
of the Coastal Plain of New Jersey than these swamps of cedar.
Although practically the northern limit of this excellent species,
it is perfectly at home in South Jersey. Free from disease, and
always a fresh rich green, cedar swamps form the most striking
feature of the landscape. It is a common saying in South
Jersey that a cedar swamp attracts a shower. It seems to be
often the case that a thunder storm follows a branch or stream
until it reaches a mass of swamp, and there drops its rain.
Owing to the excellence of the wood, these swamps are
devoured with avidity by lumbermen. The bottom when not
too difficult to clear, and when properly located, is in demand
for cranberry bogs.* When a cedar swamp is cut or burnt, if
certain conditions prevail, it may come again in cedar, usually,
however, deciduous swamp trees, inferior in nature, usurp its
place.
* The cultivation of the large or American cranberry (Ozxycoccus mtacrocarfon) is a very important
industry in South Jersey. The berry, the size of a cherry, grows in large quantities on a low creeping
vine, which forms a mat on the surface. The clearing and preparation of these bogs are expensive, but
the yields are often enormous, and the bog lasts for many years without perceptible deterioration. The
cultivation of this plant requires skill and experience. In times past fortunes have been lost as well as
won in the cranberry industry. The amount of fruit yielded year after year by a bog suitably located
and tended is often enormous A cedar-swamp bottom through which there is a running stream is
selected. This is banked and arranged so that the bog can be easily and quickly flooded, since it is desir-
‘able to keep it covered with water throughout the winter and for a short time at other seasons of the year,
to protect it from frost, to drown out undesirable weeds and insect pests or prevent a fungous disease called
‘“scald.’’ A bog may be flooded at any time without injury to the vines, except when in blossom In
clearing a bog the stumps are usually removed, but not always. The whole is turfed with a cranberry or
bog-hoe, which has a wider blade than the ordinary grub-hoe. Ditches are dug throughout the whole
bog, and sometimes the surface is sanded. It is planted in a simple manner with a suitable variety of
wild-berry from the woods or from another bog. Usually the vines are mown down with a scythe.
These pieces are dropped over the area ready for planting and pushed into the soft soil with a wooden
dibble. They soon take root, and in the course of a couple of years their vigorous stolons have complete
possession of the soil,
/
GEOLOGICAL SURVEY OF NEW JERSEY
REPORT ON FORESTRY
Plate No. XX.
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REPORT ON FORESTS. 247
The swamp lands* being moist, have naturally not suffered
from fire as much as the uplands. They often consist, therefore,
not only of a great mixture of species, but are a semi-tropical
tangle of wild grapes, and othe# vines and bushes. ‘The decid-
uous or hardwood swamps usually contain a mixture of the
following trees of more or less importance: Acer rubrum, red
or swamp maple; Lzguzdamber styraciflua, sweet gum or
bilsted; Myssa sylvatica, black or sour gum, and Magnola
glauca, or brewster, are the commonest. In some swamps there
are beeches (Fagus latifolia), tulip trees (Lzrzodendron tulipi-
sera), swamp white oak (Quercus platanordes), willow oak (Q.
phellos), holly (flex opaca), sassafras (.S. sassafras), and now and
then a pitch-pine (/zaws rzgzda), a smooth-bark pine (/P2zzs
echinata), a white cedar (Chemecyparis thyordes) or even a white
pine.t
Fire and the axe have converted many of these swamps into
sorry looking thickets and cripples,{ which are little more than
tangles of saplings, bushes and vines. It is easy to imagine how,
in the course of time, fire, burning over land of heavy nature or
land which is usually moist, will gradually kill even swamp trees
and shrubs, until nothing remains but herbaceous plants among
charred stumps. "These swamps often become very dry in sum-
mer, and the natives, to improve the quality of the berries (or
very rarely the pasturage), set fires. ‘his must be done, however,
*It is in these swamps where the animals of the woods take refuge, especially the deer, which, at a
certain time of the year when the law allows, are remorselessly chased by packs of hounds. The extinc-
tion of this animal in New Jersey is only a matter of time unless the use of dogs is absolutely prohibited
atall seasons. It is the prevailing opinion in the Adirondacks that the wisest move in the protection of
deer was the prevention of hounding by law. The meat of a hounded animal is poor in quality, to say
nothing of the cruelty which the nagging of dogs occasions. Hunting at best is an immoral sport, and in
America is everybody’s privilege. In every backwoods town there are local social gypsies or pothunters
who love sport and hate work, who spend their days wandering in the woods with dog and gun, and their
evenings in the country store or tavern relating their experiences. Several animals in South Jersey are
hunted not for their pelts or for food but for the bounty which the townships very foolishly pay for the
heads of certain so-called ‘‘ depredatory animals,’’ among the worst of which the fox is classed.
+ The white pine was at one time quite abundant in Manahawken swamp. These pines towered high
above the cedars of the swamp. This suggests the possibility of growing the white pine in such districts
either alone or mixed with white cedar. The choppers whom I consulted at the time of my visit called
the white pine ‘‘ white wood.”’
t The term “‘cripple’’ is a localism used in South Jersey and on the Chesapeake peninsula. It is
applied to a thicket or bushland. It is interesting to note that the Germans use the word in the same
sense, For instance, a stand of trees which has been abused by careless cutting, etc., is called a ‘‘ Krup-
pelbestand.’’ Underbrush is sometimes called ‘‘ Kruppelholz.’’
248 GEOLOGICAL SURVEY OF NEW JERSEY.
when the soil is not toodry.* In this way moist swamps become
meadows. ‘This land, if left to itself and protected from fires,
soon recovers, but there is another kind of grassy land, namely
“ Savanna,” which is of little Worth in New Jersey at present,
and destined to remain unchanged for many years to come.
The formation of such grass land in New Jersey is usually due
to a hard-pan which is often only a few inches below the surface.
