Library of Congress Classification
The Library of Congress Classification is a system of library classification developed by the Library of Congress. It is used by most research and academic libraries in the U. S. and several other countries. LCC should not be confused with LCCN, the system of Library of Congress Control Numbers assigned to all books, which defines URLs of their online catalog entries, such as "82006074" and "http://lccn.loc.gov/82006074". The Classification is distinct from Library of Congress Subject Headings, the system of labels such as "Boarding schools" and "Boarding schools—Fiction" that describe contents systematically; the classifications may be distinguished from the call numbers assigned to particular copies of books in the collection, such as "PZ7. J684 Wj 1982 FT MEADE Copy 1" where the classification is "PZ7. J684 Wj 1982"; the classification was invented by Herbert Putnam in 1897, just before he assumed the librarianship of Congress. With advice from Charles Ammi Cutter, it was influenced by his Cutter Expansive Classification, the Dewey Decimal System, the Putnam Classification System.
It was designed for the purposes and collection of the Library of Congress to replace the fixed location system developed by Thomas Jefferson. By the time Putnam departed from his post in 1939, all the classes except K and parts of B were well developed. LCC has been criticized for lacking a sound theoretical basis. Although it divides subjects into broad categories, it is enumerative in nature; that is, it provides a guide to the books in one library's collections, not a classification of the world. In 2007 The Wall Street Journal reported that in the countries it surveyed most public libraries and small academic libraries used the older Dewey Decimal Classification system; the National Library of Medicine classification system uses the initial letters W and QS–QZ, which are not used by LCC. Some libraries use NLM in conjunction with LCC. Others include Medicine R. Subclass AC -- Collections. Series. Collected works Subclass AE – Encyclopedias Subclass AG – Dictionaries and other general reference works Subclass AI – Indexes Subclass AM – Museums.
Collectors and collecting Subclass AN – Newspapers Subclass AP – Periodicals Subclass AS – Academies and learned societies Subclass AY – Yearbooks. Almanacs. Directories Subclass AZ – History of scholarship and learning; the humanities Subclass B – Philosophy Subclass BC – Logic Subclass BD – Speculative philosophy Subclass BF – Psychology Subclass BH – Aesthetics Subclass BJ – Ethics Subclass BL – Religions. Mythology. Rationalism Subclass BM – Judaism Subclass BP – Islam. Bahaism. Theosophy, etc. Subclass BQ – Buddhism Subclass BR – Christianity Subclass BS – The Bible Subclass BT – Doctrinal theology Subclass BV – Practical Theology Subclass BX – Christian Denominations Subclass C – Auxiliary Sciences of History Subclass CB – History of Civilization Subclass CC – Archaeology Subclass CD – Diplomatics. Archives. Seals Subclass CE – Technical Chronology. Calendar Subclass CJ – Numismatics Subclass CN – Inscriptions. Epigraphy Subclass CR – Heraldry Subclass CS – Genealogy Subclass CT – Biography Subclass D – History Subclass DA – Great Britain Subclass DAW – Central Europe Subclass DB – Austria – Liechtenstein – Hungary – Czechoslovakia Subclass DC – France – Andorra – Monaco Subclass DD – Germany Subclass DE – Greco-Roman World Subclass DF – Greece Subclass DG – Italy – Malta Subclass DH – Low Countries – Benelux Countries Subclass DJ – Netherlands Subclass DJK – Eastern Europe Subclass DK – Russia.
Soviet Union. Former Soviet Republics – Poland Subclass DL – Northern Europe. Scandinavia Subclass DP – Spain – Portugal Subclass DQ – Switzerland Subclass DR – Balkan Peninsula Subclass DS – Asia Subclass DT – Africa Subclass DU – Oceania Subclass DX – Romanies Class E does not have any subclasses. Class F does not have any subclasses, however Canadian Universities and the Canadian National Library use FC for Canadian History, a subclass that the LC has not adopted, but which it has agreed not to use for anything else Subclass G – Geography. Atlases. Maps Subclass GA – Mathematical geography. Cartography Subclass GB – Physical geography Subclass GC – Oceanography Subclass GE – Environmental Sciences Subclass GF – Human ecology. Anthropogeography Subclass GN – Anthropology Subclass GR – Folklore Subclass GT – Manners and customs Subclass GV – Recreation. Leisure Subclass H – Social sciences Subclass HA – Statistics Subclass HB – Economic theory. Demography Subclass HC – Economic history and conditions Subclass HD – Industries.
