1 c A 118 117' NORTH AMERICAN FAUNA No. 55 issued by the UNITED STATES DEPARTMENT OF AGRICULTURE BUREAU OF BIOLOGICAL SURVEY Washington, D. C. June 1936 MAMMALS AND LIFE ZONES OF OREGON By VERNON BAILEY, formerly senior biologist, Section of Mammalogy, Division of Wildlife Research CONTENTS Page Introduction . 1 The present study 2 Physiographic features of the State 4 Life zones of Oregon 11 Upper Sonoran Zone 12 Transition Zone 19 Canadian Zone... 25 Hudsonian Zone 29 Arctic-Alpine Zone 30 Mammals of Oregon . 54 An important natural resource 54 Annotated list of species 57 Order Artiodactyla: Hoofed mammals. .._ 57 Order Lagomorpha: Rabbits and conies. 93 Order Rodentia: Gnawing mammals 117 Mammals of Oregon— Continued. Annotated list of species— Continued. Order Carniyora: Flesh eaters 261 Order Pinniped ia: Seals, sea lions, sea elephants, and walruses 330 Order Cetacea: Whales and porpoises. .. 336 Order Insectivora: Insect-eating mam- mals 349 Order Chiroptera: Winged mammals- bats 368 Order Marsupialia: Marsupials 393 Bibliography - 391 Glossary of Indian names of mammals 403 Index... 404 INTRODUCTION In the early pioneer days of North America the mild climate, rich-soiled valleys, towering forests, and teeming animal life of the Northwest attracted many adventurous explorers, and before the fur-trapping days were over the basis had been laid for the per- manent settlements that held the Territories of Oregon and Wash- ington for the United States. The early history of Oregon is a thrilling romance, full of the stern realities of struggle, endurance, and suffering, leading to eventual victory over appalling obstacles and the development of a great State by a hardy class of people. Even after three-quarters of a century much of the area still remains as public land or is held in large tracts for grazing or lumbering, while national forests protect the best timber. Irrigation already has reclaimed many extensive arid valleys. The extensive lum- bering operations have opened up rich lands suitable for agricul- ture in parts of the valley country, while over the higher levels, on private and public land, reforestation will undoubtedly give better returns than farming. Still other great areas unsuitable for agri- culture and of little value for grazing are ideal for native game and wildlife of valuable and attractive forms. 7209°^-36 1 1 2 NORTH AMERICAN FAUNA [No. 55 The first great attraction of the State was its wildlife, game for food and clothing, and fur-bearing animals for trade and interna- tional commerce. Agriculture, mining, and lumbering came later and, with other industries, gradually absorbed the wildlife resources, which were not inexhaustible, as they seemed at first. While Oregon is still one of the leading States for hunting, there is today only a fraction of the original supply of game. Some of the most valuable species are extinct or nearing extinction, and others are in need of suitable range and food, of better protection, and a definite plan of management that will build up and insure a future supply not only of game animals but also of the many other attractive and interesting forms of wildlife that add so much to the value of any region. There are great areas of publicly owned forest lands where game is next to the timber in value and where it should always be maintained in controlled abundance. Other types of open-land game, however, are not protected by the national forests and have not been able to com- pete with the overgrazing of domestic livestock. Much of this public domain is of little or no value for any purpose other than its native wildlife, and considerable areas could well be devoted permanently to a gradual restoration of native forms, including the antelope, desert mountain sheep, sage grouse, and in more elevated ranges the blue grouse and mountain quail. Stock raising on extensive grazing ranges has been one of the chief industries over much of the State east of the Cascades, but this is gradually giving place to cultivation of the land, or to the development of a greater volume of forage so that more stock can be raised on a given area. The concentration in smaller units of both grazing and agricultural activities does not mean less produc- tion but greater returns per acre. The days of the big ranch and easy-going methods are passing. Better grades of stock and more careful management are taking their place. Application of scien- tific methods will make this, as every other branch of agriculture, more productive. A greater diversity of livestock, including some of our native game animals, may be predicted for the future, with the same advantages that other diversified types of farming have shown. Some of the native animals of Oregon that might well be domesticated or better managed for man's use are the elk, deer, antelope, bighorn, beaver, and muskrat, some of the waterfowl, the sage grouse, blue grouse, sharp-tailed grouse, and mountain quail. With the future development and progress of the industries, a fuller knowledge of climatic and physiographic conditions will be a distinct advantage. Also a more complete knowledge of the habits, distribution, abundance, and economic relations of the native animals of the State often will save losses of property and waste of time, and will prevent the destruction of harmless, interesting, and useful species. THE PRESENT STUDY The present report is based primarily on field work of the Bureau of Biological Survey, carried on through varying periods since 1888, in addition to such published information as has been found. The systematic survey of the State was begun under the direction of C. Hart Merriam, who in 1896 led in person a small field party 1936] MAMMALS AND LIFE ZONES OF OREGON 3 through the Blue Mountains, Steens Mountains, Warner Mountains, and from the Klamath region north through the Cascades to Mount Hood. Later the field work was carried on under the direction of H. W. Henshaw, and still later under E. W. Nelson, until fairly representative collections of mammals, birds, reptiles, and plants were obtained from every part of the State. The distribution of the species was thus ascertained with considerable detail and the sig- nificance of geographic variation generally explained. Valuable assistance came through the cooperation of the State university at Eugene, the Willamette University at Salem, the State agricultural college at Corvallis, Reed College near Portland, and the fish and game department of the State. The State university was represented in field work by Alfred C. Shelton, under John F. Bovard, and the university collections were made available for work- ing out species and ranges. F. V. Coville and S. F. Blake, Bureau of Plant Industry, rendered valuable assistance in the nomenclature of the plant lists. Morton E. Peck, of the Willamette University, contributed largely in general field work, especially in botany. The agricultural college collection has been drawn upon for such addi- tional material as it afforded, and the fish and game collection through William L. Finley gave every assistance possible, detailing Stanley G. Jewett, R. Bruce Horsfall, and O. J. Murie for field work, and building up a very useful collection of mammals and birds in the Reed College museum. The college museum, under the direction of Harry Beal Torrey, sent one of its student assistants, Mr. Launce- field, into the field on one of the collection trips, and also aided in every way possible with museum material. Private collectors have generously contributed to a knowledge of the State fauna. Of these, thanks are especially due to A. Brazier Howell, whose collection is now in the Natural History Museum of southern California ; H. E. Anthony, now of the American Museum of Natural History in New York ; Lee R. Dice, of the University of Michigan ; Alexander Walker, of Tillamook, Oreg. ; Stanley G. Jew- ett, long associated with the Biological Survey's game management and predatory-animal control in Oregon ; and Ira N. Gabrielson, then in charge of the Bureau's rodent control in the State, later its regional supervisor in the region that includes Oregon, and now Chief of the Bureau. The Biological Survey field work in Oregon has been carried on at various times and places since 1888 by Theodore S. Palmer, Clark P. Streator, Arthur H. Howell, Albert K. Fisher, Walter K. Fisher, J. Alden Loring, Stanley G. Jewett, Luther Goldman, Morton E. Peck, Alexander Walker, Ned Hollister, Harry H. Sheldon, Robert H. Becker, Edward A. Preble, and the writer. Some of this work has been done sporadically in connection with that in adjoining States, but all has helped. Much information and many important specimens have been obtained from the predatory-animal and rodent- control field workers in the Division of Economic Investigations of the Biological Survey formerly under A. K. Fisher and W. B. Bell and now part of the Division of Game Management under Stanley P. Young. Close and cordial cooperation with officials of the Forest Service has afforded important information on game matters and animal 4 NORTH AMERICAN FAUNA [No. 55 statistics that could not otherwise have been obtained. The infor- mation gathered from ranchmen, hunters, and others along the way has been of great value in supplementing field notes and has been used freely with credit under specific records. The natural-history studies of the Mazamas, the mountain-climb- ing club of Oregon, published in annual reports, have afforded val- uable information and have been freely drawn upon, as have the bulletins of the State university, agricultural college, experiment stations, Forest Service, Park Service, and United States Geological Survey. While the present report puts on record much that is not commonly known about animal life, it represents a beginning rather than the finished product of studies of the State's mammals. Its greatest value should be in enabling a large number of local people to observe correctly and record the habits of animals until much better under- stood than at present, to know what particular species they are observing, and to obtain definite and accurate information. Much of the animal life is a State and national asset and should be conserved and used to the greatest advantage consistent with wise use and the perpetuation of the species. In some cases this can be done only through the partial or complete control of other species of less value or of destructive habits. Only by applying the most thorough and reliable information can the wildlife of a country be managed efficiently. PHYSIOGRAPHIC FEATURES OF THE STATE The surface features of Oregon (pi. 1) show wide variation, rang- ing from coastal plains and great inland valleys to broad plateaus, lofty mountain ranges, and snow-capped peaks. Three types of geological formation stand out : The very old non volcanic crystalline or metamorphic rocks, the comparatively recent but still ancient lake- basin deposits of the great valleys, and the volcanic deposits of both ancient and comparatively recent times. VOLCANIC AREAS A great part of the State, including most of the Cascade Range and the plains to the eastward, is of volcanic origin, consisting of numerous large and small craters and great areas built up by suc- cessive flows of lava. The enormous depth of these lava flows is well shown by the sides of the Deschutes, Columbia, Snake, Grand Ronde, and Imnaha Canyons, by the Kiger Gorge and the east escarpment of the Steens Mountains (pi. 2, J.), and by many other cliffs and canyons in the State. In numerous side walls and rim- rock cliffs consecutive layers of lava, ranging from 20 to 50 feet and sometimes 100 feet in thickness, may be counted to a height or depth of 2,000 or 3,000 feet. Sometimes these form beautiful series of basal- tic columns or layers of royalite, and there are various forms of amorphous lavas, cooled and hardened as they flowed out in surface sheets (pi. 2, B), or in places as shiny black sheets of volcanic glass (obsidian). The vertical cleavage of the lava sheets produces the North American Fauna No. 55. U. S. Dept. of Agriculture, Biological Survey PLATE 2 STEENS MOUNTAINS (9,354 FEET ALTITUDE). B17230; B16313 A, East face, showing successive lava flows and permanent snow banks in head of Kiger Gorge; B, com- paratively recent flow of surface lava, near Cow Creek Lakes, southeastern Malheur Ccunty (photo- graph by Edward A. Preble, 1915). North American Fauna No. 55. U. S. Dept. of Agriculture, Biological Survey B33207; B33194 A, Steens Mountains, from near Alvord Ranch, showing east face of high part of range (July 7, 1927); B, Tumtum Lake, Alvord Valley, looking east from near base of Steens Mountains (July 6, 1927). North American Fauna No. 55. U. S. Dept. of Agriculture, Biological Survey PLATE 4 CAVES IN DESCHUTES AND HARNEY COUNTIES. A, Lava River Cave, 22 miles south of Bend; B, one of the Arnold ice caves, 20 miles southeast of Bend; C, Malheur Cave, 30 miles east of Malheur Lake. All harbor bats and contain tones of recent mammals North American Fauna No. 55, U. S. Dept. of Agriculture, Biological Survey PLATE 5 EAGLE CAP PEAK, WALLOWA MOUNTAINS. Photograph by Stanley G. Jewett, July 20, 1925. 1936] MAMMALS AND LIFE ZONES OF OREGON 5 sheer cliffs and abrupt rimrock effects so common over the eastern part of the State. The great peaks of the Cascades, from Mount McLoughlin (Pitt) and Mazama on the south to Jefferson and Hood on the north, are all old craters from which the Cascade Kange has been augmented by enormous flows of lava that reach both slopes and spread out over the valleys. While the ice-clad peaks, some of them world- famous spectacles, are of special interest in their fauna and flora and of great value as sources of water, the broad basal slopes of the range, bearing dense forests of valuable timber, are especially impor- tant in human economy. The configuration of surface, various types of erosion, color and character of soils, and to some extent, the character of forest and other vegetation forming the ground cover, are modified by the gen- eral volcanic base so widely spread over the State. The general fer- tility of the valley soils is in part due to their volcanic origin, while even the resulting dark colors are in some cases an advantage in added ability to absorb light and heat from the sun. It is well known that species of plants and animals range to higher altitudes on dark soil than on light and that other high-ranging species range lower down on light-colored soils. The Paulina, Yamsay, Yanax, and Klamath Mountains, lying east of the Cascades, are of the same volcanic type, but are scattered in lower groups or buttes. Their height reaches generally only to about 7,000 feet, but this is sufficient to give them cold upper slopes with an extra amount of precipitation and relatively heavy growths of timber. Still farther to the eastward other types of ranges rise abruptly from the desert valleys. While composed mainly of volcanic mate- rials, they appear as elongated ridges with one or both sides broken and pushed up along more or less well-defined fault lines. These include the Winter Eange, Warner and Hart Ranges, and the higher and still more striking Steens Mountains. The Steens Mountains, a boldly tilted uplift from the lava plains of southeastern Oregon, are largely volcanic from near the base to the summit. Their sharply faulted eastern escarpment rises abruptly 5,500 feet above the valley bottom, attaining a total altitude of about 9,354 feet in the highest parts (pi. 3, A). Of them Eussell (1903, p. 19)1 says in effect: The eastern slope of that splendid mountain is composed of the broken and eroded edges of sheets of basalt, which dip westward at an angle of about 3° to 4° and present an aggregate thickness of not less than 5,000 feet, while the lacustrine sediments beneath their base reach a thickness of at least 1,000 feet. Thin layers of sandstone separate some of the laval flows but even those which rest directly upon each other are easily counted in cross section and some 30 or 100 sheets, averaging about 60 feet thick, are more or less exposed in this escarpment. Deep canyons are guttered into the sides of the range, and canyon walls expose heavy stratifications of successive lava flows through which the mountains have been pushed up. At the northern end of the range several broad U-shaped canyons show evidence of glacial erosion, and several beautiful examples of hanging valleys along the 1 Citations in italic in parentheses refer to the bibliography, p. 394. 