Hard-pan is the name applied to a dense, almost impenetrable
stratum of compacted material. It is generally soil in the pro-
cess of becoming rock. In these savanna lands ft it is bog-ore
and organic materials cementing the particles of sand. It is
covered by several inches of humus, which is saturated wiih
water and is sour in consequence. Here and there on knolls in
these sloughs, a pitch-pine grows, but topples over in the course
of time, owing to the slight hold which it has upon the soil:
The hard-pan is similar to the “‘ortstein”’ of Northern Europe and
the “alios” of the French Landes. ‘This stratum exists in all
degrees of hardness, and often in sufficient quantities to prevent
the growth of trees on considerable areas of land, but in a region
where even good wood-land has little value, the comparatively
small area of savanna is not worthy of much consideration, be-
cause the cost of drainage and preparation would amount to more
than the land is likely to be worth for some time to come.
Stretching along the coast of Southern New Jersey and along
the Delaware river, fringing the mainland and bays, and extend-
ing along the rivers far inland, are many miles of salt marshes.
They are of course treeless.{ In former times these lands were
banked and cultivated much more extensively than at present.
Owing to the difficulty of keeping the banks in order, they have
in large part been abandoned. ‘The marshes, endless to the eye,
* Constant burning causes deterioration of pasturage in the course of time. The weaker grasses are
gradually killed. On salt marshes and wild meadows where the soil is very moist, so that the roots are
not injured by fire, regular burning is a benefit ji
+ The term savanna is a relic of the Spanish in America and in general merely means a tract of level
land covered with low vegetation, usually grass. It is used throughout the world in this sense. In old
Spanish the word means a ‘‘ sheet,’’ and was originally applied to a flat snow-covered region.
{In places hardy shrubs and trees are gradually intruding on the marshes as they become by deposit
higher and sweeter. In other places groups of trees may be seen which have been killed by too large a
dose of salt water.
REPORT ON FORESTS. 249
are intersected by many bays, salt ponds, thoroughfares and
winding creeks. They yield thousands of tons of salt hay
(Spartina junci?), and black grass (/uncus gerardz), which are
extensively used for fodder and packing. It is transported on
flat-boats or scows up the many rivers to the interior, and is also
baled and shipped to the neighboring sea-shore resorts and cities.
Owing to the fact that these marshes already yield a good
income, that is, a fair rate of interest on the amount invested,
and probably more than cultivated fields would pay, by producing
year after year a good grade of hay without any labor except
the reaping, and a little ditching now and then, it would be a
precarious investment to bank and drain them as has been done
with similar land in Holland, except in the northeastern part
of the state, where proximity to cities makes land more val-
uable than in the southern part. These banked lands, although
fertile, are unsatisfactory to till; the dykes are* a constant care
and anxiety, and storms and high tides, besides other serious
dangers, often cause irreparable damages.
The reasons for mentioning these marshes in this connection”
are, firstly, they yield an abundance of fodder and litter, and
secondly, the mud is an extremely rich fertilizer, consisting
mainly of humus, but containing also lime, and the decomposed
bodies of both macroscopic and microscopic organisms. It 1s an
inexhaustible store of fertility. In it are the materials which
the sandy soil of the interior needs most. By applying this mud
in the fall, so that the frost will pulverize and mellow it, and,
the following summer, sowing a leguminous crop for green
manure, the sandiest field is rendered so fertile that with
intensive culture, including a regular supply of water and intel-
ligent labor, it will produce fruits and vegetables of the finest
*The banks are often seriously damaged by the musk-rat (Fiber ztbethicus), an aquatic rat-like
rodent. It yields a salable fur and is extensively trapped. They dig through a bank in all directions»
causing it to leak and weakening it throughout in a way which is difficult to repair. They are prolific
and must be combatted in various ways. Many encourage the presence of black snakes (Bascanion
constrictor), which feed upon its young. A tight hemlock board or slab-fence is often constructed
against the face of the bank, or small pilings are driven close together along its outer edge. Ditches
should never be dug on both sides of a dyke, if so, the rats are very tond of channeling from ditch to
ditch. If sand is used in the construction of the outer part of a bank, rats are less apt to disturb it,
because it caves easily and thus interferes with their digging. Willows should be planted on these banks
and fascine and wattlework constructed on their faces. The great use of fascine and wattlework is not
fully appreciated in America. The banks which worry the Jersey farmer would be little more than play
to the enterprising Dutchman who, with patient toil, farms into the very jaws of the sea. He would even
look with envious eyes on our shallow inland bays and would soon convert them into many acres of rich
polder-land.
250 GEOLOGICAL SURVEY OF NEW JERSEY... 3
quality. ‘This litter and mud are abundant and available to all
those who have enterprise and energy enough to utilize them.
The mainland and marine marshes are protected from the
action of the ocean waves by a line of barrier beaches or sea
islands. "These beaches, on which are located many famous
resorts, are separated from one another by inlets through which
the tide sweeps swiftly. Strictly speaking, a beach is that part
of a shore between high and low water, but in New Jersey the
term is applied to what are really sea-islands. These islands
consist of a fine white sand which in places is mobile. When
the tide falls, the sand of the beach proper, dried by the sun
and wind, is blown either inland or into the ocean. ‘The pre-
vailing winds blow toward the sea, and the sand as it dries flies
back into the water to be whirled again on the beach by the
waves. If the wind continues for some time from the sea, sand-
hills are formed. Any small obstacle sufficient to diminish the
energy of the wind may cause the commencement of a dune.
As soon as a little hill is formed, it is easy to see how it may
continue to form while the conditions remain the same. Soon
a strong west wind, however, may hurl it back into the sea, or
an eastern gale fling it inland on the marshes. And so it goes,
forming and re-forming, changing in fact with every caprice of
the wind, gentle and almost unnoticeable during a hght sea-
breeze, but a stinging, blinding sand-blast in times of gale. In
case of an obstruction, which interferes with the action of
the wind, a dune forms equal in height to the obstacle. A
great deal of the land on these islands is now occupied by
resorts; it is all in fact owned by private parties, and is in
places extremely valuable. But here and there are tracts of
wild, shifting dunes. At Avalon there isa huge dune, caused
by a dense forest which is being slowly but surely engulfed.
