‘¢ UTR Ra haa ge tas sheet ater Sra : sdD- Saw ae i++ oe co N5G4Re ee 5 iT he Forestal Conditions AND aaa Prospects 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, OFFICIAL DONATION. iy ad Py) oan mils y A Reve : yey 4 > +. Fe Day ¢ ht Aa Pe: rece alta Py ot) Tee DoAy a ye. GEOLOGICAL SURVEY OF NEW JERSEY REPORT ON FORESTRY Plate No. XVII. e a Re s 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. i ee eC a = ‘ ra - _ ca ———— ea eo = : ba © : . Bos: _ a _ _— a maine dt teem SOE Sse - 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. GOOMIAMWT LY SOINId DHL —— ee pee ae ns EPMA “e a BE spe men el, “XIX “ON 938I1d AUYLSAAYOA NO LYOdaAy Agsaal MAN 4O AFANNS TVOIDOIOND 4 “7 1 an = a >= _ ‘ 1F : Ty : er 7 3 a ’ ' . - i oy + 2 << a aa - - zy a _ - a & ¢ uf : 7 7 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. hy A anil moar te. ms rs Sealy wk * MP SWA » Xv EDA HITE-C A W AUCA GL MAGNOLIA 2 . » ; $ ' is ' - , ' x i t a »b4 > LS fe i, 5 | . 1 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