Land use. Labor Subclass HE – Transportation and communications Subclass HF – Commerce Subclass HG – Finance Subclass HJ – Public finance Subclass HM – Sociology Subclass HN – Social history and conditions. Social problems. Social reform Subclass HQ – The family. Marriage and Sexuality Subclass HS – Societies: secret, etc. Subclass HT – Communities. Classes. Races Subclass HV – Social pathology. Social and public welfare. Criminology Subclass HX – Socialism. Communism. Anarchism Subclass J – General legislative and executive papers Subclass JA – Political science Subclass JC – Political theory Subclass JF – Political institutions and public administration Subclass JJ – Political institutions and public administration Subclass JK – Political institutions and public administration Subclass JL – Political instit
Idaho is a state in the northwestern region of the United States. It borders the state of Montana to the east and northeast, Wyoming to the east and Utah to the south, Washington and Oregon to the west. To the north, it shares a small portion of the Canadian border with the province of British Columbia. With a population of 1.7 million and an area of 83,569 square miles, Idaho is the 14th largest, the 12th least populous and the 7th least densely populated of the 50 U. S. states. The state's capital and largest city is Boise. Idaho prior to European settlement was inhabited by Native American peoples, some of whom still live in the area. In the early 19th century, Idaho was considered part of the Oregon Country, an area disputed between the U. S. and the United Kingdom. It became U. S. territory with the signing of the Oregon Treaty of 1846, but a separate Idaho Territory was not organized until 1863, instead being included for periods in Oregon Territory and Washington Territory. Idaho was admitted to the Union on July 3, 1890, becoming the 43rd state.
Forming part of the Pacific Northwest, Idaho is divided into several distinct geographic and climatic regions. In the state's north, the isolated Idaho Panhandle is linked with Eastern Washington, with which it shares the Pacific Time Zone – the rest of the state uses the Mountain Time Zone; the state's south includes the Snake River Plain, while the south-east incorporates part of the Great Basin. Idaho is quite mountainous, contains several stretches of the Rocky Mountains; the United States Forest Service holds about 38 % of the most of any state. Industries significant for the state economy include manufacturing, mining and tourism. A number of science and technology firms are either headquartered in Idaho or have factories there, the state contains the Idaho National Laboratory, the country's largest Department of Energy facility. Idaho's agricultural sector supplies many products, but the state is best known for its potato crop, which comprises around one-third of the nationwide yield; the official state nickname is the "Gem State".
The name's origin remains a mystery. In the early 1860s, when the United States Congress was considering organizing a new territory in the Rocky Mountains, eccentric lobbyist George M. Willing suggested the name "Idaho", which he claimed was derived from a Shoshone language term meaning "the sun comes from the mountains" or "gem of the mountains". Willing claimed he had invented the name. Congress decided to name the area Colorado Territory when it was created in February 1861. Thinking they would get a jump on the name, locals named a community in Colorado "Idaho Springs". However, the name "Idaho" did not fall into obscurity; the same year Congress created Colorado Territory, a county called Idaho County was created in eastern Washington Territory. The county was named after a steamship named Idaho, launched on the Columbia River in 1860, it is unclear after Willing's claim was revealed. Regardless, part of Washington Territory, including Idaho County, was used to create Idaho Territory in 1863.
Despite this lack of evidence for the origin of the name, many textbooks well into the 20th century repeated as fact Willing's account the name "Idaho" derived from the Shoshone term "ee-da-how". A 1956 Idaho history textbook says:"Idaho" is a Shoshoni Indian exclamation; the word consists of three parts. The first is "Ee", which in English conveys the idea of "coming down"; the second is "dah", the Shoshoni stem or root for both "sun" and "mountain". The third syllable, "how", denotes the exclamation and stands for the same thing in Shoshoni that the exclamation mark does in the English language; the Shoshoni word is "Ee-dah-how", the Indian thought thus conveyed when translated into English means, "Behold! the sun coming down the mountain. An alternative etymology attributes the name to the Plains Apache word "ídaahę́", used in reference to The Comanche. Idaho borders six U. S. states and one Canadian province. The states of Washington and Oregon are to the west and Utah are to the south, Montana and Wyoming are to the east.