The dune begins just above high-water mark, and then extends
inland, gradually increasing in height until its summit is even
with the foliage of the trees. It is a peculiar scene from the
top of this dune; on the land side there is a dense mass of dark
green foliage, beyond which there is the broad expanse of green
salt marshes with their bays and thoroughfares.* On the ocean
side, sloping to the breakers, there is a huge mass of fine sea-
* A waterway from one bay to another is called a ‘‘ thoroughfare’’ along the Jersey coast.
‘
GEOLOGICAL SURVEY OF NEW JERSEY
REPORT ON FORESTRY
Plate No. XXI.
RHE CREST OF THE SAND-DUNEVON SEVEN MILE. BEACH
HOWVdd AMW NOUAUS NO SOITIOH
‘IIXX (ON 932I1d
AUALSAAXOA NO LYOdaa
Aasaal MAN AO AFTANNS ITVOIDO1OaD
REPORT ON FORESTS. 25
sand, out of which project the jagged trunks and limbs of
smothered trees. The fine sand sifts into shoes, pockets, cloth-
ing and hair. It comes fresh from the great ocean-mill, ascends
the surface of the dune, and falls over its crest into the forest.
When a stiff breeze is blowing it skims along like drifting snow,
and shoots from the summit of the dune, trimming the tops of
the trees as flat as though shorn with shears.*
If these forests are what cause the dunes, by preventing
the west wind from blowing back the sand, how did the forests
form? Single trees here and there, or groups of trees, which
are clean underneath, so that the west wind sweeps through
without serious interruption, do not cause the formation of dunes.
In the course of time, however, a thicket forms under these
trees. ‘They become covered with grape vines, Virginia-creepers
and green-briars. The birds and winds scatter the seeds of
many sorts of shrubs and bushes, such as Prunus maritima,
sweet-gale, Baccharis halimtfolia, etc., ete., until a dense forest
is formed through which the west wind cannot penetrate, the
consequence of which, in the course of time, is a dune, which in
turn finally engulfs and kills the forest that had caused it.+
It is a mistake to suppose that this sand is sterile because it
appears barren. ‘True, it consists mainly of granules of quartz,
but these are extremely fine, the interstices are small, and the
capillarity great in consequence; mixed with it are particles of
shells and other materials, organic and inorganic, which are in
the ocean, working down the coast until washed ashore and
shifted with the sand.
The forest at Avalon is so dense that many birds seek shelter
there. The principal trees of these beaches are the holly (//ex
opaca), the red-cedar (/Junzperus virgintana), the sour or black-
gum (WVyssa sylvatica), magnolia (AZ, glauca), wild-cherry
(Prunus serotina), hackberry (Cel¢7s occidentalis), sassafras,
swamp-maple (dcer rubrum), and a few oaks, and pitch-pines
and even red-mulberry. The commonest, and by far the most
characteristic, trees of the beaches are the holly and red-
*I am of the opinion that the shapes of trees along our coast is due more to the sand-blast than to the
direct action of the wind. This also limits the number of species. Those plants with foliage best able to
withstand this sand-blast are the ones which grow nearest the sea.
¢ By clearing away the underbrush and trimming the trees to let the west wind through, it might be
possible in several places along the coast to dispel the dunes and prevent their future formation.
252 GEOLOGICAL SURVEY OF NEW JERSEY.
cedar. The holly thrives here, reaching a much larger size
than on the mainland, apparently enjoying the moist, salt
atmosphere and loose sand. It is a dune-tree par excellence.
Its limbs are close and jagged, in striking contrast to the
pyramidal, symmetrical holly trees of the inland open field. Its
prickly foliage is dense and dark green, and its crown is flat.
It produces rich red berries in profusion, and its bole is bright
gray in color, rugged and sturdy. It is not uncommon to find
two hollies grown together, or the limb of one tree growing
into another tree, or a limb bending down and uniting with the
trunk, forming what the natives call “‘jug-handles.”” Those who
are familiar with the region will never forget these groups of
hollies, nor the masses of aromatic red cedars with limbs fes-
tooned with gray lichens. (See plates XXI, XXII and XXIII.)
There is but little danger lurking in these sand-hills. They
are, in this respect, unlike the dunes of Gascony, which, if
robbed of their forests, would bury villages. The Jersey dunes
are so wild and picturesque that many prefer to let them have
their way; but the scenes on these beaches, so attractive and
peculiar to-day, are destined to lose much of their charm by
being transformed into resorts for recreation and pleasure.
How lacking in shade and attractiveness are our American
sea-shore resorts in comparison with those of the Old World !
Look at Arcachon (see plate XXVIII), for instance, with its
summer village by the shore and its winter village of beautiful
villas in the midst of a magnificent pine forest ; or at the famous
Dutch resort, Scheveningen, with its beautifully shaded avenues ;
or Domberg (see plate X XV), or anywhere, in fact, in the lee of
the dune, which protects the farm-land where the industrious
Dutch have beautiful villas in the midst of the woods. Sand-
bars and mud-flats should never be despised, and a country close
to the sea enjoys many advantages of which its people are not
always conscious.
The utilization* of the forests of America began with the
Indian. The Coastal Plain of New Jersey, however, was very
sparsely inhabited before Europeans landed. Here and there
along the rivers may be seen the vestiges of Indian villages, pot-
* One often hears and reads the statement that the branch of forestry called “ forest utilization ’’ and
“lumbering ’’ are synonymous. This is a mistake in that lumbering is no more forestry than the picking
of wild fruits is agriculture.
GEOLOGICAL SURVEY OF NEW JERSEY
REPORT ON FORESTRY
Plate No. XXIII.