6 NORTH AMERICAN FAUNA [No. 55 west side of the Kiger Gorge tell a part of the story of the glacial period. Summer snow banks or ice beds high up on the cold slopes in the old cirques still feed many permanent streams which are cutting sharp V-shaped courses down the valley bottoms to the arid plains below (pi. 3, B). The top of the range is just an inclined section of the desert pushed up to a height where plant life is still more de- pauperate than at lower levels. The peaks are merely the jagged edges of a much-eroded ridge ^with occasional notches cut clear through by the erosive action of ice and water. Over the great arid plains both east and west of the Steens Mountains are extensive fields of black and barren lavas, poured out by numerous small and medium-sized craters. Although cold and dead now, many of these craters appear so fresh and vivid as to sug- gest comparatively recent activity. In many places the long streams of wavy and twisted lavas tempt one to feel the rough surface to see if it is still hot. To the student of geology or the tourist it is unnecessary to go to the Hawaiian Islands or farther away than eastern Oregon to study picturesque and fascinating lava fields and craters, cinder cones, or lava caves. In many of the older lava flows where the surface had hardened over a long gentle slope, the still molten interior of a fresh stream broke out below, and the liquid interior escaping, left great tunnel- like subways, some of them miles in length, below heavy roofs of solid rock. The Malheur Caves, the Arnold Ice Caves, the Skeleton Cave, the Horse Caves, and the Lava River Cave are well-known examples (pi. 4), but there are many others without name or fame. Less attractive, but not less important, volcanic features of the State are the vast deposits of pumice, volcanic ash, and volcanic sand. In places these deposits cover the rocks to considerable depths and form great plains, sandy valleys, or deep sections of canyon walls. Notable among these are the great pumice plain between Crater Lake and the Paulina Mountains, the black-sand valleys east and south of the Paulinas and in various valleys farther east, and the numerous smaller but deep deposits along both sides of the Cas- cades. Such materials have a very practical bearing1 on soil fertility and secondarily on distribution of plant and animal life. Volcanic activity in the State has practically ceased. At present Mount Hood is the only crater giving noticeable signs of remaining activity. Slight fumaroles of gas and steam occur in the old cup near the top of the peak, and at times the steam and sulphur fumes sweep over the summit in stifling gusts. No recent eruptions, how- ever, are known. NONVOLCANIC AREAS Nonyolcanic areas in Oregon are found in some of the peaks and high ridges of the Wallowa and Elkhom (or Baker) Ranges, in the Siskiyous, in most of the Coast Range country, and in the extensive lacustrine deposits of the older valleys. The higher parts of the Wallowa Mountains, while surrounded by the heavy base of lava of the Blue Mountain Plateau, are largely composed of such materials as granite, quartzite, limestone, marble, slate, and other nonvolcanic rocks. In general the topographic con- figuration resembles the Rocky Mountains, and moreover a large 1936] MAMMALS AND LIFE ZONES OF OREGON 7 number of Rocky Mountain species of plants and animals occur. The main peaks rise to sharp pinnacles, 9,000 to 9,800 feet in altitude. The highest shown on the Forest Service contour map is the Matterhorn which reaches above the 9,800-foot level. Eagle Cap (pi. 5), formerly supposed to be still higher, is given as 9,675 feet; and Petes Point and Aneroid Point near Aneroid Lake are shown as reaching above the 9,600-foot contour. The peaks are sharp and jagged, separated by steep, ice-eaten cirques and upper slopes and deeply cut canyons. Extensive fields of permanent ice and snow persist on the high cold slopes, and one small glacier still clings to the declivity between Eagle Cap and Sentinel Peak. The many glacier-hewn valleys with numerous lateral and terminal moraines and many lake beds scooped out of the solid rock are conspicuous features of the landscape. Wallowa Lake at about 4,500 feet on the northern side of the range is an especially beautiful example of a glacial scoop, deep, long, and narrow, with high lateral and terminal moraines. Higher up some of the numerous small lakes in rocky basins close to the snow banks are frozen over for the greater part of the year, but during the summer they send down torrents of ice-cold water. The Wallowa Mountains are well supplied with permanent streams that cut their way down through deep and picturesque canyons to the Snake River on the east, the Powder River on the south, and the Grand Roncle on the north. Most of the canyon walls are of basalt or other rocks of volcanic origin, but in many places on the south and east slopes the older geological formations are exposed. Some of these are rich in valuable minerals. While most of the Blue Mountain Plateau is covered with splendid forests, the higher parts of the range reach near or above timber line and are barren or but sparingly wooded. The Elkhorn (or Baker) Range, rising abruptly west of Baker City, is similar in general character to the Wallowa Mountains but slightly lower and less rugged. The highest peak, formerly known as " Rock Creek Butte " but changed by the Geographic Board of Oregon to " Hunt Mountain " in honor of Wilson Price Hunt, leader of the John Jacob Astor party in 1811 and so far as known the first white man to see the peak, is given on the Geological Survey quad- rangle as 9,097 feet in altitude. Many other points are almost as high, and the crest of the range is well above timber line, with bare peaks and upper slopes snow patched even in late summer. The high part of the range consists largely of crystalline, sedi- mentary, and metamorphic rocks, including many ore-bearing forma- tions, but the surrounding country is a part of the Blue Mountain Plateau. The Siskiyou Mountains, on the southwestern border of the State, represent one of the geologically very old land formations. They are composed largely of granite, quartz, limestone, marble, sandstone shales, and various metamorphic rocks. On the west they extend down to the coast and locally yield valuable deposits of gold and other minerals. Siskiyou Peak at 7,662 feet and Sterling Peak at 7,150 feet reach slightly above timber line on their northern slopes. The higher parts of the mountains are steep and deeply eroded, numerous long narrow spurs or ridges winding down between deep 8 NOKTH AMERICAN FAUNA [No. 55 V-shaped canyons coursed by rapid streams. In general features, as well as in plant and animal life, this region is a part of the Trinity or Klamath Mountain system of northwestern California, which also extends northward to include the Rogue River Mountains. It is a well-watered region, and except for the higher peaks and ridge tops it is generally well forested. The Coast Ranges of western Oregon, lying between the valleys of the Williamette, Umpqua, and upper Rogue Rivers, are largely parts of an elevated and much-dissected plateau, or old coastal plain, deeply eroded into flat-topped ridges with steep, and often terraced, slopes and innumerable deep V-shaped cuts and canyons between. The ridge tops range from 3,000 to about 4,100 feet in height, the highest, Chintimini Mountain, or Marys Peak, just west of Corvallis, being 4,097 feet. Both the Coast Ranges and the coastal plain are largely of sedimentary rocks — sandstones, limestones, shales, or more recent alluvial deposits. In places basalt or other igneous rocks crop out on the surface or are exposed in terraces or canyon walls. The whole region is well watered. Dense forests and rich under- growth give a well-rounded and smooth appearance and hide most of the details of surface structure. The lacustrine and alluvial deposits of the broad valleys of Ore- gon are of special importance and interest because of their rich mellow soils, easily adaptable to profitable agriculture. Most of the larger valleys, such as the plains of the Columbia east of the Cas- cades and the Snake River Valley above the Snake River Canyon, owe their deep soil to the deposits of ancient lake beds long since drained by the lowered river channels. The broad rich valleys of the Willamette, the Upper Umpqua, and the Rogue River may be old lake beds or early embayments of the ocean. Nevertheless, parts of the valley floors are constantly receiving additions of silt from the mountains, spread out by innumerable small streams. Other parts are losing their best soil by erosion. The innumerable inland-lake basins of the high plains of eastern Oregon, each with its own type and age of soil and geological depos- its, all lie within the arid area. Generally they are devoted to grazing and ranching, but eventually should include some of the best game lands of the State. DRAINAGE Drainage is of two distinct types — the river and stream drainage to the Pacific Ocean, and the inland-lake or basin drainage of the southeastern part of the State. The river drainage includes the Columbia River system, with its numerous tributaries, and the coastal streams that carry vast quantities of water from the high and humid slopes of the Cascades to the Pacific. In the more arid southeastern part of the State are many lake basins of purely inland drainage, really a part of the Great Basin area. Among the larger basins are Malheur, Harney, Alvord, Warner, Abert, and Summer Lakes, all occupying lava-encircled valleys and fed by surface waters or very limited streams from springs. Many extensive playas, or dry mud flats, occupy the bot- tom of other valleys where shallow lakes formed by rains quickly North American Fauna No. 55, U. S. Dept. of Agriculture, Biological Survey PLATE 6 1936] MAMMALS AND LIFE ZONES OF OREGON 9 dry up, leaving miles of baked, glistening mud flats. Most of the basin lakes are shallow. The shore lines of some are steadily re- ceding because of the diversion of water for irrigation. Eventually some of these lakes also will be mere playas. Lake Harney has been reduced to that state for a decade. As usual, inland drainage is the result of rainfall that is not sufficient to overflow the valleys and cut out the rims to connect with lower levels. Added to this is an arid climate in which the evaporation over a large surface of standing water more than balances the precipitation over a considerably greater drainage area. Malheur Lake, which in 1897 when it was first seen by the writer was an enormous tule swamp overflowing into Harney Lake as it did when Peter Skene Ogden first saw it in 1826, was practically dry in 1931, when buffalo skulls were collected in its baked mud bed. Overutilization of the water of streams naturally flowing into it had ruined the hay and grain ranches around the borders of this great fertile valley, lowered the water table until the valleys became a part of the surrounding desert, and destroyed one of the most important wild-fowl-breeding grounds in the State. Eecently these conditions have been corrected by addition of a considerable part of the drainage of the Blitzen River (Donner und Blitzen) to the Lake Malheur Wildlife Refuge, allowing sufficient wa- ter to reach the lake to restore it to a normal level and extent of sur- face and swampy border. The enlarged circle of moist and fertile land restores the ranch values of the valley, and 30 miles of lake and tule swamp restore the spectacular breeding and resting grounds of swans, geese, ducks, pelicans, cranes, egrets, herons, ibises, curlew, and a host of swimming and wading birds and valuable fur bearers. Goose Lake and the Klamath Lakes, on the southern border of the State, have cut outlets through the southern rim of their basins, and their waters reach the ocean through Pit and Klamath Rivers. At one time these valleys may well have been a part of the Great Basin, with which they still closely agree in climate, flora, and fauna. Lakes of a yet different type — many of them large, deep, clear, and cold — lie along the higher parts of the Cascade Range in Oregon and serve as reservoirs of snow water that is let down during sum- mer months to thirsty fields below. The best known and most spec- tacular of these, Crater Lake (pi. 6) , half fills its cuplike crater to a depth of 2,000 feet and presents a unique picture of beautiful color and form. Although the lake is without visible outlet, the water remains at a uniform level. It seems not improbable that some of the large streams that burst out below may drain the lake through underground channels in the mountain side. Other lakes owe their origin to lava dams or terminal moraines and generally form the headwaters of important streams. Still another set of lakes is that of the immediate coastal strip — old embayments or estuaries cut off from the ocean. Not much above the ocean level, they remain as land-locked bodies of fresh water held back by sand bars or dunes. Then, too, there are the prehistoric lakes such as once covered a great area in the Columbia River Valley east of the Cascades, the Snake River Valley above the canyon, the greater Malheur Valley, and the northern end of Lake Bonneville in Alvord Valley. Present 10 NOBTH AMERICAN FAUNA [No. 55 interest in these ancient bodies of water lies mainly in the rich fossil beds that here and there mark the old shore lines. Some of the " badland " formations of these old beaches bear valuable de- posits of prehistoric mammal remains that open an important chap- ter in the geological history of the State. The John Day Valley, Camp Creek, Malheur, and Owyhee Valley fossil beds are probably the best known. GLACIATION Glaciation as a type of drainage has modified to some extent the higher elevations of the State and is still slowly eating away great cirques and amphitheatres on the upper slopes of Hood, Jefferson, the Three Sisters, McLoughlin (Pitt), the Wallowa, Baker, and Steens Mountains. Ancient moraines show glacial activity much lower on the mountain slopes than at present. Generally this evi- dence does not extend into the valley country, nor is it conspicuous after the great volcanic period. Glacial lakes are comparatively few in the State, although Wallowa Lake is a beautiful example of a glacial scoop and some of the smaller lakes high up in the moun- tains owe their origin to the ice. Many, if not most, of the lakes in Oregon, however, owe their origin directly or indirectly to vol- canic activity closing up valleys or damming streams of water with streams of lava. SOIL CONDITIONS Soils and land coyer, in special cases, exert considerable influ- ence on the distribution of species. Over much of Oregon the firm, rich, dark-colored soils from disintegrated lavas are generally fer- tile and produce dense plant growth. They vary endlessly, however, in texture, in mineral composition, and in mechanical structure. At one extreme are the fine precipitates of deep-water deposits, form- ing tenacious clays, commonly called " gumbo." Waxy when wet and hard when dry, they are extremely discouraging to most bur- rowing rodents. At the opposite are the deep mellow sands, fine and nonadhesive, that form light mellow soils. These always prove a great delight to burrowers. Only very limited areas of the light, water-washed sands, such as drift and change with every wind, are found, mainly along the Columbia River Valley above The Dalles, around the shores of Harney and Alvord Lakes, and in places along the coast. In these spots the light yellow sands drift back over the river banks, lakes, and seashore in dunes and ridges for considerable distances, giving their color and character to extensive areas. While attracting or developing certain species of plants and animals, these light sands have perhaps crowded out others with different affinities. Sand dunes in the desert are favorite haunts of kangaroo rats, pocket mice, lizards, and horned toads. Another soil type favorable to burrowing species of mammals, as well as horned toads and lizards, is composed of the deep, black, loose sands and volcanic ash, espe- cially conspicuous east and south of the Paulina Mountains. This soil is attractive also to sand- and heat-loving plants. Owing mainly to soil conditions, the extensive playas of the Alvord Valley and others east of the Steens Mountains, except for brief peri- 1936] MAMMALS AND LIFE ZONES OF OREGON 11 ods after a rain or snow, are more nearly typical desert and more lifeless than any other part of the State. Such level valley bottoms without drainage can produce neither water