Idaho shares a short border with the Canadian province of British Columbia to the north. The landscape is rugged with some of the largest unspoiled natural areas in the United States. For example, at 2.3 million acres, the Frank Church-River of No Return Wilderness Area is the largest contiguous area of protected wilderness in the continental United States. Idaho is a Rocky Mountain state with scenic areas; the state has snow-capped mountain ranges, vast lakes and steep canyons. The waters of the Snake River rush through the deepest gorge in the United States. Shoshone Falls plunges down rugged cliffs from a height greater than Niagara Falls; the major rivers in Idaho are the Snake River, the Clark Fork/Pend Oreille River, the Clearwater River, the Salmon River. Other significant rivers include the Coeur d'Alene River, the Spokane River, the Boise River, the Payette River; the Salmon River empties into the Snake in Hells Canyon and forms the southern boundary of Nez Perce County on its north shore, of which Lewiston is the county seat.
The Port of Lewiston, at the confluence of the Clearwater and the Snake Rivers is the farthest inland seaport on the West Coast at 465 river miles from the Pacific at Astoria, Oregon. Idaho's highest point is 12,662 ft, in the Lost River Range north of Mackay. Idaho's lowest poi
A seed is an embryonic plant enclosed in a protective outer covering. The formation of the seed is part of the process of reproduction in seed plants, the spermatophytes, including the gymnosperm and angiosperm plants. Seeds are the product of the ripened ovule, after fertilization by pollen and some growth within the mother plant; the embryo is developed from the seed coat from the integuments of the ovule. Seeds have been an important development in the reproduction and success of gymnosperm and angiosperm plants, relative to more primitive plants such as ferns and liverworts, which do not have seeds and use water-dependent means to propagate themselves. Seed plants now dominate biological niches on land, from forests to grasslands both in hot and cold climates; the term "seed" has a general meaning that antedates the above – anything that can be sown, e.g. "seed" potatoes, "seeds" of corn or sunflower "seeds". In the case of sunflower and corn "seeds", what is sown is the seed enclosed in a shell or husk, whereas the potato is a tuber.
Many structures referred to as "seeds" are dry fruits. Plants producing berries are called baccate. Sunflower seeds are sometimes sold commercially while still enclosed within the hard wall of the fruit, which must be split open to reach the seed. Different groups of plants have other modifications, the so-called stone fruits have a hardened fruit layer fused to and surrounding the actual seed. Nuts are the one-seeded, hard-shelled fruit of some plants with an indehiscent seed, such as an acorn or hazelnut. Seeds are produced in several related groups of plants, their manner of production distinguishes the angiosperms from the gymnosperms. Angiosperm seeds are produced in a hard or fleshy structure called a fruit that encloses the seeds for protection in order to secure healthy growth; some fruits have layers of both fleshy material. In gymnosperms, no special structure develops to enclose the seeds, which begin their development "naked" on the bracts of cones. However, the seeds do become covered by the cone scales.
Seed production in natural plant populations varies from year to year in response to weather variables and diseases, internal cycles within the plants themselves. Over a 20-year period, for example, forests composed of loblolly pine and shortleaf pine produced from 0 to nearly 5 million sound pine seeds per hectare. Over this period, there were six bumper, five poor, nine good seed crops, when evaluated for production of adequate seedlings for natural forest reproduction. Angiosperm seeds consist of three genetically distinct constituents: the embryo formed from the zygote, the endosperm, triploid, the seed coat from tissue derived from the maternal tissue of the ovule. In angiosperms, the process of seed development begins with double fertilization, which involves the fusion of two male gametes with the egg cell and the central cell to form the primary endosperm and the zygote. Right after fertilization, the zygote is inactive, but the primary endosperm divides to form the endosperm tissue.
This tissue becomes the food the young plant will consume until the roots have developed after germination. After fertilization the ovules develop into the seeds; the ovule consists of a number of components: The funicle or seed stalk which attaches the ovule to the placenta and hence ovary or fruit wall, at the pericarp. The nucellus, the remnant of the megasporangium and main region of the ovule where the megagametophyte develops; the micropyle, a small pore or opening in the apex of the integument of the ovule where the pollen tube enters during the process of fertilization. The chalaza, the base of the ovule opposite the micropyle, where integument and nucellus are joined together; the shape of the ovules as they develop affects the final shape of the seeds. Plants produce ovules of four shapes: the most common shape is called anatropous, with a curved shape. Orthotropous ovules are straight with all the parts of the ovule lined up in a long row producing an uncurved seed. Campylotropous ovules have a curved megagametophyte giving the seed a tight "C" shape.