A GROUP OF RED CEDARS ON THE COAST OF NEW JERSEY
REPORT ON HOREST S. 253
sherds, broken shells, bones and bits of jasper. At certain times
of the year large numbers crossed the State to enjoy for a time
the bathing and fruits of the sea, but the permanent population
was never large. The Indian of New Jersey domesticated no
animals and cultivated only a few plants. His clumsy stone
implements were so unwieldy and impotent that he was unable
to exterminate animals or cut down forests.* He depended
mainly upon the fruits and animals of the woods. He needed
only wood for fuel, which was everywhere plentiful, and white-
cedar logs, out of which to shape his canoes. The rivers were
his highways, the canoe his conveyance. Fires, no doubt, were
set both accidentally and purposely by the Indian, but in South-
ern New Jersey they were probably infrequent, and did compar-
atively little damage. Indians in parts of Western America still
fire the bush} to facilitate hunting. They desire open prairies
and intervales for their game. In many places east of the Missis-
sippi river, after the Indians departed, prairie fires which they
had purposely set every year, became less frequent, and forest
vegetation in consequence began to appear in the open land.
He has left his impress upon the country however, and Indian
words are indelibly attached to many localities, and to the names
of many plants and animals, such as persimmon, chinkapin, hick-
ory, tamarack, mahogany, pecan, etc.
Although the Algonquin Indian of New Jersey was dependent
upon the forest and still in a primitive state, he cultivated smal]
patches of maize and perhaps other vegetables, and was familiar
with the edible wild plants. From the Indian the whites learned
of a tree (Acer saccharum) with a sweet palatable sap{t that grew
*«* The chief use of the hatchets among the Delaware Indians of New Jersey,’’ says Kalm, “‘ was to
make good fields for maize plantations. If the ground was covered with woods, they cut off the bark all
round the trees with their hatchets at a time when they lose theirsap. The trees thus girdled died, and
the ground was a little turned up with crooked or sharp branches ”’
+ The term ‘“ bush’”’ is a peculiar one. It usually means a single low woody plant. In certain
regions, however, it is applied to a wild forest with a dense underbrush. The sugar maple forest or
orchard is sometimes called the ‘‘sugar-bush.’’ The word in Dutch is ‘‘ bosch,’’ and means forest, and,
no doubt, the Hollanders were the first to apply it in this sense in South Africa and America. The word
‘bois’? in French and ‘‘ bosco’’ in Italian are probably modifications of the same word. There is an old
English word “ boscage,’’ which means a thicket or woodland growth. In old English law boscage
meant food for cattle derived from trees or bushes, also a tax on wood brought into a city.
{¢ Col. Wm. Fox, in his paper on the maple-sugar industry, in the latest report of the New York State
Forest Game and Fisheries Commission, says: ‘‘ For our first knowledge of this product we are
indebted to the North American Indian, the same people who gave us corn and tobacco. From the
records of the earliest explorers on this continent it appears that the Indians tapped the maples, gathered
the sap in rude receptacles, and boiled it. The first white settlers used the same methods, which substan-
tially remain unchanged to day.’”’
254 GEOLOGICAL SURVEY OF NEW JERSEY.
in the northern mountains. ‘The settler, in times of famine,
often appealed to the Indian, and many of the fruits and vege-
tables upon which he fed have been since neglected. The Indian-
club and the Indian-fig, for instance, two of his important food-
plants, are perhaps worthy of cultivation and improvement.*
The Indian of New Jersey was soon superseded by the settler,
who, provided with two powerful implements—the axe and the
gun—cleared small patches of land, and built cabins along the
rivers. [rapping was the settler’s first occupation and peltry ft
was one of the first and most important products of the virgin
forest. Hunting and trapping in early times were hazardous,
but often lucrative occupations. The forest was difficult to clear,
and just as the young poplars to-day harass the New England
farmer, by invading his pastures, and the mink and fox rob the
hennery, so in early times a hundred-fold more bothersome were
the suckers and seedlings, and animals from the woods between
the clearings. Fire was freely used, and from the ashes potash
was extracted by leaching. This lixivium, by mixing with
erease produced soft-soap, which is still manufactured by country
people. In many places to-day wood 1s extensively burnt for its.
ashes and used as a fertilizer.
Soon shipbuilding developed into an important industry. Oak
and pine of the finest kinds were plentiful. Saw-muills were
built along the streams, and lumber was shipped even to the
West Indies in exchange for rum, sugar and molasses. The
construction of schooners continued until recent times to be an
important industry. Now, only small sloops, scows and bateaux
are built. Ships of iron, propelled by steam, have superseded
the clipper.
* It may often be the humblest and least conspicuous plants which yield the richest food materials,
and not always the major forest products which, considering labor and time, yield the largest returns.
The salep of Turkey and the truffles of France are excellent examples. Salep is a farinaceous food
obtained from the tubers of wild orchids, It contains a substance called bassorine, which is very nutri-
tious. Over $3,000,000 worth of truffles are exported annually from France. They come mostly from
Perigord, and grow in limestone regions on the roots of oaks.
+ Several wild animals have, and perhaps others might be, profitably bred for their pelts. The
skunk (Mephitis mephitica), one of the commonest and most disagreeable of all the animals of Eastern
America, produces a salable fur called ‘‘Alaska sable,’’ and in spite of the facts that it emits a nauseating
odor and that a kind of hydrophobia results from its bite, has been kept in confinement and bred for its
skin. The mink has been tamed and reared in minkeries in New York State. It has been said that a
mink is as profitable as a cow. Coues, in his “‘ Fur-bearing Animals of North America,’’ says: ‘‘ Were
not fashion so notoriously capricious, mink pelts would maintain a conspicuous place in the fur-marts of
the world; certainly few surpass them in richness of color, gloss and fineness ””
REPORT ON FORESTS. 255
Scattered here and there throughout the Pines are the remains
of what were once centers of a flourishing industry. This
was the manufacture of iron from bog ore (limonite). In some
places the furnaces and forges have been completely obliterated
and forgotten; in others only bits of black slag remain,
while in others the ruins are still standing. These centers
of industry, usually located in the neighborhood of streams
and bogs, were connected by stage routes, along which here
and there were clearings and taverns. Immense quantities of
charcoal were consumed by these forges and furnaces, the owners
of which usually possessed the land for several miles in every
direction. Wood in those days was in demand, and coalings were
frequent. Even after the iron industry in the Pines succumbed,
charcoal was shipped to the cities by schooners in large quan-
tities. Owing to the abundance of other forms of coal, the demand
for charcoal has gradually decreased. Along the rivers there
were many depots to which the charcoal was carted, which are
still in evidence, owing to the great masses of coal-dust which
‘accumulated there. Coal and iron were worked side by side
in the neighboring State of Pennsylvania, transportation by
rail increased the competition; the iron industry in the Pines
was unable to survive, and with it faded the manufacture of
charcoal,* and the value of coal-wood. The ruins of furnaces,
the large dilapidated houses, the overgrown roads, the wharves,
the piers, the old ship-yards, and the masses of coal-dirt on the
landings are evidences of what the country was when iron was
made from bog-ore, and when schooners were built to trade to
foreign lands. The woods were full of men hewing timbers,
cutting coal-wood, working in the coalings, raising bog-ore and
carting materials from place to place. The death of these indus-
tries, however, is only the result of progress. In*the develop-
ment of the whole of a country, certain parts, although they
may have once played an important role, must suffer. In the
course of its development almost every country is subjected to a
series of industrial ups and downs.