plants, because they dry up quickly after rainfall, nor dry-land plants, because the occasional sheet of water kills them. Thus devoid of vegetation, they have an animal life limited to occasional antelope, jack rabbits, coyotes, swift foxes, badgers, and lizards that wander over them. In the more humid areas under the abundant growth of vegetation, the base soil is generally covered with rich humus of varying depths that is especially attractive to burrowing insects and a great variety of small invertebrates. Consequently this same mold-covered soil is most attractive to numerous species of insectivorous mammals and birds and holds the greater part of the shrew and mole population of the State. PLANT COVER Types of vegetation or plant associations, as modified by soil mois- ture and other local conditions, have a powerful influence on the distribution of species of animals. Next to altitude or latitude the varying degrees of humidity are most influential in determining the characteristics of these plant associations. In a general way the heaviest timber, as well as dense undergrowth, is found in the areas of heaviest annual rainfall and the lightest vegetation in the areas of lightest rainfall. The annual precipitation ranges from a maxi- mum of about 100 inches in places on the coast and in the mountains to less than 10 inches in the valleys of the southeastern part of the State. The gradual change from dense humid forest and under- growth through open forest, scattered woodlands, sagebrush, and shrubby cover to the low and scattered bunch vegetation of the desert valleys is shown in crossing the State from west to east. Most pronounced is the change following a line drawn from the northwest to the southeast corner. Coastal salt marshes, inland tule swamps, and open grasslands all have a bearing on the distribution of certain species of animal life. LIFE ZONES OF OREGON Owing to its broad extent, wide range of altitude, and varied physiographic features, Oregon shows great diversity of climate and contains 5 of the 7 primary life zones of the continent. ( See frontis- piece.) Only the hot Lower Austral and Tropical Zones are unrepre- sented. The Upper Sonoran, the arid western subdivision of Upper Austral Zone, characterized by greasewood, saltbush, and rabbitbrush, covers the low warm valleys of the State east of the Cascades, and en- ters the Eogue and Umpqua Valleys west of the mountains. The Transition Zone, characterized by the yellow pine, Oregon maple, and mountain-mahogany, occupies the higher valleys and bench lands east of the mountains and has a more humid subdivision in the val- ley foothills and Coast Kanges west of the Cascades. The Canadian Zone, the zone of spruce, fir, and lodgepole pine, covers the broad high part of the mountains. The Hudsonian Zone, the zone of the whitebarked pine, and dwarfed spruces and hemlocks near timber line, caps or surrounds the highest peaks in a narrow belt, rarely 12 NOKTH AMERICAN FAUNA [No. 55 over 1,000 feet in vertical extent. The Arctic- Alpine Zone, of very limited extent, caps most of the highest peaks well above all timber growth and includes the dwarf alpine vegetation and a very few species of birds and mammals. Tables 1 to 8 (pp. 31 to 53) show the life-zone distribution of the mammals, reptiles, birds, and plants of the State. UPPER SONORAN ZONE The western arid division of the transcontinental Upper Austral Zone covers most of the Columbia and Snake River Valleys of eastern Oregon, and about half of the higher sagebrush plains area of the State east of the Cascade Range. This part of the zone, with a very limited rainfall and fairly uniform climate, can be treated as a part of the arid Upper Sonoran, with many of the characteristics of the Great Basin area, although the Columbia River Valley with slightly more rainfall shows some peculiarities of note and a part of it could be treated as belonging to the semiarid subdivision of the zone. West of the Cascades limited areas of the zone are found in the upper Rogue and central Umpqua Valleys. There is a narrow strip along the Klamath River on the southern border of the State, and east of the range a limited area occurs near the Klamath Lakes. These semiarid valleys are marked by plants, birds, and mammals that range mainly in northern California and clearly belong to the California Valley subdivision of the zone. SEMIARID DIVISION OF UPPER SONORAN ZONE In the California Valley division of Upper Sonoran Zone in the Umpqua, Rogue, and Klamath River Valleys the base level is low, about 500, 1,200, and 2,000 feet, respectively. Only a narrow upper edge of the zone shows in these valleys ; in the Umpqua Valley over the flats and warm slopes in the Roseburg section, east of the Coast Ranges, from 500 up to 1,000 feet; in the Grants Pass and Ashland part of the Rogue River Valley on the open bottoms and warm slopes from about 1,200 to 2,000 feet; and in the Klamath River Valley from about 2,000 to 3,000 feet on the warm exposures. This is below the Klamath Canyon which cuts off the zone from its higher and more arid division around the Klamath Lakes. In all of these valleys the Upper Sonoran elements are largely mixed and blended with Transition species from higher levels, as inevitably occurs in so nar- row a zone border, but still with sufficient character to indicate im- portant climatic conditions favorable to southern species as well as some of the less hardy crops. In these valleys are found the California jack rabbit, Rogue River kangaroo rat, brown-footed wood rat, California meadow mouse, white-toothed pocket gopher, gray fox, ringtail, Pacific pale bat, and such birds as the valley quail, long-tailed jay, brown towhee, house finch, bush tit, and long-tailed chat. The plants that indicate the zone in these valleys are found mainly on the warm slopes and open flat country, while on cool or shaded 1936] MAMMALS AND LIFE ZONES OF OREGON 13 slopes a far greater number of Transition Zone species generally occur. Those most conspicuously indicating Upper Sonoran are sev- eral species of CeanotJyus (cuneatus, integerrimus, sanguinem) , man- zanita (Arctostaphylos viseida), bitterbush (Purshia Pridentata) , birch-leaved mahogany (Cercocarpus "betulaefolius), syringa (Phila- delphia gordonianus) , cherry (Prunm subcordata), silktassel-bush (Garry a fremonti), skunk bush (Rhus trilobata and diversiloba) , serviceberry (Amelanchier florida and pallida), lupines (Lupinus ore g 'onus pusttlus and subsericeus) , wild licorice (Glycyrrhiza lepi- dota and glutinosa), Hosackia (Lotus), several species, rabbitbrush (Chrysothamnus nauseosus) , and a great number of grasses and her- baceous plants. A few of these species extend northward into the Williamette Valley, indicating an approach in climate to the Upper Sonoran Zone, but not in sufficient numbers of species or abundance of individuals to warrant mapping even the warm slopes of the valley as other than Transition. In the Columbia River Valley east of the Cascades the climate is slightly warmer and more humid, with greater rainfall in winter, than over the Great Basin area farther south and east. Consequently the fauna and flora are somewhat peculiar, as shown by the follow- ing species: Townsend's ground squirrel, northwest pocket mouse, Dalles and Columbia pocket gophers, Scheffer's mole, and little canyon bat. There is generally a greater abundance of grass with a considerable number of other plants not found over the rest of the zone in eastern Oregon. Certain crops are also raised follow- ing the winter rainy season, without irrigation but through dry- farming methods and careful tillage. As a new country becomes settled and the best of the land is brought under cultivation, the native species of plants and animals are eradicated or supplanted by those introduced from other coun- tries, and even the stock range is so overgrazed as to destroy much of the original type of vegetation. It becomes increasingly more diffi- cult to define the life zones. But fortunately over most of Oregon there is still sufficient native life to give a good index to long-estab- lished climatic conditions. The practical value of this knowledge of life zones becomes apparent when a new valley, plain, or slope is brought under culti- vation and the question arises as to crops, fruit, or stock best adapted to its climate. In long-cultivated valleys these questions generally have been answered, although often by costly failures. Now expe- rience shows that the successful products of one valley may be safely extended into another having satisfactory indications of the same or closely similar native fauna and flora. In other words the study and careful mapping of life zones gives a practical aid to agricul- ture as well as a guide to management of wildlife resources. It would not be wise to try to restock the desert ranges of eastern Oregon, once inhabited by the rimrock mountain sheep, with Canadian Zone animals from the high Rocky Mountains, but any of the Upper Sonoran desert forms from Nevada, southern California or Arizona would thrive on these low ranges and canyon walls. Restocking and building up a depleted game supply will require careful consideration of life-zone conditions. 14 NOBTH AMERICAN FAUNA [No. 55 EXTREME ARID DIVISION OF UPPER SONORAN ZONE One is impressed by the apparent nonconformity of the elevations of the Great Basin division of Upper Sonoran east of the Cascades over different parfe of the State. These variations, however, in- volve well-known and long-recognized principles of climatic con- trol of distribution. The actual altitudinal limits of zone levels are known to vary considerably with direction and steepness of slope exposure, elevation of base level, aridity, type of prevailing winds, and other less-apparent factors of modification, but the long-estab- lished fauna and flora serve as the most reliable index to zone level of any point as determined by average climatic conditions. For in- stance in the Columbia Eiver Valley with a base level of 100 to 300 feet, the Sonoran Zone extends from the bottom of the valley up to about 2,000 feet on cold northerly slopes, lower on steep, and higher on gradual slopes, and to about 3,000 feet on warm southerly slopes. With a higher base level of about 1,000 feet at the junction of the Grand Ronde River with the Snake River near the northeast corner of the State, the Sonoran Zone extends up to about 3,500 feet on warm slopes in the Grande Ronde and Imnaha Canyons. Still farther up in the Snake River Valley with a base level of 2,150 feet at Ontario, the upper limits of the zone run correspondingly higher, while in the extensive lake-basin valleys of the Malheur, Warner, Abert, and Summer Lakes sections, with base levels of 4,100 to 4,500 feet, the upper limits of the zone reach to approximately 4,500 feet on north- erly and 5,000 feet on southerly slopes. The actually coldest points of slope exposure are northeast and the warmest southwest, as pointed out long ago by Merriam (1890, pis. /-//, following index). Thus the elevation of base level in eastern Oregon is shown to raise the upper limits of the zone in higher valleys fully 2,000 feet by simply holding up the absorbed and radiated heat of the sun's rays to a fairly uniform distance above the surface where they fall upon the earth. Other zone levels are modified in the same manner and by many other generally recognized factors of climate and distribu- tion, but the Upper Sonoran of eastern Oregon most admirably illus- trates the general principles of zone modification by change of base level. A somewhat detailed knowledge of the plant and animal life of a region is necessary for the recognition and full understanding of the lire zones in the field. The colored map is at best but a feeble guide to the actual areas which are far more detailed and graphic when spread before one in the garb of their native plant and animal life. MAMMALS In eastern Oregon the Upper Sonoran Zone is clearly indicated by the presence of black-tailed jack rabbits, little speckled and gray ground squirrels (CitellMs townsendii, vigilis, and canus), the ante- lope squirrel, desert wood rat, Oregon grasshopper mouse, silky cliff mouse, large-eared harvest mouse, several species of pocket mice (Perognathus parvus, lordi, Columbian^ and mollipilosus) , five-toed kangaroo rats, several species of pocket gophers (Thomomys town- 1936] MAMMALS AND LIFE ZONES OF OREGON 15 sendii, nevadensis, coliAnibianus, and quadratus], the desert fox, a little spotted skunk, and several species of bats. It has long been the winter range of the antelope, mountain sheep, and mule deer. BREEDING BIRDS The Upper Sonoran Zone is characterized by such breeding birds as the cinnamon teal, white-faced glossy ibis, black-necked stilt, mourning dove, burrowing owl, Arkansas kingbird, ash-throated flycatcher, Say's phoebe, Bullock's oriole, western lark sparrow, sage sparrow, Brewer's sparrow, long-tailed chat, catbird, rock wren, canyon wren, and long-tailed chickadee. REPTILES This zone is further characterized by such reptiles as the Oregon rattlesnake (Crotalus confluentus oreganws and Iwtosw) Heermann's and desert gopher snakes (Pituophis catenifer heermanni and deserti- cola), western striped racer (Coluber taeniatus), western collared lizard (Crotapkytus collaris baileyi), leopard lizard (0. wislizenii) , western brown-shouldered uta (Uta stansburian^i) , sagebrush swift (Sceloporus graciosus), two horned toads (Phrynosoma douglassii and platyrhinos) , and the desert whip-tailed lizard (Cnenddophorus iessellatus) . The greater number of species as well as individuals of reptiles of the State are found in Upper Sonoran Zone, a smaller number in Transition Zone, and practically none in higher zones. PLANTS The plant life characterizing the Upper Sonoran Zone east of the Cascades is largely of desert types, among which desert shrubs are most conspicuous. Along the river valleys the hackberry (Celtis dowglasii) , a few willows (Salix amygdalcndes and argophylla) , and wild currants (Ribes awewn) are common, and over the dry slopes are found a few junipers (Juniperus occidentalis} , which, with the bitterbush (Purshia tridentata) and sagebrush (Artemisia tridenta- ta) , reach into the Transition Zone above. Other conspicuous plant indicators of the zone are greasewood (Sarcdbatus vermiculatus) , saltbushes (Atriplex canescens, nuttallii and conferti folia), woolly sage (Eurotia lanata) , Dondia depressa, Grayia spinosa, Tetradymia canescens and spinosa, Artemisia pedata, douglasii, and dracuncu- loides, rabbit brush (Chrysothamnus nauseosm and viscidiflorus] , wild sunflower (Helianthus annmvs), serviceberry (Amelanchier utahensis), sumac (Rhu£ glabra occidentalis) , Mentzelw albicaulis and laewcaulis, wild tobacco (Nicotiana attenuata), little bluebon- nets (Lupinus brevicaulis, laxiflorus, mediwn, mollis, ornatus, saxosus, and others), prairie clover (Psoralea lanceolata scaora), licorice root (Glycyrrhiza lepidota), plantain (Plantago pwsliii), yellow caper (Cleome lutea), sand dock (Rumex venosus), sandverbena (Abronia mellifera) , wild sage (Ramona incana) , low evening primrose (Pack- ylophus canescens), alfileria (Erodium ricutarium) , ricegrass (Ory- zopsis hymenoides). (See also p. 40.) 