The last ovule shape is called amphitropous, where the ovule is inverted and turned back 90 degrees on its stalk. In the majority of flowering plants, the zygote's first division is transversely oriented in regards to the long axis, this establishes the polarity of the embryo; the upper or chalazal pole becomes the main area of growth of the embryo, while the lower or micropylar pole produces the stalk-like suspensor that attaches to the micropyle. The suspensor absorbs and manufactures nutrients from the endosperm that are used during the embryo's growth; the main components of the embryo are: The cotyledons, the seed leaves, attached to the embryonic axis. There may be two; the cotyledons are the source of nutrients in the non-endospermic dicotyledons, in which case they replace the endosperm, are thick and leathery. In endospermic seeds the cotyledons are papery. Dicotyledons have the point of attachment opposite one another on the axis; the epicotyl, the embryonic axis above the point of attachment of the cotyledon.
The plumule, the tip of the epicotyl, has a feathery appearance due to the presence of young leaf primordia at the apex, will become the shoot upon germination. The hypocotyl, the embryonic axis below the point of attachment of the cotyledon, connecting the epicotyl and the radicle, being the stem-root transition zone; the radicle, the basal tip of the hy
Sierra Nevada (U.S.)
The Sierra Nevada is a mountain range in the Western United States, between the Central Valley of California and the Great Basin. The vast majority of the range lies in the state of California, although the Carson Range spur lies in Nevada; the Sierra Nevada is part of the American Cordillera, a chain of mountain ranges that consists of an continuous sequence of such ranges that form the western "backbone" of North America, Central America, South America and Antarctica. The Sierra runs 400 miles north-to-south, is 70 miles across east-to-west. Notable Sierra features include the largest alpine lake in North America; the Sierra is home to three national parks, twenty wilderness areas, two national monuments. These areas include Yosemite and Kings Canyon National Parks; the character of the range is shaped by its ecology. More than one hundred million years ago during the Nevadan orogeny, granite formed deep underground; the range started to uplift four million years ago, erosion by glaciers exposed the granite and formed the light-colored mountains and cliffs that make up the range.
The uplift caused a wide range of elevations and climates in the Sierra Nevada, which are reflected by the presence of five life zones. Uplift continues due to faulting caused by tectonic forces, creating spectacular fault block escarpments along the eastern edge of the southern Sierra; the Sierra Nevada has a significant history. The California Gold Rush occurred in the western foothills from 1848 through 1855. Due to inaccessibility, the range was not explored until 1912; the Sierra Nevada lies in Central and Eastern California, with a small but important spur extending into Nevada. West-to-east, the Sierra Nevada's elevation increases from 1,000 feet in the Central Valley to heights of about 14,000 feet at its crest 50–75 miles to the east; the east slope forms the steep Sierra Escarpment. Unlike its surroundings, the range receives a substantial amount of snowfall and precipitation due to orographic lift; the Sierra Nevada's irregular northern boundary stretches from the Susan River and Fredonyer Pass to the North Fork Feather River.
It represents where the granitic bedrock of the Sierra Nevada dives below the southern extent of Cenozoic igneous surface rock from the Cascade Range. It is bounded on the west by California's Central Valley and on the east by the Basin and Range Province; the southern boundary is at Tehachapi Pass. Physiographically, the Sierra is a section of the Cascade-Sierra Mountains province, which in turn is part of the larger Pacific Mountain System physiographic division; the California Geological Survey states that "the northern Sierra boundary is marked where bedrock disappears under the Cenozoic volcanic cover of the Cascade Range." The range is drained on its western slope by the Central Valley watershed, which discharges into the Pacific Ocean at San Francisco. The northern third of the western Sierra is part of the Sacramento River watershed, the middle third is drained by the San Joaquin River; the southern third of the range is drained by the Kings, Kaweah and Kern rivers, which flow into the endorheic basin of Tulare Lake, which overflows into the San Joaquin during wet years.