Another peculiar old-time industry was the mining of cedar.
he bed of a cedar swamp is a mass of forest detritus, several
*Tt is unfortunate that so little charcoal is used in the American household. The fine flavor of
French cookery is partly due to the use of an excellent quality of charcoal. Other kinds of coal and wood
emit gases in the process of combustion which taint food more or less, and for successful broiling charcoal
and the brazier are necessary.
256 GEOLOGICAL SURVEY OF NEW JERSEY.
feet in depth, in which there are logs of white-cedar perfectly
preserved and excellent in quality. The white-cedar, like the
cypress of the South, reaches a ripe old age. Over one thou-
sand annual rings have been counted in buried stumps six feet in
diameter, and, judging from fallen trunks, the age of these
swamps is many centuries. It establishes the fact beyond a
doubt that the white-cedar has been growing in South Jersey
for ages, and that it is perfectly at home there in every sense of
the word. The wood of many of these buried logs is sound and
light. These were dug out, sawn into billets, and split by hand
into what were called ‘“ mud-shingles,’ which last for many
years. *
It seems strange that the mining of cedar, when wood was
plentiful, should be more profitable than at present, when white-
cedar is scarce and poorer in quality. Lumber is cheaper in
parts of Eastern America to-day, however, than it was a quarter
of acentury ago. This is due to the fact that a much wider
field has been brought into competition by the development of
railroads, and special long-distance freight rates from regions
where timber is still plentiful, and where very complete, labor-
saving, wholesale methods of working it are in practice.
The production of tar was not very extensively developed,
and lasted only for a short time. The existence of the industry
was due to the peculiar exigencies of the times. During the
Civil War the North was deprived of necessary naval stores, for
which the ship-chandlers were willing to pay enormous prices.
The natives of southern New Jersey took advantage of this
opportunity and collected large quantities of ‘‘ fat-pine knots,”
out of which they manufactured tar.
At one time the splitting of hoop-poles for barrel-hoops was
an important industry. Coppice oak was used for the purpose.
*In “ mining’’ cedar logs a great deal of skill and experience was required. Of course, many of the
trees in the swamp were worthless when they fell. The person in search of shingle logs, therefore, first
sounds the swamp-bottom with an iron rod. When he finds a solid log, he notes its position, size and
length. With a sharp spade and axe he cuts down to it, in order to secure a chip of it, from which he is
able to tell, especially by the smell, whether it was uprooted by the wind or broken off above the ground.
In the first case it is apt to be much sounder and better. If satisfactory, he digs a trench along its length,
and saws it off at both ends. The hole he has dug soon fills with water, and, after the log has been com-
pletely loosened, it rises and floats, being surprisingly buoyant. It turns over also, at the same time,
being lighter and fresher 1n appearance on the underside. It is then rolled out of the bed where it has
rested many years, is sawn into proper lengths, and split into shingles, There is still, no doubt, buried
cedar in the swamps of South Jersey, but although fine in quality, it requires so much labor to work it
that it is no longer profitable.
REPORT ON FORESTS. 257
Owing to the substitution of bags for barrels and iron for wooden
hoops, there is practically at present no demand for hoop-poles.
At one time many people found employment in gathering the
leaves of the upland sumac.* These were ground at the mills
and were used for tanning.
The principal industries of the present are the cutting of
wood for fuel and the working of timber for constructive pur-
poses. Several minor products of more or less importance are
also collected.
Wood for fuel may be divided into two classes—pole-wood
and cord-wood. When small-sized trees are cut in the pole
stage, such as oak coppice, they are merely stripped of their
branches, and are not divided into regular lengths, and are sold
as pole-wood, which is consumed locally and bought and sold
by the one-horse or two-horse wagon-load. This wood is abund-
ant and has little worth. If killed by fire, as is often the case,
it is not seriously injured for fuel, although slightly charred,
and often disagreeable to handle. Large quantities of this wood
may be had for the asking. ‘The person who sells pole-wood
usually receives little more than his labor is worth in cutting
and delivering it to the purchaser.
Cord-wood + is cut into sticks four feet long, and split once.
It is usually either pure pine or oak, sometimes mixed. If located
near a railroad or along a good wagon-road, there is a slight
margin of profit in this wood. In many parts of the Coastal
Plain of New Jersey it has no worth, because the cost of cutting
and transportation is equal to or even more than the market
price. Often, however, if the owner has teams of his own, he
cuts the wood when slack of other work and transports it in
order to furnish himself with labor. His wood-land really has
* The chestnut oak (Quercus prinus) furnishes the best tanning material of eastern trees. It is
hardly safe to recommend the planting of trees for tan-bark owing to the fact that other means of tanning
are in process of development, and new and perhaps better methods are liable to replace the old. There
are a few people, however, who believe that oak bark will be worth more a few years hence. The use of
quebracho, from South America, has had an important effect on this industry, but quebracho wood and
hemlock will not last forever. The chestnut-oak is common in South Jersey, and one should have no
hesitation in planting it. It grows fairly well in the shade of pine trees. In spite of the use of many other
tanning materials, the choicest leather is ‘‘ oak-tanned.’’