16 NORTH AMERICAN FAUNA [No. 55 Many of these plants are dominant species over special areas and not only give color and character to the desert but have important value as forage, cover, windbreak, shade, conservers of soil and moisture, or shelter for birds and mammals. So much is said of the sagebrush and the " sagebrush country " that a word of explanation seems necessary. The name is well fixed by long usage and well defined, but the plants have no rela- tion to the real sages (Salvia) and other pungent mints. The sage- brushes are all shrubby wormwoods of the order Compositae, silvery- leaved desert shrubs, strongly and pleasantly aromatic, intensely bitter to the taste, and many of them beautiful and graceful little shrubs or diminutive desert trees. A pure stand of the commonest of the sagebrushes (Artemisia tridentata) growing over a rich-soiled but arid valley, makes a beautiful display of silvery gray-green and feathery foliage, and a single bush by itself, 2 to 6 feet high, is a perfect diminutive tree that might grace the rarest garden (pi. 7). There are half a dozen distinct species — Artemisia tridentata, angustifolia, trifida, arbuscula, cana, borealis, pedatifida, spinescens, and some others — all true sage- brushes. They are not good forage plants or they would have dis- appeared years ago, but in the absence of all other food sheep will live on them for a short time and often browse them severely. Sage hens will eat the leaves when other food is scarce, and even antelope and jack rabbits will nibble them at times. These bushes shade the ground and hold the snow, build up humus, bind the soil, conceal the sage grouse and young antelope, and provide choice fuel for the camp fire. Their* pleasant odor is one of the charms of the desert, and the smell of a dried spray brings back the memory of broad valleys and clean wholesome air. The sagebrush has no direct com- mercial value, but without it or an equivalent, the desert would be poor indeed. The rabbitbrush, or golden sage, of the genera Chrysothanwius and Tetradymia,, are often the dominant shrubby growth over part of the valley country of eastern Oregon, giving a golden glow to the vege- tation during the season of flowering or at other times a fine feath- ery gray from the slender leaves and stems. In either leaf or flower they are graceful and attractive plants and besides the important function of giving cover and protection to the soil they serve as shelter and to some extent as food for the animal life. They belong to the same family as the sagebrush and goldenrods. Each has its own peculiar taste and odor, some rank and repellent, others aro- matic and pleasing. The odors of the desert vegetation are as strik- ing as its color and form and to an old inhabitant are among the great attractions of desert life. Of the true greasewood only one species, Sarcobatus vermiculatus, comes into Oregon. It is abundant in alkaline valley bottoms and often the dominant shrub, giving its shiny bright-green color to miles of alkali-incrusted playa border or the saline shores of basin lakes. It grows where water is abundant not far below the surface and where most other plants cannot endure the mineral carried in the water. The abundant fleshy and juicy leaves, borne on the spinescent twigs, are soft and rounded, like so many smooth green caterpillars, hence the name vermiculatus. They are also very salty North American Fauna No. 55. U. S. Dept. of Agriculture. Biological Survey PLATE 7 m B16314; B A, Hay ranch at Cow Creek Lakes, in typical sagebrush and stock country, in the arid southeastern part of the State (photograph by Edward A. Preble, July 8, 1915); B, irrigated ranches in Owyhee Valley, near Rome, Oreg., where alfalfa is the chief crop on the ranges for grazing cattle and sheep (photograph by Laura A. Mills, July 3, 1927). North American Fauna No. 55, U. S. Dept. of Agriculture. Biological Survey PLATE 8 B 16300; B 16330 A , Typical rimrock valley, White Horse Creek, southeastern Oregon (photograph by Edward A. Preble, June 17, 1915); B, camp of Biological Survey collector (Mr. Preble), in southeastern Oregon, under the junipers, where even a little shade is grateful. 1936] MAMMALS AND LIFE ZONES OF OREGON 17 in flavor but not unpleasant in taste and are generally eaten to some extent by sheep and other stock. The bushes are so very spiny, however, that only the tender tips are browsed off. Many other plants are wrongly called greasewood where the true Savoo$atu8 does not occur, but the name should not be used for any other bush. Dondia, or Suaeda, and Salicornia (samphire) are closely related to the greasewood and have somewhat the same habits. They are even more addicted to salt and alkaline ground and even more strongly impregnated with salt and soda. The saltbushes, several species of shrubby Atriplex including canescens, confer tifolia, patwa, nuttallii, and a number of herba- ceous species, are generally common over the desert Sonoran valleys and in places give a dominant character to the low vegetation. They generally indicate the presence of a little salt or alkali in the soil, and the leaves have a not unpleasant saline taste. Generally they are good forage plants and hence are often entirely eradicated over val- leys that are overgrazed. A. confertifolia with its abundant spines- cent twigs is the least likely to be destroyed by overgrazing. Woolly sage, the beautiful silvery white little shrub, Eurotia tanata^ called by the sheep herders " winterf at ", is one of the most valuable forage plants of the desert. Being so desirable as winter forage and so unprotected it is practically exterminated over most of its range, except at such long distances from water that stock cannot get to it A few scrubby junipers are found in the canyons and on steep slopes but rarely in extensive stands where accessible for ranch use. Their shade is often grateful and their fragrant wood is prized as camp fuel in the foothills and rim-rock canyons (pi. 8). Weeds, those hobos of the plant world and the pest of the farmer, have few friends or defenders. Out in the deserts of eastern Ore- gon, however, they seem to have found a use. Where sheep have eaten everything but the lava rocks and killed out all the native plants, even the sagebrush and cactus, the little exotic mustards, chickweeds, pennycress, tarweeds, prickly lettuce, foxtail, and brome- grass have volunteered to clothe the nakedness of the soil and in many places have bravely succeeded. Over great areas the little seeds of these weeds are the only available food for pocket mice, kangaroo rats, and other small rodents. These plants, too, are the principal food for thousands of sheep. In 1927, in Klamath Valley the county agent reported a flock of 100,000 sheep, pastured all summer entirely on foxtail and China lettuce, that yielded thousands of fat lambs for market. The cash value of weeds' to eastern Oregon would amount to a high figure if it could be estimated, although insignificant compared with the value of native vegetation destroyed by overgrazing. CROPS FOR UPPER SONORAN ZONE IN EASTERN OREGON While arid and much of it unsuited to agriculture because of rough surface or lack of available water, eastern Oregon contains many extensive valleys of rich, mellow soil, with ample water supply for local irrigation. The Columbia Kiver Valley, including the Des- 7209°— 36 2 18 NORTH AMERICAN FAUNA [No. 55 chutes and John Day Valleys, with an enormous extent of rich land, is being rapidly brought under irrigation. The Snake River Valley, including in Oregon the Malheur and Owyhee River drain- age valleys, still largely undeveloped, has a great agricultural future. The northern part of Malheur Lake Valley, including the inland drainage of the Silvies River and Silver Creek, with rich soil and good water has grown into a prosperous agricultural section. In many other valleys small streams and large springs provide water for ranch purposes and livestock centers, while others are used largely by game. These conditions obtain in the valleys of Warner, Goose, Abert, and Summer Lakes, with their limited water supply, and in many smaller isolated valleys over eastern Oregon. The Klamath Valley section with ample water for its rich-soiled valleys is just awakening from the lethargy of the old days of scattered grazing to its possibilities in terms of industries and inten- sive agriculture. Practically all of these valley and basin areas of eastern Oregon lie within the limits of Upper Sonoran Zone, with mild climate and open winters. There is, however, one great disadvantage that cannot be ignored without serious danger of losses and failure. The exces- sively dry climate of this part of the State during the summer causes occasional frosts at intervals during the growing season, and the irregular frosty nights often destroy flowers, young fruit, or the leaves of tender crops that would otherwise prove profitable. The climate is mild, the growing season is long, and the summer days are hot, but superdried air loses its heat so quickly that a sharp frost at night may follow a hot day in summer. As is well known, it is the moisture in the air that retains and equalizes the heat from the sun's rays, for excessively dry air has little power of retaining heat. This frost danger has greatly restricted the agricultural value of much of the arid interior of the country, especially that lying at eleva- tions above 4,000 feet, and while many hardy and frost-resistant crops and vegetables can be raised with partial success, the section is generally devoted to stock raising, or has been until much of it, over- stocked and overgrazed, no longer produces a food supply to make this industry profitable. Originally this arid interior when fully stocked with native game and teeming with wildlife was the hunting ground of numerous bands of Indians, who made little impression upon the game until horses and firearms were introduced among them. Now the game is scarce and scattered and some of the original species are gone past recall, but great areas in eastern Oregon are still better adapted to game production than any other industry and could with practical advantage be utilized for such purposes. Owing to their low altitude and greater moisture, the immediate valleys of the Columbia and Snake Rivers are comparatively free from the danger of serious frosts. The higher and drier basins, even with the same fauna and flora, must be carefully watched and studied. In the Rogue and Umpqua River Valleys west of the Cascades, where the proximity to the Pacific Ocean affords a greater moisture content to the summer atmosphere, the danger from frost is not notice- able. Here fruits and tender crops of the Sonoran Zone are produced in their perfection. 1936] MAMMALS AND LIFE ZONES OF OREGON 19 These critical frost conditions apply not only to eastern Oregon but to a more extensive area of the Great Basin, involving parts of eastern California, Nevada, Utah, and southern Idaho. They must be understood if the area is to be developed to its best possibilities. Detailed information on climate and crop conditions, on recom- mended farm practices, and on suitable crops for the various sections of Oregon can be obtained in publications of the United States De- partment of Agriculture and of the Oregon Agricultural College. TRANSITION ZONE The Transition Zone, as the name implies, lies between the Austral, or Sonoran Zone to the south or at lower altitudes, and the Canadian Zone to the north or at higher elevations. It derives a part of its fauna and flora by the overlapping of species of the lower and higher zones. In Oregon and the Pacific Northwest generally, it is unusu- ally broad and well defined with many restricted species of its own. In Oregon the zone may be divided into four well-marked subdivi- sions based on different degrees of humidity, varying from an annual precipitation of approximately 100 inches down to 10 or 15 inches. The humid division lying west of the Cascades is characterized gen- erally by heavy forests of pine, hemlock, Douglas fir, western hem- lock, and many Abroad-leaved trees (pi. 9) . Along its western edge lies the narrow coast strip, rarely more than a few miles in width, extend- ing from southwestern British Columbia to northwestern California and well marked by the Sitka spruce and accompanying species of plants and animals. Along the eastern side of the Cascades and over the Blue Mountain plateau with a much reduced rainfall, the semiarid or semihumid division of the zone is characterized by open forests of yellow pine (pi. 10, A). On the high plains and plateaus of the southeastern part of the State the more arid division of the zone is devoid of real timber and characterized by mountain-mahog- any (pi. 10, #), sagebrush, and the broad-leaved balsamroot. Al- though blending into each other, these subdivisions of the zone must be treated separately to be understood and recognized. COAST STRIP OF TRANSITION ZONE The coastal strip, or fog belt, as it is sometimes called, gets the first sweep of the damp, cool, but never very cold ocean winds. It has a remarkably even climate throughout the year, with an annual rainfall of 80 to 100 inches. While almost free from frost in winter, it is cold and damp in summer, thus allowing an unusually even temperature with an almost complete overlapping of Transition and Canadian Zone species. It has been mapped first as one zone and then the other, but the best authorities acknowledge it to be a mixture or overlapping of the two. To the southward the rainfall decreases slightly, and south of the mouth of the Coquille River the shores are steeper, more abrupt, and consequently drier and slightly warmer. Hence a considerable num- ber of California plants extend up the coast as far as the Coquille and not beyond. On plants alone Peck (1925a, p. 35) divides the strip at this point but the subdivision is not strongly marked in other forms of life. 20 NOETH AMERICAN FAUNA [No. 55 MAMMALS Aside from seals, sea lions, and sea otters, the mammals that can be considered closely associated with the coast strip are few and only very local subspecies, such as two forms of pocket gophers (Thomomys hesperus and helleri), a meadow mouse (Microtus cali- fornium angusticeps) , and possibly a shrew (Sorex paeificus yaqui- nae) . In general, it is occupied by the humid Transition Zone spe- cies of land mammals. BIRDS Of birds, the Pacific wren tit and a song sparrow may be charac- teristic; and the tufted puffin, pigeon guillemot, California murre, several cormorants, and the black oyster catcher are shore or island breeders along the coast. However, the strip is too narrow to restrict many of the free-ranging species such as birds and mammals. A close study might show a considerable number of reptiles, insects, and mollusks. PLANTS For most of the coast strip, the Sitka spruce, the most contorted form of Pinus contorta, and the Port Orford cedar are the dominant forest trees, but many others not restricted to it enter from the adjoining humid Transition or from the higher Canadian Zone. Western hemlock, lowland white fir, Douglas fir, western yew, and Sitka willow are abundant in the fog belt. They also have a wider range well up into the Cascades. The salmonberry, salal, evergreen blueberry (V actinium ovatum), California rhododendron, sweetgale, and Baccharis pillulairis are all common in this narrow belt, showing a mixture of southern and northern species. Of mosses, lichens, and other low forms of plant life, a long list of restricted varieties may be expected. The low beach plants such as Lupinus littoralis, Polygonum pa- ronychia, Abronia latifolia, Fragaria chiloensis, Convolvulus solda- nella^ and many others indicate an association of light- and sand- loving species, somewhat apart from the shaded forest belt and possibly of more southern origin. The sphagnum bog plants, in or just back of the forested coastal strip, are mainly northern species, such as Oxytioccus intermedius, Kalmia glauca, Myrica calif omica, Gentiana sceptrum, Eriophorum chamissonis, Drosera rotundifolia, and many others that have only a secondary relation to the life conditions of the fog belt. HUMID DIVISION OF TRANSITION ZONE The humid division covers a wide extent mainly of forested country from the coast strip east to the middle-west slopes of the Cascades in Oregon. In altitude it reaches from sea level up to 3,000 and 4,000 feet, respectively, on the cold and warm slopes of Mount Hood, and to approximately 5,000 feet all around Mount McLoughlin (Pitt). The upper edge of the zone varies between these extremes of altitude along both sides of the mountains accord- ing to high or low base level of the adjoining valleys. The degree of humiditv to which this subdivision of the zone owes most of its characteristics varies from an average annual pre- North American Fauna No. 55, U. S. Dept. of Agriculture, Biological Survey PLATE 9 HUMID TRANSITION ZONE TIMBER. Coast mountain section, Tillamook County (photograph by Alex Walker). North American Fauna No. 55, U. S. Dept. of Agriculture, Biological Survey PLATE 10 A, Yellow pine timber of the Transition Zone, Blue Mountains, near Canyon City (June 26, 1915)- B mountain-mahogany, Transition Zone, Lake County (photograph by Stanley G. Jewett). North American Fauna No. 55. U. S. Dept. of Agriculture. Biological Survey PLATE 11 B20374; B33204 WHERE TIMBER LINE REACHES ITS LOWEST LIMITS. A, Mount Hood, 11,255 feet; B, Mount Jefferson, 10,523 feet; both views on cold slopes, from the northeast. North American Fauna No. 55, U. S. Dept. of Agriculture, Biological Survey PLATE 12 MIDDLE SISTER. OF THE THREE SISTERS PEAKS (10,029 FEET). Photographed from the northwest June 26, 1923, by Alex Walker. North American Fauna No. 55, U. S. Dept. of Agriculture, Biological Survey PLATE 13 North American Fauna No. 55, U. S. Dept. of Agriculture. Biological Survey PLATE 14 MOUNT MCLOUGHLIN. FORMERLY MOUNT PITT (9,493 FEET). View from the southeast across lower end of Klamath Lake, showing approximate levels of the life zones. 