The eastern slope watershed of the Sierra is much narrower. From north to south, the Susan River flows into intermittent Honey Lake, the Truckee River flows from Lake Tahoe into Pyramid Lake, the Carson River runs into Carson Sink, the Walker River into Walker Lake. Although none of the eastern rivers reach the sea, many of the streams from Mono Lake southwards are diverted into the Los Angeles Aqueduct which provides water to Southern California; the height of the mountains in the Sierra Nevada increases from north to south. Between Fredonyer Pass and Lake Tahoe, the peaks range from 5,000 feet to more than 9,000 feet; the crest near Lake Tahoe is 9,000 feet high, with several peaks approaching the height of Freel Peak. Farther south, the highest peak in Yosemite National Park is Mount Lyell; the Sierra rises to 14,000 feet with Mount Humphreys near Bishop, California. Near Lone Pine, Mount Whitney is at 14,505 feet, the highest point in the contiguous United States. South of Mount Whitney, the elevation of the range dwindles.
The crest elevation is 10,000 feet near Lake Isabella, but south of the lake, the peaks reach to only a modest 8,000 feet. There are several notable geographical features in the Sierra Nevada: Lake Tahoe is a large, clear freshwater lake in the northern Sierra Nevada, with an elevation of 6,225 ft and an area of 191 sq mi. Lake Tahoe lies between a spur of the Sierra. Hetch Hetchy Valley, Yosemite Valley, Kings Canyon, Kern Canyon are examples of many glacially-scoured canyons on the west side of the Sierra. Yosemite National Park is filled with notable features such as waterfalls, granite domes, high mountains and meadows. Groves of Giant Sequoia
The Cascade Range or Cascades is a major mountain range of western North America, extending from southern British Columbia through Washington and Oregon to Northern California. It includes both non-volcanic mountains, such as the North Cascades, the notable volcanoes known as the High Cascades; the small part of the range in British Columbia is referred to as the Canadian Cascades or, locally, as the Cascade Mountains. The latter term is sometimes used by Washington residents to refer to the Washington section of the Cascades in addition to North Cascades, the more usual U. S. term, as in North Cascades National Park. The highest peak in the range is Mount Rainier in Washington at 14,411 feet; the Cascades are part of the Pacific Ocean's Ring of Fire, the ring of volcanoes and associated mountains around the Pacific Ocean. All of the eruptions in the contiguous United States over the last 200 years have been from Cascade volcanoes; the two most recent were Lassen Peak from 1914 to 1921 and a major eruption of Mount St. Helens in 1980.
Minor eruptions of Mount St. Helens have occurred since, most from 2004 to 2008; the Cascade Range is a part of the American Cordillera, a nearly continuous chain of mountain ranges that form the western "backbone" of North America, Central America, South America. The Cascades extend northward from Lassen Peak in northern California to the confluence of the Nicola and Thompson rivers in British Columbia; the Fraser River separates the Cascades from the Coast Mountains in Canada, as does the Willamette Valley from the upper portion of the Oregon Coast Range. The highest volcanoes of the Cascades, known as the High Cascades, dominate their surroundings standing twice the height of the nearby mountains, they have a visual height of one mile or more. The highest peaks, such as the 14,411-foot Mount Rainier, dominate their surroundings for 50 to 100 miles; the northern part of the range, north of Mount Rainier, is known as the North Cascades in the United States but is formally named the Cascade Mountains north of the Canada–United States border, reaching to the northern extremity of the Cascades at Lytton Mountain.
Overall, the North Cascades and Canadian Cascades are rugged. The southern part of the Canadian Cascades the Skagit Range, is geologically and topographically similar to the North Cascades, while the northern and northeastern parts are less glaciated and more plateau-like, resembling nearby areas of the Thompson Plateau; because of the range's proximity to the Pacific Ocean and the region's prevailing westerly winds, precipitation is substantial on the western slopes due to orographic lift, with annual snow accumulations of up to 1,000 inches in some areas. Mount Baker in Washington recorded a national record single-season snowfall in the winter of 1998–99 with 1,140 inches. Prior to that year, Mount Rainier held the American record for snow accumulation at Paradise in 1978, it is not uncommon for some places in the Cascades to have over 500 inches of annual snow accumulation, such as at Lake Helen, near Lassen Peak. Most of the High Cascades are therefore white with ice year-round; the western slopes are densely covered with Douglas-fir, western hemlock and red alder, while the drier eastern slopes feature ponderosa pine, with some western larch, mountain hemlock and subalpine fir and subalpine larch at higher elevations.