A cord, in Jersey, is four feet wide, four feet high and eight feet long. It contains eight cord feet
or one hundred and twenty-eight cubic teet, or 3.62 cubic meters.
I7 FOR
258 GEOLOGICAL SURVEY OF NEW JERSEY.
little intrinsic value.* It is merely a means to an end. It
pays, however, to convert the straight limbs and tops of trees,
from which saw-logs have been cut, into cord-wood. South
Jersey has to compete in the production of cord-wood with the
woodland along the rivers of the neighboring States of Delaware,
Maryland and Virginia, where a large negro population exists,
which is skillful with the axe and willing to work for small
wages.
The production of fuel-wood in South Jersey, however, will
always take care of itself. Woods should be managed, therefore,
with saw-stuff in view. Good lumber? is scarce and high in
price, while fuel-wood { has practically no value whatever.
Much could be said of chopping in general, and the imple-
ments and methods in use of felling and converting trees. The
American axe, the most perfect and useful of ordinary imple-
ments, is worthy of a chapter in itself. Intelligent chopping
should be classed as skilled labor; in fact, by a judicious use of
the axe in the hands of a person with an exact knowledge of the
conditions which obtain, it is often possible to bring order out
of chaos and correct the work of careless slashers. §
It requires only a short space to describe the handling of tim-
ber in South Jersey. There is no rafting, no skidways, no lum-
ber camps. All this belongs to the past, when ship-building
*A few years ago wood was sold in Philadelphia from South Jersey for the purpose of dry distillation.
There are several establishments of this kind in neighboring States. I fail to see why this industry could
not exist in South Jersey as well as elsewhere. It is an industry which would use the rough wood, for
which there is no market, and which rots in the forest. There are many dry distillation plants in New
York and Pennsylvania, and the gemand for the product is constantly on the increase,
+ The terms “‘ timber’’ and “‘lumber’’ are used in a peculiar way in America. Lumber means sawn
stuff in merchantable form. It means also disused articles or discarded goods of any kind, and, according
to some authorities, it is a modification of the word Lombard, the Lombards having been, in early times,
famous pawnbrokers. Although the word lumber only means sawn or dressed stuff, the term lumberman is
applied to a forest proprietor, a lumber merchant, or a worker of timber, Timber is applied to large-sized
sawn or dressed stuff, and to the forest of trees large enough to produce such material. Such a forest is
designated ‘‘standing timber.’”’ ‘‘ Timber-culture ’’ is used instead of silviculture, and the term ‘‘ stump-
age’’ means standing timber, considered with reference to its value for cutting, so called because the
amount cut is ascertained by counting and measuring the stumps.
tA chopper should cut the tree close to the ground, leaving a clean-cut sloping or roof-shaped stump.
This lets the water off, prevents decay, and produces a vigorous coppice. The slashings should be piled
in open places and burnt where there is no danger of the flames injuring neighboring trees. Always pro-
tect the young growth, favor the most useful kinds, and never forget that they are the materials from
which the future forest is formed.
21t would be difficult to find an apter term for the common run of wood-choppers than ‘‘slashers,’’
and the lumbermen themselves have aptly applied the term ‘‘slashings’’ to the immense piles of rubbish
which they leave in their wake. It is this slash which brings disaster to the woods because of its great
combustibility.
REPORT ON FORESTS. 259
was an important industry. ‘The writer can just remember the
long line of mule teams, bound to the shipyards on the shore,
with long straight stems of the oak and smooth-bark pine. The
logs are now, usually, short and small, the roads are good and
level, so that with the help of a couple of skids, cant-hooks and
parbuckles the handling of logs is a stumple operation.
The saw-mills are simple in nature and only work lumber for
local demands, finding, however, in the resorts along the shore a
good market for building materials.
The income from the gathering of wild fruits is probably
equal to, if not more than the yield from fire-wood. ‘The most
important of these are the cranberry, huckleberry and blueberry.
The cranberry (Oxycoccus macrocarpon*) is now extensively
cultivated. It keeps well throughout the winter, and forms a
rich crimson sauce, which is relished with turkey. Large
quantities of these berries are exported to other States, and
even to foreign countries.
The high-bush blueberryt (Vaccenzum corymbosum), which
reaches perfection in the swamps of South Jersey, has never
been cultivated. It is preferred by many to all other wild fruits.
It reaches the dimensions of a large shrub, if not a small tree,
on rich, moist, loose soil. The quality of the berries can be
easily improved by trimming. The natives know this and
accomplish it in a drastic, wholesale fashion by firing the woods.
The young shoots which spring up after a fire bear large luscious
berries.
The wild grapes are also abundant. The fox grape (V2tzs
labrusca), is plentiful in the swamps, the vines of which often
form luxuriant tangles in the tops of the trees. The fruit is
dark purple or amber in color, with a tough pulp, but delicious
musky aroma, and famous for Jelly.
The persimmon tree (Dzospyros virginiana) bears an abund-
ance of rich fruit. The improvement of this fruit by grafting
has begun. At present, when a little green, the fruit is puckery ;
when ripe, too soft; it 1s also too small and has too many seeds.
* The term ‘‘cranberry’”’ is properly restricted to the genus Oxycoccus, the term ‘“‘ huckleberry’’ to
the genus Guylussacia, and the term “‘ blueberry ”’ to the genus Vaccinium.
g y MA 8
+ White or pink varieties are not uncommon, which are simply cases of albinism. These are very
sweet and worthy of propagation.
260 GEOLOGICAL SURVEY OF NEW JERSEY.
It contains, however, a larger amount of nutritive matter than
other fruits, and is excellent for pies and puddings. *
The beach-plum (Pras maritima) grows in sea-sand, close
to the ocean, and in the driest, most inhospitable places, and at
the same time bears a large crop of plums, which are excellent
in flavor. It is only a shrub, but well worth planting in sandy
regions. In addition to the above fruits there are many others
of more or less importance for food, flavors and wines.