1936] MAMMALS AND LIFE ZONES OF OREGON 21 cipitation of 40 inches in the Willamette Valley to 80 inches near the coast and along the upper slopes of the Cascade Range. The greater part of this heavy precipitation occurs during the winter months, when the mountains are being heavily laden with the deep snows that lie late into the spring and in higher zones remain throughout the summer. This abundant supply of water is shown in the magnificent forest growth along the sides of the mountains and toward the coast where the moisture is in still greater abundance. The warmer and drier Willamette and other valleys are conspicu- ously less-heavily forested and better adapted to general agriculture. MAMMALS Some of the characteristic mammals of the humid Transition Zone of Oregon are Roosevelt's elk, Columbian black-tailed deer? Oregon white-tailed deer, Washington rabbit, Oregon brush rabbit, silver gray squirrel, Douglas's squirrel, Townsend's chipmunk, Douglas's ground squirrel, Oregon flying squirrel, dusky wood rat, ruddy deer mouse, California red-backed mouse, tree mice (Phenacomys longi- cawlus and silvwola), white-footed phenacomys, Townsend's and gray-tailed meadow mice, Oregon creeping mouse, mountain beavers (Aplodontia rufa and pacifica), jumping mouse Zapus princeps trinotatus] , pocket gophers (Thomomys bulbivorus, oregonus, and niger), and northwest coast bobcat (Lynx fasciatus). BIRDS Some of the breeding birds of humid Transition Zone are : Sooty grouse, Oregon ruffed grouse, band-tailed pigeon, California pygmv owl, Harris's woodpecker, northern pileated woodpecker, Lewis s woodpecker, Vaux's swift, Steller's jay, Townsend's warbler, west- ern winter wren, California creeper, Oregon chickadee, chestnut- backed chickadee, wren tit, western golden-crowned kinglet, and black-headed grosbeak. PLANTS The abundant vegetation of this division of the zone is to a great extent peculiar to the Pacific slope and of species that range from western British Columbia to northwestern California. The princi- pal forest trees are sugar pine, Willamette pine, Jeffrey pine, nar- row-cone pine, Douglas fir, western hemlock, lowland fir (Abies (grandis), noble fir (Abies nobilis}, white fir (Abies concolor, includ- ing lowiana) , incense cedar, western red cedar, Oregon yew, Oregon maple, vine maple, Oregon alder, mountain alder, black cottonwood (Populus trichocarpa) , tanbark oak, Oregon white oak, California oak, western chinquapin, Oregon ash, madrone, California laurel, cascara, western dogwood, Oregon crab apple, and black hawthorn. The more characteristic shrubs are California hazel, wild cherry, manzanita, Oeanothus thyrsiflorus and integerrimus, Garrya ellyp- tica, mountain-laurel, salal, purple elderberry, devilsclub, red blue- berry, evergreen blueberry, salmonberry, and thimbleberry. Some of these humid Transition Zone species run more or less irregularly along the middle-eastern slope of the Cascades where the low sum- mit of the range allows considerable rain to pass over, but their main abundance will be found on the west slope. 22 NOKTH AMERICAN FAUNA [No. 55 SEMIARID TRANSITION ZONE The semiarid (better called semihumid) division of the Transi- tion Zone as marked by the yellow-pine forests covers the broad basal slopes east and south of the Cascades and the extensive plateau levels of the Blue Mountain section. Its breadth and altitude vary with the configuration of the land, base level, and slope exposure. On the northeast slope- of Mount Hood the Transition Zone reaches from about 1,000 to 3,000 feet in altitude, although but a short distance west of The Dalles (near Mosier) it comes down to the banks of the Columbia River at less than 100 feet above sea level where the cool, moisture-laden winds from the west come up through the river gorge. On the southwest slope of Mount Hood the zone extends from the broad bottom of the Willamette Valley up to about 4,000 feet near Government camp but does not cross over the crest of the range so as to encircle the mountain completely (pi. 11, A). On Mount Jefferson it reaches up to approximately 3,500 feet on cold slopes and to 4,500 feet on warm southwest slopes, showing a slight rise in altitude with slightly raised base level on both sides of the range (pi. 11, B). In the vicinity of the Three Sisters Peaks, with a base level of about 3,000 feet on the east and 1,000 on the west, the zone reaches up to about 4,500 feet on northeast slopes and about 4,800 on south- west slopes, although the zone does not reach to the actual base of the peaks nor cross over the crest of the range north or south of them (pi. 12). Mount Thielsen (pi. 13) and Crater Lake are more nearly in the zonal position of the Three Sisters, mainly above the Transition and passing through Canadian and Hudsonian Zones. In the Klamath section, with Mount McLoughlin (Pitt) as the highest center, and with base levels of 4,200 feet at Klamath Lake, 3,000 feet in the Klamath River Canyon to the south, and 1,400 feet in the Medford section of the Rogue River Valley on the west, the Transition Zone extends up to approximately 5,000 feet all around Mount McLoughlin (pi. 14). On the southwest slope it reaches from about 2,500 feet, east of Medford, to 5,000 feet on the west base of the mountains, while on the Klamath Valley side it runs from the level of Klamath Lake up to about the same altitude, 5,000 feet, on the northeast slope of the peak. In the Klamath coun- try there is no lower limit of the zone shown on any northeast slope as the Sonoran Zone occupies only the valley bottoms and warm slopes. In the Klamath Canyon directly south of McLoughlin, Transition Zone comes down to 3,000 feet on local cold slopes and to about 4,000 feet on local hot slopes, but this deep, narrow canyon shows all the complications of such types of country. In the broad expanse of comparatively low country stretching north from Fort Klamath and the Klamath Marshes to the Paulina Mountains, where Transition Zone would naturally be expected, the plant and animal life show a predominance of Canadian Zone species, due to local influences, as noted under Canadian Zone (p. 25). In the Blue Mountain section, Transition Zone on the Columbia River Valley side extends on northeast slopes from about 2,000 to 1936] MAMMALS AND LIFE ZONES OF OREGON 23 4,000 feet; on the Snake River Valley side on northeast slopes from about 2,800 to 4,800 feet ; and on southwest slopes from about 3,500 to 5,500 feet. On the south side of the mountains, with a higher base level, the zone extends on southwest slopes near Burns from about 4,500 feet up to 5,500 feet in the mountain north of there, and on especially steep, dry slopes up to 6,000 feet. Despite the varying levels of this division of the zone, the climatic conditions are fairly uniform with an average annual rainfall of approximately 20 inches, and it is sufficiently cool to allow generally a fair depth of snow on the ground for several of the winter months. Apparently the only climatic distinction from the treeless arid sub- division of the zone is the slightly greater humidity and the resultant difference in plant and animal life. MAMMALS Of mammals some of the most characteristic species of the semi- humid Transition Zone are the Rocky Mountain mule deer, Rocky Mountain elk, Klamath chipmunk, yellow-bellied chipmunk, Oregon and golden-mantled ground squirrels, Gambel's white-footed mouse, brown pocket gopher, and others less restricted to the division. BIRDS Of breeding birds the semihumid division of Transition Zone is characterized in part by Richardson's grouse, pygmy owl, MacFar- lane's screech owl, Rocky Mountain hairy woodpecker, white-headed woodpecker, western wood pewee, Oregon towhee, mountain tanager, Audubon's warbler, and pygmy nuthatch. PLANTS The semihumid division of Transition Zone is best characterized by the ponderosa pine, generally growing in clean open forests of great beauty and value. These forests reach their greatest perfection in the Upper Deschutes and Klamath country, but are also well devel- oped over much of the Blue Mountain Plateau. Other characteristic trees of the division are the western tamarack (Larix occidentalis) , western birch (Betula fontinalis), and many willows along the streams. The shrubby vegetation is represented by the bitterbush (Purshia tridentata), squawcarpet (CeanotJius prostratus) , buck- brush (Ceanothus velutinm) , snowberry (Symphoricarpos racemo- sus), bearberry (Arctostaphylos uva^ursi), and barberry (Berberis repens) . ARID TRANSITION ZONE The arid subdivision of Transition Zone in eastern Oregon covers the high valleys, plateau tops, and lower mountain slopes of approxi- mately the southeastern quarter of the State. It includes the moun- tains and plateaus east of Goose and Summer Lakes and south of the Blue and Maury Mountains, among which the Steens and Warner Mountains are the highest. In flora and fauna it is essentially a part of the Great Basin division of the zone, too arid for timber growth, with an average annual rainfall below 15 inches. 24 NORTH AMERICAN FAUNA [No. 55 The Steens Mountains, typical of the Great Basin type of arid ranges, are practically devoid of timber and show much distorted zone levels. Owing to the high base level of approximately 4,000 feet on the east side and 4,500 feet on the west side of the range, the zones are pushed to unusual heights. Transition Zone, as nearly as it can be defined, reaches from about 4,200 to 6,000 feet on the northeast slopes and from about 5,000 to 7,000 feet on the southwest slopes. On the very steep eastern slope of the range there is much crowding and overlapping of the zones, and a general narrowing of Transition and Canadian. MAMMALS, BIRDS, AND PLANTS The mammals most characteristic of the arid Transition Zone are, or have been, the desert mountain sheep, Rocky Mountain mule deer, Idaho rabbit, woodchuck (Marmota flaviventris avarcti , and pygmy mouse (Microtus pcmpemmus). Its characteristic birds are the sage grouse, Brewer's sparrow, green-tailed towhee, and sage thrasher. It is practically treeless except for the low mountain-mahogany and some of the high-ranging junipers (Jwiiperus ocddentalis and scopulorum), which often ascend through it. Generally, it is char- acterized by open sagebrush slopes well covered with sagebrush (Artemisia tridentata, arbuscula^ and trifida), Balsamorhiza sagit- tata, Wyethia (miplexicaAdis^ and Paeonia brownii. Agriculture in this arid division of Transition Zone is practically limited to stock raising, mainly summer grazing of sheep and cattle. Where water is available for irrigation, there are ranch gardens and some hay, but water is scarce, and in the dry climate frosts are frequent during even the summer months. Ranches are few and far between and generally control extensive areas of grazing land. CROP ADAPTATIONS IN TRANSITION ZONE While little agriculture, except an occasional irrigated garden, is attempted in the arid Transition Zone, the semihumid bench land of this zone in the Blue Mountain section and along the eastern side of the Cascades produces excellent small-grain and potato crops, in most cases without irrigation. Still better crops of grains, potatoes, alfalfa, and some fruits, however, are grown where irrigation is possible. In the humid Transition Zone west of the Cascades a great variety of crops are raised — small grains, wheat, oats, rye, barley, peas, hops, clover, vetch, timothy hay, potatoes, vegetables, nuts, and fruits in profusion. Most of the valleys are famous for their flowers, roses of wonderful beauty and variety, gladioli, dahlias, and a great variety of hardy flowering plants. Each valley and every section of a valley have slightly different climatic conditions, and with the varying soil and humidity each one shows special adaptations that cannot be covered by any generalized lists of crops. The only safe course for the grower in selecting crops of special advantage in each location is to follow the advice of the local county agents, the State agri- cultural college, and the experiment stations. 1936] MAMMALS AND LIFE ZONES OF OREGON 25 Game and fur-bearing animals can be considered a legitimate crop, and much of the Transition Zone, both in the timbered and in the treeless arid divisions, is especially adapted to their production. The wildlife of the forests if well handled is often as valuable as any other forest product. CANADIAN ZONE The Canadian Zone in Oregon covers all but the high peaks4 and ridges of the higher Cascade, Siskiyou, Blue, and Steens Mountains, and caps many of the lower groups, such as the Paulina, Yamsey, Winter, and Warner Kanges. On Mount Hood at the northern end of the Cascades in Oregon, with a 100-foot base level around three sides of the mountain, the zone runs correspondingly low (fig. 1), N.E. FIGURE 1. — Life zones on Mount Hood from northeast to southwest exposures, with low base level on both sides and the zones consequently running low. reaching from 3,000 to 5,000 feet on the cold northeast slopes and from about 4,000 to 6,000 feet on warmer southwest slopes. This lowering of the life zones, in addition to the great height of the peak, accounts for the magnificent display of ice and snow above timber line on Mount Hood. I0,5£3 feet S.W. N.E. FIGURE 2. — Life zones on Mount Jefferson from northeast to southwest exposures, show- ing approximate altitudes above sea level and slight elevation due to higher base level. 26 NORTH AMERICAN FAUNA [No. 55 In the middle section of the Cascades around Mount Jefferson (fig. 2) the zone extends from about 3,500 to 5,500 feet on the north- east slopes and from about 4,500 to 6,500 on the southeast slopes, and around the Three Sisters Peaks (fig. 3) there is a noticeable eleva- tion of the zone to about 4,500 to 6,000 feet on the northeast slopes, and a little under 5,000 to 7,000 on the southwest slopes in con- formity with the more elevated base level of the upper Deschutes and Willamette Valleys on the two sides of the range. s.w. 10.352 feet- N. E Sea /eve/ FIGURE 3. — Life zones on Three Sisters Peaks from northeast to southwest exposures, showing approximate elevation above sea level and effect of elevated base level on northeast slope. In the southern Cascades the zone extends generally from about 5,000 to 7,000 feet in altitude on the cold, or northeast slopes, and from about 5,500 to 7,500 feet on the warmer southwest slopes, except on Mount McLoughlin, where it shows little variation from 5,000 to 7,000 feet clear around the mountain (fig. 4). In many places west of the mountains with the low base level of nearby valleys, sw. N.E So no ran Sea level FIGURE 4. — Life zones on Mount McLoughlin (Pitt) from northeast to southwest expo- sures, showing effect of elevated base level on northeast side in neutralizing the usual difference in zone levels on sunny and shady slopes. the lower edge of the zone falls 500 to 1,000 feet lower, or to 4,000 or 4,500 feet in altitude, without corresponding change in its upper limit. 1936] MAMMALS AND LIFE ZONES OF OREGON 27 In the Wallowa and Baker Ranges of the Blue Mountains, Cana- dian Zone covers the high middle slopes from approximately 5,000 to 7,000 feet on the northeast slopes and 6,000 to 8,000 on the warmer southwest slopes, but varying considerably in different parts of the ranges (fig. 5). The highest peaks in the Baker Range reach to 8,920 and 9,097 feet, according to the United States Geological Survey map, while in the Wallowa Range the Forest Service map shows the higher peaks reaching from 9,000 to 9,800 feet. Considerable masses s.vy. ^^T>\ N-C. So no ra n Sea level FIGURE 5. — Life zones in the Wallowa Mountains from the northeast to the southwest exposures, the zones considerably elevated by moderately high base level around two sides of the mountains. of permanent snow and ice and one small glacier on these peaks indicate their altitude. The Steens Mountains, with a 4,000- to 5,000-foot base level all around, show the highest zone levels in the State. The Canadian Zone extends from about 6,000 to 7,500 feet on cold slopes and 7,000 to 8,500 feet on warm slopes, but the mountains are so bare of timber and vegetation in general that their zones are not clearly marked 9,354 feet S.W. ^ — — — ^_ .A N.E. Sea /eve/ FIGURE G. — Life zones of the Steens Mountains, showing approximate levels of life zones on northeast and southwest exposures and emphasizing the elevating effect of high base level on the full set of zones. (fig. 6). The extreme aridity of the climate prevents any real forest growth, while erosion and overgrazing have destroyed much of the native flora and fauna. 