Annual rainfall is as low as 9 inches on the eastern foothills due to a rain shadow effect. Beyond the eastern foothills is an arid plateau, created 17 to 14 million years ago by the many flows of the Columbia River Basalt Group. Together, these sequences of fluid volcanic rock form the 200,000-square-mile Columbia Plateau in eastern Washington and parts of western Idaho; the Columbia River Gorge is the only major break of the range in the United States. When the Cascades began to rise 7 million years ago in the Pliocene, the Columbia River drained the low Columbia Plateau; as the range grew, erosion from the Columbia River was able to keep pace, creating the gorge and major pass seen today. The gorge exposes uplifted and warped layers of basalt from the plateau. Indigenous peoples have inhabited the area for thousands of years and developed their own myths and legends about the Cascades. In these legends, St. Helens with its pre-1980 graceful appearance, was regarded as a beautiful maiden for whom Hood and Adams feuded.
Native tribes developed their own names for the High Cascades and many of the smaller peaks, including "Tahoma", the Lushootseed name for Mount Rainier, "Koma Kulshan" or "Kulshan" for Mount Baker, "Louwala-Clough", meaning "smoking mountain" for Mount St. Helens. In early 1792, British navigator George Vancouver explored Puget Sound and gave English names to the high mountains he saw. Mount Baker was named for Vancouver's third lieutenant, Joseph Baker, although the first European to see it was Manuel Quimper, who named it la gran montaña del Carmelo in 1790. Mount Rainier was named after Admiral Peter Rainier. In 1792, Vancouver had his lieutenant William Robert Broughton explore the lower Columbia River, he named Mount Hood after an admiral of the Royal Navy. Mount St. Helens was sighted by Vancouver from near the mouth of the Columbia River, it was named for Al
Pinus ponderosa known as the ponderosa pine, bull pine, blackjack pine, or western yellow-pine, is a large pine tree species of variable habitat native to the western United States and Canada. It is the most distributed pine species in North America, it grows in various erect forms from British Columbia southward and eastward through 16 western U. S. states and has been introduced in temperate regions of Europe. It was first documented into modern science in 1826 in eastern Washington near present-day Spokane. On that occasion, David Douglas misidentified it as Pinus resinosa. In 1829, Douglas concluded that he had a new pine among his specimens and coined the name Pinus ponderosa for its heavy wood. In 1836, it was formally described by Charles Lawson, a Scottish nurseryman, it is the official state tree of Montana. Pinus ponderosa is a large coniferous pine tree; the bark helps to distinguish it from other species. Mature to over-mature individuals have yellow to orange-red bark in broad to broad plates with black crevices.
Younger trees have blackish-brown bark, referred to as "blackjacks" by early loggers. Ponderosa pine's five subspecies, as classified by some botanists, can be identified by their characteristically bright-green needles; the Pacific subspecies has the longest—7.8 in —and most flexible needles in plume-like fascicles of three. The Columbia ponderosa pine has long—4.7–8.1 in —and flexible needles in fascicles of three. The Rocky Mountains subspecies has shorter—3.6–5.7 in —and stout needles growing in scopulate fascicles of two or three. The southwestern subspecies has 4.4–7.8 in, stout needles in fascicles of three. The central High Plains subspecies is characterized by the fewest needles. Needles are widest and fewest for the species. Sources differ on the scent of P. ponderosa. Some state. Others state that it has no distinctive scent, while still others state that the bark smells like vanilla if sampled from a furrow of the bark. Sources agree that the Jeffrey pine is more scented than the ponderosa pine.
The National Register of Big Trees lists a Ponderosa Pine, 235 ft tall and 324 in in circumference. In January 2011, a Pacific ponderosa pine in the Rogue River–Siskiyou National Forest in Oregon was measured with a laser to be 268.35 ft high. The measurement was performed by Michael Taylor and Mario Vaden, a professional arborist from Oregon; the tree was climbed on October 13, 2011, by Ascending The Giants and directly measured with tape-line at 268.29 ft high. This is the second tallest known pine after the sugar pine; this species is grown as an ornamental plant in large gardens. During Operation Upshot–Knothole in 1953, a nuclear test was performed in which 145 ponderosa pines were cut down by the United States Forest Service and transported to Area 5 of the Nevada Test Site, where they were planted into the ground and exposed to a nuclear blast to see what the blast wave would do to a forest; the trees were burned and blown over. Pinus ponderosa is a dominant tree in the ponderosa shrub forest.