The floor of a cedar swamp is usually covered with a mass of
sphagnum-moss. ‘This is collected, baled in hay presses, and
sold to nurserymen for packing purposes. ‘This material is
remarkable for its ability to retain moisture and is extensively
used in the shipment of plants.
Large quantities of holly, mistletoe, cedar, etc., are sold in
the cities. Many thousands of the most beautiful and sym-
metrical young conifers are sacrificed annually for Christmas
trees. If the trees were raised for this purpose it would be a
legitimate business, but the Christmas-tree gatherer, in order to
secure extra fine specimens, cuts the tops out of large-sized red-
cedar trees, just as fishermen peel the inner bark from the butts
of the white-cedar for fish-strings.
Many flowers, especially those of Magnolia glauca, are col-
lected in large quantities and sold.
The cultivation of the willow for basket work is in its infancy
in New Jersey. The wood of the white-oak (Q. alba), when
split into thin slivers, is an excellent basket material.t These
baskets are strong and durable. The common American market-
basket is not woven. It is extremely cheap and simple, and
goes with the contents.
There are many plants of more or less value medicinally.
Perhaps the most important, which is common throughout the
* The persimmon grows luxuriantly in the old fields of South Jersey, where animals have carried the
seeds. It is possible to bud or graft thesé trees with choice varieties of the persimmon, which produce,
when in the proper stage of ripeness, a very delicious and salable fruit.
+The basket-tree of the South, however, is Ouercus michauxii, the basket or swamp-white-oak.
This tree is very closely related to Quercus platanotdes, if not a southern form of the same. It grows
in the swamps of South Jersey, but is not abundant. It is one of the most magnificent trees of the oak
family. A few years ago it was plentiful on rich southern swamp bottoms. Its wood is of very fine
quality for constructive purposes, and possesses a peculiarity which especially fits it for basketry. Each
annual ring may be easily separated in the form of a thin flexible strip of great pliability and strength.
The thousands of baskets used in the cotton fields of the South were woven from ribbons of this wood.
This, together with the facts that it requires rich land, and does not reproduce itself freely, is about to
cause its extermination.
REPORT ON FORESTS: 261
woods of the E. Carolinian Zone, but rare in New Jersey, is the
witch-hazel (HHamamelis virginiana), a fluid extract of the twigs,
etc., of this plant is a famous lotion for allaying inflammations.
It is used by everybody for the ills of both man and beast. It
is a peculiar shrub, with several branching crooked trunks,
about ten feet in height. Its pale yellow flowers bloom late in
autumn when the leaves are falling, and the woody capsule,
which explodes and scatters its two black shining seeds, matures
the following summer. It grows well on the poorest kind of
gravelly soil.
Acorns are abundant and are fed to swine. ‘There is a fair
crop almost every year, and an immense crop every now and
then. ‘Turkeys which thrive on dry, sandy soil, feed on the
acorns. Black walnuts contain rich food material and are used
by confectioners. Hazel-nuts grow well in the swamps, having
escaped in several places from cultivation. "The wild chestnut
thrives in the moist sand of South Jersey, and although the
nuts are usually small, they are very sweet and abundant. In
addition, the collection and careful preparation of the seeds of
important forest trees would yield ever-increasing returns.
I have yet to mention forest litter, especially the collection of
‘“pine-chats”’* or leaves, which in many pine regions plays a
very important and peculiar role.
Forest litter is extensively collected in southern New Jersey
for the bedding of animals and as fertilizer for sweet potatoes ;+
in fact, fair crops of this staple food material may be raised on
extremely sandy soil, without other manure.
It is, however, south of New Jersey, on the peninsula between
the Chesapeake and Delaware, where the litter is most assidu-
ously collected and used. The conditions which exist there are
peculiar and instructive to those interested in the amelioration
of pine-lands. In fact, it is the demand for forest litter which in
a great measure has prevented forest fires and impressed upon
the natives the value of their forests.
*In provincial English the term “ chat’? means catkin, or a twig for kindling. The term “ catkin””
means little cat. There may be some connection between the old English application of the term to small
twigs and the use of the word pine-chat in the South.
¢ The German literature on this subject is quite exhaustive. The manurial value of pine straw lies
mainly in its nitrogen contents. From one acre there may be had annually about 2,500 pounds of straw>
furnishing about 20 pounds of nitrogen, 12 pounds lime, 34 pounds potash, 31{ pounds magnesia and less
than 3 pounds phosphoric acid.
262 GEOLOGICAL SURVEY OF NEW JERSEY.
Almost every farm has its pine forest. These, of course, are
of all sizes and ages, varying from fields as thick and dense as
grain to forests fit for large-size timber. There are few signs of
forest fires.
The soil is light and sandy, dune-like in nature, along the
shore, to which the pines grow close, although a few have been
killed here and there by shifting sand. The natives recognize
the value of the forest in holding the soil in place, and in pro-
tecting their truck-patches from the force of the wind, which
would naturally at times sweep over this narrow peninsula.
On entering one of these forests, one observes at once that
although there are many small trees of holly, and bushes of
sweet-gale, the ground is free from litter and brush. If one
happens to visit the region at the proper season he will see men
and women raking up the forest litter. Very early in the spring
or late in winter one can see field after field covered with pine-
chats, to be plowed under just as soon as the weather permits.
In fact, the fields are laid out in squares, by means of the plow,
in order that the pine-chats may be easily measured and thus
evenly distributed. Just as soon as a field becomes worn out it
is abandoned; the adjoining woods furnish the seed, the wind
sows it, and soon a fresh growth of pines appears. Here and
there throughout the forests there are avenues, which, although
constructed to facilitate the collection of pine-chats, serve at the
saine time the purpose of fire-lanes.