28 NORTH AMERICAN FAUNA [No. 56 MAMMALS In the Cascades the Canadian Zone is characterized by the snow- shoe rabbit, brown and dusky conies, Cascade squirrel, flying squirrel, yellow-bellied marmot, red-backed mouse, lemming mouse, large- footed meadow mouse, mountain jumping mouse, Mazama gopher, and mountain mole. In the Blue Mountains the characteristic mammals are the Rocky Mountain mule deer, elk, mountain sheep, varying hare, Jewett's cony, Richardson's squirrel, Idaho flying squirrel, red-backed mouse, large-footed meadow mouse, Rocky Mountain meadow mouse, Ore- gon jumping mouse, brown pocket gopher, Rocky Mountain marten, Canada lynx, mountain shrew, hoary and silver-haired bats. In the Steens Mountains are found the Rocky Mountain mule deer, Taylor's cony, Rocky Mountain meadow mouse, Oregon jumping mouse, mountain shrew, and silver-haired bat. In summer the Canadian Zone has a peculiar value as a resort for some of the most important large game and fur-bearing mammals, the Rocky Mountain elk and mule deer, bighorn sheep, and formerly for marten, wolverine, Canada lynx, and red foxes. BIRDS Common breeding birds of the Canadian Zone in the Cascades are Barrow's goldeneye, three-toed woodpeckers, Williamson's sapsucker, red-breasted sapsucker, olive-sided flycatcher, black-headed jay, Ore- gon jay, Cassin*s finch, Bendire's crossbill, pine siskin, white-crowned sparrow, Thurber's junco, Rocky Mountain nuthatch, GambePs chick- adee, and ruby-crowned kinglet. The characteristic birds of the Blue Mountain Canadian Zone in- clude Richardson's and Franklin's grouse, Canada ruffed grouse, Williamson's sapsucker, olive-sided flycatcher, Rocky Mountain jay, Cassin's finch, Bendire's crossbill, siskin, white-crowned sparrow, and ruby-crowned kinglet. In the Steens Mountains are found the water ouzel, crossbill, junco, white-crowned sparrow, and rufous hummingbird. PLANTS The zone is generally characterized in the Cascades by lodgepole pine, western white pine, Engelmann spruce, Shasta fir, grand fir, silver fir, Alaska cedar, aspen, mountain maple, mountain-ash, high- bush cranberry, Shepherdia canadensis, Pachistima myrsinites, Vaccinium, erythrococcu/m, and Xerophyll/u/m tenax. In the Blue Mountain region dominant plants are lodgepole pine, limber pine, Engelmann spruce, grand and white fir, aspen, balsam poplar, mountain maple, mountain alder, mountain-ash, red elder, Arctostaphylos nevadensis, Shepherdia canadensis, Pachistima myr- sinites, Vaccinium scopariwn and erythrococcum, Lonicera involu- crata and conjugialis, Linnaea borealis, Clintonia miiflora, and many others showing a slight difference from the flora of the same zone in the Cascades. In the Steens Mountains the plant and animal life of Canadian Zone are similar to those of the Blue Mountain Canadian Zone with a 1936] MAMMALS AND LIFE ZONES OF OREGON 29 much more limited list of species. For flora it can show only two tree species in sheltered gulches, aspen and balsam poplar, some willows along the streams, and considerable other shrubby vegetation of the Blue Mountain or Rocky Mountain types. HUDSONIAN ZONE Hudsonian Zone is the narrow timber-line belt just below the permanent snow and ice fields of the higher peaks of the State. In vertical width it is seldom over 1,000 feet and on the steep upper slopes where found is at most but a narrow belt with a limited number of characteristic forms of life. It varies considerably in altitude on different peaks and ranges, conforming to the other zones in the influence of high or low base level. On Mount Hood it ranges from about 5,000 to 6,000 feet on cold slopes and 6,000 to 7,000 on warm slopes; on Jefferson 5,500 to 6,500 on cold and 6,500 to 7,500 on warm slopes; on Three Sisters from 6,000 to 7,000 on cold and 7,000 to 8,000 on warm slopes; on Mount McLoughlin (Pitt) from approximately 7,000 to 8,000 all the way around; in the Blue Mountains from 7,000 to 8,000 on cold and 8,000 to 9,000 on warm slopes ; and in the Steens Mountains about 7,500 to 8,500 on cold, and 8,500 to 9,354 feet on warm slopes but with poorly defined limits. Thus a difference of 2,000 feet in the level of the zone on corresponding slopes, shown in the State, is traceable to a still greater difference in elevation of base level. PLANTS The plants of Hudsonian Zone, in spite of its scattered sections, are more nearly the same throughout the State than are those of the lower zones. Throughout the Cascades the species are largely the same around all of the peaks high enough to afford the Hudsonian climatic conditions. In the Blue Mountain section- the Hudsonian species differ somewhat in showing a close affinity with the Rocky Mountain flora, and in the Steens Mountains the greater aridity cuts out all trees and many of the shrubs from the zone list. In the Cascades the characteristic species of the zone are the white- stemmed pine, alpine hemlock, alpine larch, alpine fir, alpine juniper, alpine mountain-ash, pink heather, white heather, little wintergreens (CrOMltheriaovata and humifusa), little blueberry (Vac- cinium scoparium) , LutTcea pectinata, wild currant (Ribes howellii), creeping dewberry, white rhododendron, red monkeyflower, smooth alum root, mountain lily (Erytkronium montanum), louse- wort (Pedicularis surrecta), grass of Parnassus, stonecrop (Sedwrn divergens), and twisted polygonum. In the Blue Mountains around the Wallowa and Baker _ peaks the characteristic Hudsonian Zone plants include all of the timber-line trees of the Cascades, a part of the shrubs and smaller plants, and in addition a considerable number of Rocky Mountain species, such as Ledwn glandulosum, Lonicera utahensis, Ribes lacus- tre (molle?), Dasiophora fruticosa, Erytkronium parviflorum, Clay- tonia lanceolata, Hoorebekia greenei, Ligmticum leibergi, Merathropta intermedia, Gilia nuttallii, Epilobiwn fastigiatum and homemannii. 30 NORTH AMERICAN FAUNA [No. 55 Dodecatheon tetrandrum, Angelica lyallii, Saxifraga mertensiana, Rhodiola frigida, Polygonum imbricatum, Pedicularis l>racteosa and racemosa, Ranunculus populago, Pentstemon fruticosus, and Aster integrifolius and cusickii. In the Steens Mountains the Hudsonian Zone is poorly denned, owing to the aridity of the summits, absence of trees and shrubby growth, and greatly denuded and eroded slopes. Still there is suffi- cient native life to serve as an approximate guide to the zonal divi- sions. The principal Hudsonian indicators in plants are dwarf willows, alpine juniper (Juniperus sibirica), thorny gooseberry, red currants, shrubby cinquefoil (D^asiphora frutioosa) , dwarf blueberry (V actinium scoparium), Kalmia glauca microphylla, Artemisia tile- sii, Eriogonum umbellatum and vweum, Saseifraga colunibiana, Sytmphoricarpos acutios, Spraguea multiceps, PolygonUm bistor- toides, Phacelia sericea, Quamasia leichtlinii, Dodecatheon puberu- Iwrn, Pedicularis surrecta, Helenium hoopesii, Phlewn alpinwni, and Delphinium cyanoreios. ARCTIC-ALPINE ZONE Arctic- Alpine, the last belt of dwarf plant and scanty animal life, corresponding to the Arctic tundra of the far north, is represented on most of the peaks in Oregon reaching above 9,000 feet in altitude. On Mount Hood it ranges from about 6,000 feet on northeast and 7,000 feet on southwest slopes upward to the permanent ice and snow, which cover most of the higher parts of the peak ; and on Jefferson from 6,500 and 7,500 feet upward. On the Three Sisters the zone lies above 7,000 and 8,000 feet, respectively, on the cold and warm slopes; on Mount McLoughlin (Pitt), above 8,000; in the Blue Mountains and Steens Mountains, above 8,000 and 9,000 feet, varying somewhat in accordance with varying local conditions of slope, soil, wind, and moisture, running1 lower on steep northerly slopes where the sun's rays are partially cut off and higher on the steep southerly slopes which catch the more nearly vertical rays of the sun. The effect of high and low base level is still apparent in this highest of the life zones. PLANTS In the Arctic- Alpine Zone of the Cascade peaks are such low or prostrate plants as Ranunculus eschscholtzii. Anemone hudsoniana, Antennaria media. Phlox douglasii and diffusa, Pentstemon menziesii, Veronica alpina, Silene suksdorfi, Saodfrag® tolmiei and bongardi, Potentilla flab elli folia, Oxyria digyna, Polygonwn newberryi, Genti- ana calycosa, Lewisia columbiana, Epilo'bium alpinum and anagalli- di folium, Erigeron salsuginosus, Hieracium gracile, Oreastrum alpigaenum. Arctic- Alpine Zone in the Blue Mountains is marked by such dwarf vegetation as the dwarf willow (Salix nivalis), Dry as octopetala, Ivesia gordoni, Sieversia rossii, Potentilla flabe7tifolia, Sawifraga deMlis and ~bongardi, Silene acaulis, Phlox diffusa and douglasii, Arenaria vema, sajanensis and nuttallii, Claytonia megarrhiza, Epi- lobium, alpinum and anagallidifolium, Lewisia nevadensis and tri- phylla, Dodecatheon jeffreyi, Oxyria digyna, Eriogonum piperi,, 1936] MAMMALS AND LIFE ZONES OF OREGON 31 Polygonum viviparum ana minimum, Veronica alpina, Mimulus al- pinus, Phacelia sericea, Pedicularis contorta, (J-entiana calycosa, Erigeron acris debilis and compositus, Hulsea nana, Arnica parryi, Antennaria media and lanata, Hieratium gracile, Phleum alpinum, and Phegopteris alpestris. In the Steens Mountains the vegetation is poorly represented in this zone, and the collecting has been but fragmentary. The follow- ing plants have been collected and noted as representing the zone on the peaks of these mountains : Ranunculus gloverianus, GUia nut- tallii, Aren-aria congesta and aculeata, Alsine ~boreaUs, Oxyria digyna, Veronica alpina, Drdba nemorosa, Spraguea umbellata&mimulticeps, Erigeron compositus trifidus, Achillea alpina, and Phleum alpinum. MAMMALS AND BIRDS Of mammals there seems to be no species restricted to the zone in the Cascades in Oregon, as the white goat does not come south of the Columbia River. Of breeding birds the rosy finch is perhaps the only characteristic species. In the Steens Mountains no mammals or birds are confined to the Arctic- Alpine. Collecting in the high peaks of the Wallowa and Baker Ranges has not been sufficiently thorough to establish any species of birds or mammals as breeding and occupy- ing in a restricted sense the Arctic-Alpine Zone. TABLE 1. — Mammals of Oregon, try life zones Species Common name Zone Sonoran Transition 1 0 Hudsonian Semiarid 1 Humid 3 £ "2 Bison bison oregonus Oregon bison - Ovis canadensis canadensis . Rocky Mountain bighorn X x canadensis californiana Riinrock bighorn Antilocapra americana oregona Prong-horned antelope x x Alces diner ica.no, shirasi Rocky Mountain moose americana gigns- _ _ Alaska moose (introduced) x Cervus canadensis nelsoni Rocky Mountain wapiti, elk . _ canadensis roosevetti . Roosevelt's wapiti, or elk x Odocoileubs hemionus macrotis Rocky Mountain mule deer X X X .... columbianm columbianus Columbian black-tailed deer x virginianus leucurus Columbian white-tailed deer x virginianus ochrourus Yellow-tailed deer x Lepus americanus bairdii Rocky Mountain snowshoe hare- Oregon snowshoe hare j amcricanus ktamathensis americanus washingtonii Washington snowshoe hare x townsendii townsendii . . Western white-tailed jack rab- bit. California jack rabbit californicus californicus californicus wallawalla . . Oregon jack rabbit x Sylvilagus nuttallii nuttallii Oregon cottontail bachmani ubericolor Redwood brush rabbit. . . x Brachylagus idahoensis Pygmy rabbit Ochotona schisticeps taylori Warner Mountain cony, pika. x schisticepsjewetti Blue Mountain cony, pika x princeps brunnescens Brown cony, pika fenisex fumosa. .. Dusky cony, pika x x Sciurus griseus griseus Silver gray squirrel X x X douglasii douglasii Douglas's squirrel douglasii cascadensis Cascade squirrel x x douglasii albolimbatus Sierra squirrel x X X x hudsonicus richardsoni... Richardson's squirrel... X 32 NORTH AMERICAN FAUNA [No. 55 TABLE 1. — Mammals of Oreyon, by life zones — Continued Species Common name Zone Sonoran Transition G 03 i § 0 Hudsonian Semiarid 1 •d w Semihumid 3 *n 4| Eutamias townsendii townsendii Townsend's chipmunk . townsendii cooperi - Cooper's chipmunk x townsendii ochrogenys Redwood chipmunk townsendii siskiyou - Siskiyou chipmunk x townsendii senex Allen's chipmunk x amoenus amoenus Klamath chipmunk amoenus luteiventris . . . Yellow-bellied chipmunk x x amoenus ludibundus Hollister's chipmunk x amoenus ochraceus - . Ochraceous chipmunk... x minimus pictus Sagebrush chipmunk x Callospermophilus chrysodeirus chryso- deirus. chrysodeirus trinitatis Golden-mantled ground squirrel. Tawny-mantled ground squirrel . Copperhead ground squirrel X X x chrysodeirvA connectens x Ammospermophilus leucurus leucurus-. Citellus douglasii. Antelope squirrel . Douglas's ground squirrel x x coiumbianus columbianus Columbian ground squirrel . oregonus - Oregon ground squirrel- x townsendii Townsend's ground squirrel Piute ground squirrel X mollis mollis -. x mollis canus Gray sage squirrel . . . mollis vigilis . ... - Speckled sage squirrel x elegans nevadensis Nevada ground squirrel x Marmota flaviventris flaviventris Yellow-bellied marmot X X flaviventris avara Pale yellow-bellied marmot x x Olaucomys sabrinus oregonensis Oregon flying squirrel x sabrinus fuliginosus Cascade flying squirrel x sabrinus klamathensis Xlamath flying squirrel X sabrinus bulletins .. Sawtooth Mountain flying squirrel. Bangs's flying squirrel X sabrinus bangsi x Rattus norvegicus . .. Norway rat x x rattus rattus Black rat rattus alexandrinus Roof rat. x Mus musculus musculus . .. _ House mouse x Neotoma cinerea occidentalis Western bushy-tailed wood rat.. Dusky bushy-tailed wood rat ... Dusky-footed wood rat cinerea fusca - x fuscipes fuscipes X lepida. nevadensis Nevada wood rat x Onychomys leucogaster fuscogriseus Peromyscus maniculatus rubidus Oregon grasshopper mouse _ . Ruddy deer mouse x maniculatus gambellii GambePs deer mouse x X maniculatus sonoriensis Sonoran deer mouse maniculatus artemisiae Sagebrush deer mouse.. . x X crinitus crinitus Idaho canyon mouse x Gilbert's white-footed mouse truei preblei Treble's white-footed mouse Desert harvest mouse _ . X Reithrodontomys megalotis megalotis — x California harvest mouse Clethrionomys californicus californicus.