Because of the value of the pine-chats the forest floor is free
from inflammable materials just at a time when fires are most
likely to occur. The removal of this debris is contrary to the
principles of German forest management, because it naturally
impoverishes the forest soil. In the course of time, however,
many of these potato-fields are allowed to come up in pines, and
fresh fields are cleared when the pines have been cut.*
* Unlike other crops, the forest constantly improves the soil, provided the litter is not removed or
allowed to burn, The roots of trees penetrate to its deeper layers, and absorb large quantities of mineral
matters. A large percentage of this material goes to the leaves, and is deposited on the surface. The
surface soil is both enriched by these mineral substances and protected by a mulch of humus in varying
stages of decomposition, As the lower layers rot, new layers of leaves and twigs are being constantly
deposited, so that the forest soil, in the course of time, fairly reeks with nourishing plant-food. It has
been shown, without doubt, that the removal of litter from poor soils is ruinous. It is like stealing food
from a starving man. ‘The removal of forest litter from rich soils is indeed, however, a very small matter,
and it is doubtful if it really does very serious injury.
REPORT ON FORESTS. 263
Another point of great advantage is, that the forest 1s not con-
tinuous, but cut into parcels, with farm lands and glades inter-
vening. In fact it is a land of thrifty forests without foresters,
and practically without the need of forest laws.
For private holdings of pine lands, I aim inclined to favor this
method of management, under the peculiar conditions existing
in certain parts of America. In this way the forest constantly
yields, indirectly, an important income. It is simply a rotation
of crops, of which the pine is the most important, producing
throughout its whole life a material which, to the farmer of the
eastern shore of Virginia, is of more value than wood.*
It is easily seen, from the condition of the forest industries
which have just been described, that the Coastal Plain of New
Jersey has passed through the first and most lucrative stage of
its existence. The time is at hand for the establishment of
industries with permanency in view. The most important step
in the right direction would be the protection of its woodlands,
game, fish, oysters and clams, which were once so abundant.
* By this system of culture the pine naturally and quickly regenerates. Large quantities of swine
run in the forest in this region, and probably do as much good as damage in keeping the soil loose on
che surface and by covering the seeds in the process of rooting.
Il. Forest Policy and Silvicultural Suggestions...
HKORKS ie POLICY.
As has been explained already, there exists in Southern New
Jersey a vast area of land which is in a deplorably unproductive
state. It is sufficient to say that in the hands of private owners,
under the circumstances which at present exist, the future of a
large part of this land is not bright. A change of some kind is
necessary, and this must come either in the form of a change
_ of ownership or of the circumstances which fetter ownership.
The only way in which the ownership may be quickly and
materially changed would be by State purchase. It is question-
able whether under the circumstances State ownership would
be justifiable, and whether, even if it could be easily accomplished,
it would improve the situation. The State ownership of forest
land in New Jersey is only justifiable on the ground that the
presence of forests is necessary for purposes of protection
against the destructive forces of nature, for pleasure parks or
for the purpose of preserving the beauty of certain unusually
beautiful or wonderful localities, such as the Palisades.
It is generally conceded in this country that State ownership
of forest land for revenue is unnecessary. The American people,
in fact the Anglo-Saxon race as a whole, has a wholesome aver-
sion to the participation of the State in industries for the pur-
pose of revenue.
Many claim that even in cases where the forest exerts no very
marked influence in a protective way against the destructive
forces of nature, that the State ownership of forests is justifi-
able on the grounds that it requires so long for trees to mature
that private individuals are unable to grow and handle them
satisfactorily to themselves or to their neighbors.
This argument, however, does not always hold good. Were
aman to plant the seed and then wait for the forest to mature,
even the most ardent forester would become impatient. Were
(265)
266 GEOLOGICAL SURVEY OF NEW JERSEY.
he to begin, however, with a forest such as exists even in New
Jersey, he could, even from the beginning, reap something every
year, and his forest would, at the same time, improve in quality
and productiveness. It is quite possible for a private individual
to sow the seed and reap at least three or even four crops of sal-
able materials in a lifetime. It is worthy of note that some of
the finest, that is the most productive, forests of Denmark are
under private control. s teEe. 2° a aah ay h- oe 0.0236 0.0215 0.0458
The Expt. Station Record gives tables which, in general,
show the limits assigned to rich and to poor soils. They are as
follows:
* The sands of the Golden Gate Park were so poor in nature that barley sown on its surface after
being ploughed and cultivated in a favorable season with plenty of moisture, grew only about six inches
in height and failed to perfect its seed. After planting sea grass to fix the sand and lupines to enrich the
soil, the trees which were planted only grew to a height of ten feet, owing to the lack of nutriment in the
soil. See the Reclamation of Drifting Sand Dunes, in the Forester, for October, 1899.
REPORT ON SORES LS: 299
Nitrogen, Phos. Acid. Potash, Lime.
Wiety POOT'SIi1S, 5-2 5. . 0.05 % 0.01 % 0.05 % 9.10 %
IBOOR SOUS aes =e ct aie (1 0.05-0:10 0.01-0.05 0.05-0.10
NCCI GIs ee a ores. oe, 2 OSLO 0.05-0. 10 0. 10-0.20 1.00
ie imac eum 42! 24. 2 O310-0,20 0. 10-0. 20 0.20-0.30
Metyaitcimaee ss 6% fs) 2 > ©2204 0,20 up 0.30 up 2.00
According to this the treeless Plains, as far as the soil is con-
cerned chemically, except in the quantity of lime, if these analy-
ses are correct, have a first-class pine soil. The soil of the Jersey
Plains contains the following ingredients:
Sample I. Sample IT.
INGERO CCT metaer ts: iimrd. vel gh tae sed ee 0.06 0.03
WHOSPMOFICraCId.: Es re ane we ge se 0.07 0.065
AOE AG IMME Cermanee ters atet sar. el ial tay) ec) ne 0.05 0 02
inte Merrett uke Sieh c ee ety ee 0.06 0.02
SiltcariiTSole ter, gloss Se Beso es 96.40 96.95
JENIUGS 0a NE OITA vac oy en Eas 0.28
PerierOmde nee e.mail alee Som 0.40 . 0.20
MGREOUS OMI Gel x: cach la wm “ey 1.26 1.06
WVIAC MESHAS wale ce ta ec ge sn omc