- California red-backed mouse x Dusky red-backed mouse x californicus mazama Mazama red-backed mouse X gapperi saturatus British Columbia red-backed mouse. Red tree mouse x silvicola Dusky tree mouse .. x albipes White-footed phenacomys x Mountain phenacomys X X intermedius olympicus Olympic phenacomys Peale's meadow mouse x x x Gray-tailed meadow mouse x x x Rocky Mountain meadow mouse. x x mordax abditus Tillamook meadow mouse X 1936 J MAMMALS AND LIFE ZONES OF OREGON 33 TABLE 1. — Mammals of Oregon, try life zones — Continued Species Common name Zone Sonoran Transition c as Hudsonian Semiarid 5 Humid 2 X3 1 Cascade meadow mouse x Large-footed meadow mouse Oregon creeping mouse - x Baird's creeping mouse X Pygmy mouse x Rocky Mountain muskrat x x Nevada muskrat - x Oregon coast muskrat Pacific coast beaver I X X X X Nevada beaver x x Aplodoniia rufa rufa Brown mountain beaver x Pacific mountain beaver x Ercihizon epixanthutn cpixanthum Yellow-haired porcupine X X X x X X X .... Northwest jumping mouse trinotatus pacificus Pacific jumping mouse x Mountain jumping mouse x princeps oregonus Blue Mountain jumping mouso. Coltimbian five-toed kangaroo rat. Preble's kangaroo rat - - x x x microps preblei x I>ipodomys heermanni californicus Northern California kangaroo rat. Qabrielson's kangaroo rat X x Microdipodops megacephalus oregonus- . Oregon gnome mouse x Oregon pocket mouse x parvus Tnollipilosus Coues's pocket mouse . - x Northwest pocket mouse x nevadensis Nevada pocket mouse x Thomomys bulbivorus Camas pocket gopher.. x townsendii townsendii Townsend's pocket gopher x Nevada pocket gopher x bottac ieucodon White-toothed pocket gopher. .. x bottae laticeps Huinboldt Bay pocket gopher. . Douglas's pocket gopher x x douglasit oregonus Oregon pocket gopher x Black pocket gopher x Mazama pocket gopher X X monticola hflleri Heller's pocket gopher . x Deschutes pocket gopher fuscus fuscus Brown pocket gopher x hesperus West coast pocket gopher x Dalles pocket gopher x x columbianus Columbia pocket gopher x Felis concolor oregonensis Oregon cougar x concolor hippolestet Rocky Mountain cougar x x cntus House cat _ - . x x x x x Lynx Tufus uinta Rocky Mountain bobcat x x rufus pallescens Cascade bobcat x rufus fasciatus Oregon bobcat -- x canadensis canadensis Canada lynx x Canis famUidTis Domestic dogs X X X x X X lycaongigas Northwestern timber wolf lycaon nubilus Plains wolf x latrans lestes . ... Mountain coyote.. X X X X Vulpes fulvus cascadensis Cascade red fox .. x fulvus inacrourus Rocky Mountain red fox x macrotis nevadensis Nevada long-eared fox _ ..... x Urocyon cinereoargenteus townsendi Afustela longicauda arizonensis Oregon gray fox. . x Arizona weasel x X X longicauda saturate Cascade weasel. x washingtoni Washington weasel x Oregon bridled weasel x cicognanii slreatori Puget Sound weasel x cicognanii tnuricus Sierra least weasel x Rocky Mountain least weasel X x X Lutrcola vison energumenos Western mink x x 3-lartes caurina caurina Pacific marten x x Rocky Mountain marten x pennanti pacifica... Pacific fisher... X 7209°— 36 3 34 NOBTH AMERICAN FAUNA [No. 55 TABLES 1. — Mammals of Oregon, 'by life zones — Continued Species Common name Zone Sonoran Transition 0 1 c B I •o •c -< Humid Semihumid •o 3 Gulo luscus luscus Wolverine x Lutra canadensis pacifica Western otter X Enhydra lutris nereis Sea otter. _ x Taxidea taxus neglecta California badger X X x Mephitis occidentalis occidentalis .. California skunk x occidentalis spissigrada Puget Sound skunk_ . . x occidentalis notata-.. Columbia Valley skunk... X occidentalis major Great Basin skunk. x x x Great Basin spotted skunk X X phenax latifrons Oregon spotted skunk— x Procyon lotor pacifica Northwestern raccoon x lot or fxcelsus Snake River Valley raccoon ... x Bassariscus astutus raptor Ringtail x Euarctos americanus cinnamomum americanus nltifrontalis Idaho black bear x x x Olympic black bear_ x Ursus klamathensis Klamath grizzly idahoensis Idaho grizzly x Yellowstone Park grizzly x Eumetopias jubata Steller's sea lion x Zalophus californianus California sea lion- x Northern fur seal fhoca richardii richardii Hair seal x C etaceans 1 -- -- Whales and porpoises Scapanus townsendii Townsend's mole x latimanus dilatus Klamath mole x latimanus alpinus Mazamamole x Coast mo]« x orarius schefferi Schefler's mole x x Neurotrichus gibbsii gibbsii Gibbs's mole x Sorex palustris navigator Rocky Mountain water shrew .. X x bendirii bendirii Bendire's shrew x bendirii palmeri Palmer's shrew x trowbridgii trowbridgii Trowbridge's shrew x trowbridgii mariposae ... Yosemite shrew . .. x obscurus obscurus Dusky shrew X X obscurus bairdi . . Baird's dusky shrew x obscurus permiliensis Cascade dusky shrew x obscurus setosus .. . Olympic dusky shrew x x pacificus pacificus Pacific shrew __ x pacificus yaquinat . Yaquina shrew x vagrans vagrans Vagrant shrew . x x vagrans tnonticola _ . _ . Rocky Mountain shrew x vagrans amoenus Sierra shrew _ . x ornatus trigonirostris _ _ . _ _ Siskiyou shrew x Merriam's shrew. preblei Preble's shrew x Myotis californicus californicus Little California bat x x californicus caurinus Northwest coast bat ._. - x subulatus inelanorhinus Black-nosed bat x tvotis evotis Little big-eared bat x evotis chrysonotus Desert golden bat x Dusky bat x yumanensis sociabilis Tejon bat X X lucifugus carissima Yellowstone bat x x lucifugus alascensis Alaska little brown bat x tolans longicrus Long-legged bat x volans interior Interior bat x Eptesicus fuscus fuscus Big brown bat X X X Lasionycteris noctivagans Silver-haired bat x Pipistrellus hesperus hesperus Little canyon bat x Nycteris cinerea Hoary bat X x Corynorhinus rafinesquit townsendii rafinesquii pallescens Jack-rabbit bat x Pale jack-rabbit bat x x Intermediate jack-rabbit bat Antrozous pallidus pacificus Pacific pale bat x pallidus cantwelli Large gray bat x Didelphis virginiana virginiana ..- Virginia opossum x i Ocean; no zones given. 1936] MAMMALS AND LIFE ZONES OF OREGON 35 TABLE 2. — Reptiles of Oregon, by life zones l LIZARDS Species Common name Zones Sonoran Transition 1 O Hudsonian Semiarid •0 'C < Humid Semihumid 1 Crotaphytus wislizenii Leopard lizard x silus. Short-nosed tiger lizard x collaris baileyi Western collared lizard x Uta stansburiana stansburiana __ Northern brown-shouldered liz- ard. Sagebrush swift.. X x Sceloporus graciosus graciosus graciosus gracilis Mountain swift x occidentalis occidentals Pacific blue-bellied lizard x occidentalis biseriatus Western blue-bellied lizard x x Phrynosoma douglassii douglassii Pygmy horned toad x platyrhinos Desert horned toad x Oerrhonotus principis Northern alligator lizard x scincicauda scincicauda Western alligator lizard x x Cnemidophorus tessellatui tessellatus. . . Plestiodon skiltonianus Desert whiptail lizard x Western skink . x x SNAKES Charina bottae bottae Pacific rubber snake. . x x Diadophis amabilis Western ringneck snake x x Coluber constrictor mormon Western yellow-bellied racer x taeniatiistaeniatus Western striped racer x Pituophis catenifer catenifer Coast gopher snake x catenifer heermanni. Valley gopher snake x catenifer deserticola Desert gopher snake x Contia tennis Sharp-tailed snake x Thamnophis sirtalis concinnus Western garter snake x sirtalia infernalis __ Pacific garter snake x x ordinoides ordinoides Puget Sound garter snake x ordinoides biscutatus Klamath garter snake x x x ordinoides vagrans Wandering garter snake x x Crotalus oreganus Pacific rattlesnake __ x x confluentus Plains rattlesnake x x TURTLES Clemmys marmorata Pacific terrapin x x x x Chrysemys marginata bellii _ Western painted turtle. x x x 1 Specimen identifications by Remington Kellogg. 36 NOETH AMERICAN FAUNA TABLE 3. — BreetiAng birds of Oregon, by life zones1 [No. 55 Species . Common name Zone Sonoran Transition Cana- dian Hudsonian Arctic-Alpine 1 Semiarid S *c •< Pi E CO 5 S 3. 2 a x 2 •< 2 W g 1 a 5 Qavia immer immer Common loon x X Colymbus nigricollis californi- cus. Aechmophorus occidentaiis Podilymbus podiceps podiceps . Oceanodroma furcata. Eared grebe x x Western grebe X X Pied-billed grebe Forked-tailed Petrel X leucorhoa beali Beal's petrel X Pelecanus erythrorhynchos Phalacrocorax auritus albocilia- tus. penidllatus x Farallon cormorant . X I X — Brandt's cormorant x pelagicus resplendens Baird's cormorant x Ardea herodias treganzai Treganza's heron x x herodias fannini Northwestern Coast heron. American egret x Casmerodius albus egretta X Butorides virescens anthonyi Nycticorax nycticorax hoactli-.. Botaurus lentiginosus Anthony's green heron X — Black-crowned night heron. American bittern X x X x X X X X X Ixobrychus exilis hesperis X x X x Plegadis guarauna White-faced glossy ibis — - Brant a canadensis canadensis. . Anas platyrhynchos platyrhyn- chos. C'haulelasTnus streperus Common Canada goo^e x x x x CoTmnon fnallard x x x x X x Gadwall x x X x X x Dafila acuta tzitzihoa American pintail x Nettion carolinense Green-winged teal x x x Querquedula discors Blue-winged teal x x x cyanoptera Cinnamon t^ftl x x Spatula clypeata _ Shoveler X x x Aix sponsa Wood duck x Nyroca americana . Redhead X valisineria Canvasback x Glaucionetta islandica Barrow's goldeneye X X Histriordcus histrionicus pacifi- cus. Erismaiurajamaicensis rubida . Mergus merganser americanus . Cathartes aura septentrionalis.. Astur atricapillus striatulus Accipiter velox velox Western harlequin duck x Ruddy duck X X X X American merganser X x Turkey vulture x x Western goshawk X x Sharp-shinned hawk X x cooperi Cooper's hawk x x Buteo borealis calurus Western red-tailed hawk X X x x swatnsoni Sv/ainson's hawk x regatis Ferruginous roughleg x Aquila chrysaetos canadensis. . . Haliaeetus leucocephalus alas- canus. Circus hudsonicus Golden eagle X X X X X X X Northern bald eagle Marsh hawk x Pandion haliaetus carolinensis . Falco mexicanus Osprey X Prairie falcon x peregrinus anatum Duck hawk x x x peregrinus pealei Peale's falcon x columbarius suckieyi Black pigeon hawk x x sparverius phalaena Desert sparrow hawk X X x x x x Dendragapus obscurus rich- ardsoni. fuliginosus fuliginosus Canachites franklini Richardson's grouse x X Sooty grouse X X Franklin's grouse X Bonasa umbellus togata Canada ruffed grouse x x umbellus sabini x x x Pedioecetes phasianeUus co- lumbianus. Centrocercus urophasianus Colinus virginianus virginianus. Lophortyx californica calif ornica Columbian sharp-tailed grouse. Sage hen X x x x x California quail x Valley quail x x pictavicta..- Plumed quail.-. X i Listed with the assistance of Stanley G. Jewett. 1936] MAMMALS AND LIFE ZONES OF OREGON 37 TABLE 3. — Breeding 'birds of Oregon, &y life zones — Continued Species Common name Zone Sonoran Transition Cana- dian Hudsonian Arctic-Alpine 5 3 p. 5 00 6 "3 w 1 s *c •< Humid 1 Orus canadensis tabida Sandhill crane X X Rallus limicola limicola Virginia rail X x X x X x Sora x x Fulica americana americana..- American coot X X X X Black oyster-catcher X Charadrius nivosus nivosus Oxyechus vociferus vodferus Western snowy plover x Killdeer X X X X x X x X x x X Wilson's snipe Numenius americanus ameri- canus. Long-billed curlew X X X Spotted sandpiper X x X x X X X x X x X X Catoptrophorus semipalmatus inornatus. ftecurrirostra americana Western willet Avocet X x X \ Black -necked stilt Steganopus tricolor Wilson's phalarope X X X X Larus Occident 'alls occidentalis.. Western gull x California gull x x x x delawarensis Ring-billed gull -- . X X X x X Forster's tern X x X x Hydroprogne caspia imperator. Chlidonias nigra surinamensis - Una aalge californica Caspian tern Black tern X x California murre x Pigeon guillemot x Lunda cirrhata Tufted puffin i x Columba fasciata fasciala Band-tailed pigeon i X X X Zenaidura macroura margi- nella. Coccyzus americanus occiden- talis. Tyto alba pratincola Western mourning dove I x x Barn owl x x MacFarlane's screech owl. Kennicott's screech owl X X x x asio ksnnicotti X X Flammulated screech owl- Dusky horned owl x Bubo virginianus saturatus virginianus pallescens x x Western horned owl X X X X X Olaucidium gnoma pinicola gnoma californicum Rocky Mountain pygmy owl. California pygmy owl x Coast pygmy owl x Speotyto cunicularia hypugaea.. Western burrowing owl x Northern spotted owl x x x x x flammeus flammeus Short-eared owl X X x Cryptoglaux acadica acadica Phalaeonoptilus nuttalli nut- talli. Saw-whet owl x x x x x x Pacific nighthawk x x x x Chaetura vauxi Vaux's swift X X X Selasphorus platycercus platy- cercus. TUfuS Broad-tailed humming- bird. Rufous hummingbird X X X X X Stellula calliope Calliope hummingbird X X Megaceryle alcyon caurina Colaptes cafer cafer Western belted kingfisher. Northwestern flicker X X X X X X X x X X cafer collaris Red-shafted flicker X x Ceophloeus pileatus picinus Balanosphyra formicivora bairdi. Asyndesmus lewis Western pileated wood- pecker. California woodpecker x x x x Lewis's woodpecker. __ X X X Sphyrapicus varius nuchalis Red-naped sapsucker x Northern red-breasted sap- sucker. Williamson's sapsucker x x thyroideus thyroideus Y Harris's woodpecker X J X x villosus orius Modoc woodpecker x . villosus monticola Rocky Mountain hairy woodpecker. 1 x x 38 NORTH AMERICAN FAUNA [No. 56 TABLE 3. — Breeding Mrd$ of Oregon, by life zones — Continued Species Common name Zone Sonoran Transition Cana- dian Hudsonian Arctic-Alpine Semiarid 1 Coast strip w. !2 A 1 02 s *tM •3 Humid Semiarid Dryobates pubescens leucurus.. pubescens gairdneri Batchelder's woodpecker. - x x Oairdner's woodpecker- x x x albolarvatus albolarvatus Picoides arcticus Northern white-headed woodpecker. Arctic three-toed wood- pecker. Alaska three-toed wood- pecker. Eastern kingbird x x Picoides tridactylus fasciatug Tyrannus tyrannus X x — - X verticalis Arkansas kingbird x x Myiarchus cinerascens cinera- scens. Sayornis say a say a Ash-throated flycatcher x x Say's phoebe x x x Empidonax trailli trailli Alder flycatcher x x hammondi Hammond's flycatcher x x wrighti . Wright's flycatcher x x gTlSCUS Gray flycatcher ... x dilficilis difficilis Western flycatcher X x Myiochanes richardsoni rich- ardsoni. Nuttallornis mesoleucus . Western wood pewee— x x Olive-sided flycatcher x x Otocor is alpestris arcticola Pallid horned lark x x alpestris merrilli Dusky horned lark X x Tachycineta thalassina lepida.. Jridoprocne bicolor Violet-green swallow. ._. X X X X X X X x X x ,— Tree swallow Riparia riparia riparia Bank swallow— X X X X X X Stelgidopteryx ruficoltis serri- pennis. Hirundo erythrogaster Rough-winged swallow — Barn swallow X X x X X X X X X X X X X X X Petrochelidon albifrons albifrons Progne subis hesperia Northern cliff swallow Western martin Perisoreus canad ensis capitalis.. obscurus obscurus Rocky Mountain jay x Oregon jay - x x obscurus griseus Gray jay x Cyanocitta stelleri carbonacea.. stelleri annectens Coast jay Black-headed jay .... .... X X x x Aphelocoma californica califor- nica. californica woodhousei Pica pica hudsonia California jay x Woodhouse's jay x American magpie x x Corvus corax sinuatus American raven . . x x brachyrhynchos hesperis brachyrhynchos caurinus Cyanocephalus cyanocephalus.. Nucifraga Columbians Western crow x x x Northwestern crow x Pinon jay . . x x Clark's nutcracker x x Penthestes atricapillus septen- trionalis. atricapillus occidentalis garnbeli gambeli Long-tailed chickadee x x Oregon chickadee X X Mountain chickadee x x rufescens rufescens Chestnut-backed chicka- dee. Oregon titmouse x x Baeolophus inornatus segues- tratus. inornatus inornatus _ .. x Plain titmouse x Psaltriparus minimus minimus minimus californicus Coast bush tit x California bush tit x minimus plumbeus Lead-colored bush tit x Sitta carolinensis nelsoni Rocky Mountain nut- hatch. Slender-billed nuthatch .. X X X X ---- carolinensis aculeata . X X canadensis Red-breasted nuthatch x x X X pygmaea pygmaea Pygmy nuthatch x Certhia familiaris montana familiaris zelotes Rocky Mountain creeper X X X X Sierra creeper familiaris occidentalis Chamaea fasciata phaea California creeper x x Coast wren tit x Cinclus mexicanus unicolor Troglodytes aedon parkmani Nannus hiemalis pacificus... Dipper X x X X X X Western house wren Western winter wren... X X 1936] MAMMALS AND LIFE ZONES OF OREGON 39 TABLE 3. — Breeding Urds of Oregon, by life zones — Continued Species Common name Zone Sonoran Transition Cana- dian Hudsonian Arctic- Alpine I 1 o, i O Humid £ "3 % S w Semiarid Thryomanes bewicki calophonus Seattle wren T X San Joaquin wren x Telmatodytes palustris plesius.. palustris paludicola Western marsh wren X X Tule wren x X Catherpes mexicanus punctula- tus. Salpinctes obsoletus obsoletus... Dotted wren x Common rock wren x x Catbird x x x Oreoscoptes montanus Sage thrasher X Turdus migratorius propinquus IXOTCUS naevius naevius Western robin X X X X x x x Pacific varied thrush Northern varied thrush x Hylocichla guttata sequoiensis. . guttata auduboni x Audubon 's hermit thrush- Russet-backed thrush x ustulata ustulata x x x x ustulata, swainsoni Olive-backed thrush X X Sialia meiicana occidentalis Western bluebird X X Mountain bluebird X X X X X X Myadestes townsendi Regulus satrapa olivaceus Corthylio calendula cineraceus.. Anthus spinoleita rubescens Western golden-crowned kinglet. Western ruby-crowned kinglet. x x X X x Cedar wax wing X X X Lanius ludovicianus excubi- torides. White-rumped shrike x x I In t ton 's vireo x x solitarius cassini Cassin 's vireo X X x X Red-eyed vireo Western warbling vireo x x x Verjnivora ctlata lutescens Lutescent warbler x x Calaveras warbler x x x x Dendroica aestiva aestiva Eastern yellow warbler California yellow warbler. Audubon 's war bier . . . X X aestiva brewsteri x x auduboni auduboni X X x X x Black-throated gray war- bler. Townsend's warbler townsendi x x occidentalis Hermit warbler X X Oporornis tolmiei Macgillivray's warbler x x x Geothlypistrichas Occident alis Western yellow-throat x x trichas arizela Pacific yellow-throat x x Icteria virens longicauda Long-tailed chat x x Wilsonia pusilla pileolata Northern pileolated war- bler. Golden pileolated warbler _ American redstart x x pusilla chryseoto. x x Setophaga ruticilla x Dolichonyx oryzivorus... Bobolink x Sturnella neglecta Western meadow lark x x x x Xanthocephalus xanthocepha- lus. Agelaius phoeniceus nevadensis. phoeniceus caurinus. Yellow-headed blackbird x x Nevada redwing x x x x Northwestern redwing X X Icterus bullocki Bullock's oriole x x Euphaguscyanocephalus Brewer's blackbird-- x x X x X x Molothrus ater artemisiae. Nevada cowbird x x Piranga ludoviciana Western tanager x Hedymeles melanocephalus me- lanocephalus. Passerina- amoena Black-headed grosbeak x x Lazuli bunting x Hesperiphona vespertina brooksi Carpodacus purpureus califor- nicus. cassini Western evening grosbeak- California purple finch -. x x x x Cassin's purple finch X X . mexicanus frontalis Pinicola enucleator montana Leucosticte tephrocotis littoralis. tephrocotis tevhrocotis... Common house finch x x Rocky Mountain pine gros- beak. Hepburn's rosy finch x x X Orav-crowned rosv finch.. 40 NORTH AMERICAN FAUNA [No. 55 TABLEI 3. — Breeding birds of Oregon, by life zones — Continued Species Common name Zone Sonoran Transition Cana- dian Hudsoaian § !& ^ 6 l Shasta fir X X X X Acer douoldsii \ Douglas maple - X X X X X X x X x X X X do - X X x Rockcress X do X x Sierra bearberry . . X X Golden arnica - X Idtifolid Broadleaf arnica X X Great aster - - X x X Broadleaf aster Cusick aster X Little barberry X Cdpnoides cusickii Corydalis x do x Cdstillcjd etdtd Paintbrush X do x x x X Chdmdecypdris wootkdtensis Nootka cypress X x X x Turtlehead Chimaphila umbellata occidentalis . . Pipsissewa - X x X X X Bugbane Cinna latifolia Drooping wood reed X X Cirsium aifiericanutn Thistle Clematis x Clintonict uniflora Queencup X X X Mazama x Goldthread .. .. X x Bunch berry x X Fairybells - x Dodecatheon aipinum Shootingstar X X Drymocallis x Echinoponax horridutn Devilsclub X Goldenyarrow x Deertongue -- .. .. X x X x X Bedstraw x x oregonum do X GUla nuttallii Nuttall gilia X X X X X X X Alumroot Hydrophyllum albifrons Waterleaf Rush x Juniperus communis montana Kelloggia galioides Mountain juniper X X X X X Kelloggia X Rabbitberry x Washington lily x Linnaea borealis Twinflower X X X X X X X Sweetberry honeysuckle Bearberry honeysuckle x X X X conjugalis Twinberry X Lupinus andersoni Bluebonnet; lupine x lyallii lobbii do x x x sulphureus . do X Bluebells x X X x Lewis monkeyflower x X x X Yellow monkeyflower x Blue-eyes X x X Myrtle boxleaf x X JPatonia brownii Brown peony X • X X Fernleaf x do x do-- X Blue pentstemon X x X X x Shrubby pentstemon Striped pentstemon X x Crimson pentstemon Reed canary grass x Phleum alpinum Alpine timothy... X X Z X 7209°— 36 * 50 NOKTH AMERICAN FAUNA [No. 55 TABLE 6. — Plants of the Canadian Zone in Oregon — Continued Species Common name Cas- cades Siski- you Blue Moun- tains S teens Moun- tains Rocky Moun- tains Picea breweriana... Brewer spruce engelmanni Engelmann spruce x x x X X X Pinusflexilis Limber pine X monticola ... Western white pine murrayana Lodgepole pine x x Pleuropogon refractus Semaphore-grass X x Poo kelloggii . Bluegrass . Polemonium carneum... Polemonium X x occidental do X Polygonum kelloggii . . Polygonum X x X X X X Populus tremuloides aurea Golden aspen X X x x balsamifera Balsam poplar Potentilla drummondii Cinquefoil X x Pyrola secunda Winterlettuce x X X Pyrus sitchensis Mountain-ash X X x X Quercus sadleriana Deer oak vaccinifolia Huckleberry oak X X Ribes binominatum Siskiyou gooseberry X x triste Drooping currant. lacustre Prickly currant X X x X X marshaUii Marshall gooseberry Rubus nivalis... .. Snow dewberry x Rudbeckia occidentalis Coneflower X X Sambucus melanocarpa Blackbead elderberry X X Sanguisorba latifolia . White burnet x x Saxifraga rufidula.. Saxifrage X Sedum obtusatum Stonecrop X Senecio triangularis Groundsel x X X pseudaureus do X Silene oregana Catchfly X Stenanthium occidental _ Slenderlily X X X Streptopus amplexifolius Twistedstalk Thermopsis montana Goldenpea .. .. x Thlaspi glaucum . Blueleaf pennycress_ X X X Trautvetteria grandis Bigleaf X x ' Trientalis arctica Starflower Trifolium plumosum. Pussy clover X howellii Bigleaf clover X x X x Ttuga heterophylla __ Western hemlock X X X X X X X X Vaccinium occidental Western bog blueberry X x X x macrophyllum Big whortleberry . scoparium Grouse whortleberry x X X x Valeriana sitchensis scouleri Valerian X x Veratrum californicum Snowy false-hellebore viride Green false-hellebore X X x X X Viburnum pauciflorum . Rayless cranberrybush Purple violet Viola purpurea . x x x Xerophyllum tenax Beargrass x x TABLE 7. — Plants of the Hudsonian Zone in Oregon Species Common name Cas- cade Moun- tains Blue Moun- tains S teens Moun- tains Rocky Moun- tains Far North Abies lasiocarpa Alpine fir x Agoseris gracilens Sheeplettuce x x alpestris do x x Agrostis humilis Mountain red top x Alliummacrum Wild onion \ validum ... Swamp onion x Alnus sinuata Sitka alder x Aplopappus greenei Goldenweed x AquiUgia flavescens Cnlumbinft x x Arabis drummondii Rockcress x platysperma _ . do Arenaria capillaris.. Sandwort x pumicola do Arnica latifolia Arnica x longifolia.. do x Artemisia tilesii x x x Aster engelmanni _ Aster x foliaceu$ frondeua . . do x x integrifolius do x x x Astragalus hooker ianus.... Bal loon pod. _. X X 1936] MAMMALS AND LIFE ZONES OF OREGON 51 TABLE 7—Plcmts of the Hudsonian Zone in Oreyon — Continued Species Common name Cas- cade Moun- tains Blue Moun- tains Steens Moun- tains Rocky Moun- tains Far North Athyrium alpestre americanum Betula glandulosa Alpine ladyfern X x x Resin birch BTOTIIUS suksdorfii Bromegrass X x X x Calochortus lobbii Mariposa Calthd biflora White marshmarigold x x leptosepala ... Elkslip X X X X x Cardamine lyallii Bittercress . X X X x Carex mertensii Sedge X X x X Cassiope mertensiana. . . . Moss-heath Castillejd oreopola Paintbrush do X x Chatnaecyparis nootkatensis Nootka cypress - X Cheilanthes siliguosa Oregon cliffbrake x x Chelone nemorosa . Turtlehead X x Claytonid asarifolia Springbeauty x Cryptogramma acrostichoides Dasiphord fruticosa Rockbrake X X X X X x X X X X Shrubby cinquefoil X X Delphinium cyanoreios Larkspur depauperatum do X x x Dcschampsid atropurpurea Mountain hairgrass X X Dodecatheon puberulum Shootingstar X tetrandTum do x Drabd stenoloba Rockcress X X X Epilobiuin clo.vo.tuin Willowweed fastigiatuin - do - x x hornemannii - do X x X X luteum .-do.... X oregontnse. do x Erigeron membranaceus. Fleabane X (Buckwheat family) umbellatum do x tineum do X Eriophorum polystachyon Cotton-sedge X X Erythronium montanum Avalanche-lily x Bucephalus ledophyllus Asteroid X Gaultherid hmnifusa Creeping wintergreen X X Gilia nuttallii Oilia X X Helenium hoopesii Orange sneezeweed flemievd ranunculifolid . Saxifrage X X x Heuche TO, gldbrd .- . Smooth alumroot .. . X Juncoides glabratunt Woodrush pipcri do X X Juniperus communis tibirica Dwarf juniper X X Kalmia polifolia microphylla . Rocky Mountain kalmia X X Larix lyallii \lpine larch X Ledum glandulosum Labrador-tea X X x Ligusticum leibergi Lo veroot x tenuifolium do x L/onicero utahensis Utah honeysuckle x x Lupinus latifolius subalpinus Alpine bluebonnet X lyallii Lyall bluebonnet Mimulus lewisii _._ Lewis mimulus X X x Mitello, breweri Bishopscap pentandra do x x X x X Parnassia fimbriata .. Parnassia X X PtdiculdTis bracteosa Fernleaf X X X SUTTCCtd do X Pentstemon fruticosus. Pentstemon X Tupicola . . - do X Phacelia linearis Curlybloom newberryi .. do x sericca do X Phleum alpinuTn Mountain timothy Phyllodoce empetriformis. Red mountainheath X X X X X Pinus albicaulis Whitebark pine Poo lepiocoma Redtop Thizomata do x Polemonium humile Mountain polemonium Bistort . X X X X X X X X X Polygonum bistortoides X Potentilld cnscadensis Cinquefoil Quamasid leichtlinii Camas Railldrdelld argentea Woollyleaf x Ranunculus alistnetlus Buttercup X populago ... do x Rhodiold integrifolia ... Roseroot x x x Rhododendron albiflorum False-azalea X X X Ribes howellii Howell currant montigenum... Gooseberry currant X X 52 NORTH AMERICAN FAUNA [No. 55 TABLE 7. — Plants of the Hudsoniwn Zone wi Oregon — Continued Species Common name Cas- cade Moun- tains Blue Moun- tains Steens Moun- tains Rocky Moun- tains Far North Rubus lasiococcus Downy dewberry x pedatus Dwarf dewberry x Salix lemmoni _ . Lemmon willow X Saussurea americana ( Compositae) x x Saxifraga bronchialis . __._... Saxifrage X x x Columbians, do - x mertensiana do x x odontoloma. _ . . .. .... do X X odontophylla do _ . X Sedum debile Stonecrop x divergens . . - - do Senecio subnudus Groundsel X triangularis do x x Siiene oregana Catchfly X Sorbus occidentalis Mountain-ash Sparganium minimum Bur-reed Pink spirea x x Symphoricarpos acutus Snowberry x Tofieldia intermedia — Boglily X Tsuga mertensiana Mountain hemlock X x Vaccinium deliciosum Timber line whortleberry scoparium Grouse whortleberry - - - X Valeriana sitchensis Valerian X x x Rayless cranberrybush Viola venosa Yellow violet -- - I x orbiculata do X Zygadenus elegans Deathcamas x x TABLE 8. — Plant* of the Arctic-Alpine Zone in Oregon-1 Species Common name Cas- cade Moun- tains Blue Moun- tains Steens Moun- tains Rocky Moun- tains Arctic Achillea alpina Alpine yarrow x Agrostis hiemalis geminata Tickle grass x x x x rossae Ross redtop x x Alsine borealis Starwort x x Anemone hudsoniana Windflower . x x Antennarid media Pussytoes x x x lanata. do Apiopappus lyallii Goldenweed x x Arcnaria aculeata Sandwort x nuttallii ...do--- x x sajanensis do. x x x verna do x x x x Arnica parryi Arnica x x Aster andersoni Mountain ast.p.r x alpigenus... ... . . Timber line aster _. x Athyrium alpestre americanum Alpine lady fern x Campanula scabrella Alpine bellflower x x Cardamine bellidifolia Bittercress x Claytonia megarrhiza Springbeauty x x Collomia debilis Little collomia x Crepisnana .. Dwarf crepis . x x x Danthonia intermedia Oatgrass x x x Dodecatheon Jeffrey i—. . Shootingstar _ - x x X Douglasia laevigata Douglasia x Draba lemmoni Whitlowgrass x x aureola do x nemorosa . . . do x Dryas octopetala White dryad x x x Epilobium alpinum Alpine willowweed x x x x anagallidifolium Purple willowweed x x X x delicatum Tall willowweed x x Erigeron acris debilis Fieabane x x compositus do x compositus trifidus do x x salsuginosus .. ...do... X X X X 1 Taken in part from Piper (1906) and in part from lists of plants collected or identified in the field by the writer and checked by Morton E. Peck. At best the list is fragmentary, but the species are so grouped as to show the relationship of the Blue Mountain and Steens Mountain flora to that of both the Cascades on the west and the Rocky Mountains on the east. 1936] MAMMALS AND LIFE ZONES OF OREGON 53 TABLE 8. — Plants of the Arctic-Alpine Zone foi Oregon — Continued Species Common name Cas- cade Moun- tains Blue Moun- tains Steens Moun- tains Rocky Moun- tains Arctic Eriogonum coryphaeum (Buckwheat family) _ x x do X x x Eritrichiutn howardi Moss-forget-me-not Festuca, ovina brachyphylla Alpine fescue x X x X Greenleaf fescue X x X x Qentiana, calycosa Gentian x Alpine gilia X X x nuttallii Nuttallgilia x Hieracium gracile Hawkweed x x X X Alpine hulsea X X x Ivesia gordoni Chipmunktail x Juncus mertensianus Rush x x X x X parryi do X x X x subtriflorus do._ ... X X Lcptarrhena amplexifolia Saxifrage x Lewisid Columbians C olumbia bitterroot x nevadensis Nevada bitterroot . X x X x triphylla Threeleaf bitterroot x Lomatium angustatum.- . Biscuit root X x X x X X Lutkea pectinata Mountainmat . Mimulus alpinus Alpinfl TnimuHlS x X rubellus. ._ .. Red mimulus -.. X X x Oxyria digyna MnriTi tain-sorrel X X X X X Pedicularis contorta Fernleaf Pentstemon menziesii. Pentstemon.-. X x X menziesii davidsoni .do .. x 1 Phacelia sericea Curlyhloorn x X X X X Phleum aipinum Mountain timothy. X x X x X Phlox diffusa Phlox douglasii do X x X X X Phyllodoce glanduliflora Cream mountainheat h X Polygonum davisiae Polygonum x minimum do X x X X X newberryi do ...do— . X X X Potentilla flabellifolia Cinquefoil x dissecta, do x Pulsatilla occidentalis American pasqueflower x X X Ranunculus eschscholtzii Buttercup X suksdorfii do Salix nivalis Snow willow . x Saxifraga bongardi Saxifrage X X X X do tolmiei do x Scirpus caespitosus Sedge x X X Senecio fremontii Groundsel Sibbaldia procumbens Sibbaldia Sieversia rossii ... Sieversia. .. X X X X Silene acaulis Mr>ss narnpinn suksdorfii IVfoun tMn'caTnpinn x Smelowskia calycina Arctic crucifer X X Spraguea muUiceps Pussypaws X X umbellata do. Alpine pennycress X X x X X X X Thlaspi alpestre Trisetum spicatum Spike fisptnrri X X Veronica alpina Alpine speedwell X X 54 NOBTH AMEBICAN FAUNA [No. 65 MAMMALS OF OREGON AN IMPORTANT NATURAL RESOURCE Since the advent of the white man, the mammal life of Oregon has been an important factor in the development of the State, as it had been for ages before in maintaining the original native popula- tion. The quest of valuable furs brought hardy pioneers into the region, and the abundance of game enabled them to live and carry on extensive explorations that yielded a valuable knowledge of the country and its resources. As man and domestic animals filled the more fertile parts of the country, the abundance of native life de- creased; but in many parts of the State the game and fur-bearing animals still have a high value and can be maintained in reasonable numbers. Other forms of life destructive to game, livestock, poultry, and crops must be controlled and kept within reasonable bounds, while many of the useful species need careful protection and encour- agement. The merely harmless but interesting forms of small mammals may have a real value of interest and education that should not be overlooked in our human economy. Whatever may be our attitude toward the native wildlife, our course should be guided by a full knowledge of all of the species, their physical characters, dis- tribution, natural or controlled abundance, natural habits, and as far as possible their relations to our own lives and industries. The object of the present report is not only to give as full informa- tion as possible on all of the mammals of Oregon, but to give information that will enable others to go ahead with future studies based on present knowledge, until far better means for understand- ing, appreciating, managing, and controlling our native fauna are attained. A sequence of species has been adopted that brings many of the more important animals ahead of the smaller and more obscure kinds, and while not entirely in systematic order, this sequence seems logical for practical use. Both common and scientific names of the species are given, as well as native Indian names wherever possible, some of which eventually may well replace our names of less satisfactory application. Some of the native names were obtained direct from the Indians; others are quoted from manuscripts or publications as indicated by initials of the writers.2 Most of the measurements of the mammals are in millimeters as taken in the field by collectors and include total length, from tip of nose to tip of tail vertebrae in a straight line ; length of tail from tip of vertebrae to base with tail held straight at right angles to back; hind foot from tip of heel to tip of longest claw with toes held straight; and length of ear from the inner notch at base to tip, unless otherwise stated. 2Vernon Bailey, W. H. Dall, George M. Dawson, David Douglas, Luther J. Goldman, George Bird Grinnell, Lewis and Clark, Maximilian Prince of Wied, C. Hart Merriam, George Suckley, J. K. Townsend. 1936] MAMMALS AND LIFE ZONES OF OREGON 55 Weights are given in grams for the small mammals, and pounds and ounces for the larger species. The reports of the numbers of the larger mammals estimated to inhabit the various districts of the national forests (table 9), while rarely showing actual counts, are based on careful observations made throughout the year by rangers and supervisors and are the best records available of the numbers present on the forest areas. The national forests of Oregon cover nearly half the State and support much more than half the large game animals. The records are especially valuable as showing year by year the approximate increase or decrease of the species and as affording a basis for intelligent control efforts, or regulation of hunting. The annual game census of the Forest Service, district 6, for 1929, which has been selected because the data for that year are the most nearly complete for the various classes, gives the number of licensed hunters on the forests as 25,873; the number of mule deer killed by hunters as 2,864; black- tailed deer, 1,768; elk, 89; and black bear, 538. The report gives 7,113 deer and 19 elk killed by predatory animals. Other notes of interest in the report are 3,201 coyotes killed on the forests by Biological Survey hunters, 85 by forestry officials, and 3,043 by local hunters and trappers. Of bobcats, 295 are reported taken by the Biological Survey hunters, 12 by forestry officials, and 1,369 by local trappers. Of mountain lions, 9 are credited to the Biological Survey hunters, 1 to forestry officials, and 134 to local hunters. Elk, deer, antelope, sage grouse, and porcupines are reported to be increasing. Predatory animals are reported as generally decreasing in abundance. 56 NORTH AMERICAN FAUNA FNo. 55 a a 11 S«o o > °°Si ill3! «J O O rH 1^ ^^ O O SOOQ«OOOiOO> CO«OO^M05(NiO So :8 It-