Like most western pines, the ponderosa is associated with mountainous topography. However, it is found on banks of the Niobrara River in Nebraska. Scattered stands occur in the Willamette Valley of Oregon and in the Okanagan Valley and Puget Sound areas of Washington. Stands occur throughout low level valleys in British Columbia reaching as far north as the Thompson and Columbia watersheds. In its Northern limits, it is most common below 800m. Ponderosa covers 80 %, of the Black Hills of South Dakota, it is found on foothills and mid-height peaks of the northern and southern Rocky Mountains, in the Cascade Range, in the Sierra Nevada, in the maritime-influenced Coast Range. In Arizona, it predominates on the Mogollon Rim and is scattered on the Mogollon Plateau and on mid-height peaks in Arizona and New Mexico, it does not extend into Mexico. The fire cycle for ponderosa pine is 5 to 10 years, in which a natural ignition sparks a low-intensity fire. Pinus ponderosa needles are the only known food of the caterpillars of the gelechiid moth Chionodes retiniella.
Blue stain fungus, Grosmannia clavigera, is introduced in sapwood of P. ponderosa from the galleries of all species in the genus Dendroctonus, which has caused much damage. Modern forestry research has identified five different taxa of P. ponderosa, with differing botanical characters and adaptations to different climatic conditions. Four of these have been termed "geographic races" in forestry literature; some botanists treated some races as distinct species. In modern botanical usage, they have been formally published. Pinus ponderosa subsp. Brachyptera Engelm. — southwestern ponderosa pine. Four corners transition zone including southern Colorado, southern Utah and central New Mexico and Arizona, westernmost Texas, a single disjunct population in the far northwestern Oklahoma panhandle; the Gila Wilderness conta
Junipers are coniferous plants in the genus Juniperus of the cypress family Cupressaceae. Depending on taxonomic viewpoint, between 50 and 67 species of junipers are distributed throughout the Northern Hemisphere, from the Arctic, south to tropical Africa, from Ziarat, east to eastern Tibet in the Old World, in the mountains of Central America; the highest-known juniper forest occurs at an altitude of 16,000 ft in southeastern Tibet and the northern Himalayas, creating one of the highest tree-lines on earth. Junipers vary in size and shape from tall trees, 20–40 m tall, to columnar or low-spreading shrubs with long, trailing branches, they are evergreen with needle-like and/or scale-like leaves. They can be either dioecious; the female seed cones are distinctive, with fleshy, fruit-like coalescing scales which fuse together to form a "berry"-like structure, 4–27 mm long, with one to 12 unwinged, hard-shelled seeds. In some species, these "berries" are red-brown or orange; the seed maturation time varies between species from 6 to 18 months after pollination.
The male cones are similar to those of other Cupressaceae, with six to 20 scales. In zones 7 through 10, junipers can release pollen several times each year. A few species of junipers bloom in autumn, while most species pollinate from early winter until late spring. Many junipers have two types of leaves; when juvenile foliage occurs on mature plants, it is most found on shaded shoots, with adult foliage in full sunlight. Leaves on fast-growing'whip' shoots are intermediate between juvenile and adult. In some species, all the foliage is with no scale leaves. In some of these, the needles are jointed at the base, in others, the needles merge smoothly with the stem, not jointed; the needle-leaves of junipers are hard and sharp, making the juvenile foliage prickly to handle. This can be a valuable identification feature in seedlings, as the otherwise similar juvenile foliage of cypresses and other related genera is soft and not prickly. Juniper is the exclusive food plant of the larvae of some Lepidoptera species, including Bucculatrix inusitata and juniper carpet, is eaten by the larvae of other Lepidoptera species such as Chionodes electella, Chionodes viduella, juniper pug, pine beauty.
Junipers are gymnosperms, which means they have no flowers or fruits. Depending on the species, the seeds they produce take 1 -- 3 years; the impermeable coat of the seed keeps water from getting in and protects the embryo when being dispersed. It can result in a long dormancy, broken by physically damaging the seed coat. Dispersal can occur from being swallowed whole by mammals; the resistance of the seed coat allows it to be passed down through the digestive system and out without being destroyed along the way. These seeds last a long time, as they can be dispersed long distances over the course of a few years; the number of juniper species is in dispute, with two recent studies giving different totals, Farjon accepting 52 species, Adams accepting 67 species. The junipers are divided into several sections, though which species belong to which sections is still far from clear, with research still on-going; the section Juniperus is an obvious monophyletic group though. Juniperus sect. Juniperus: Needle-leaf junipers.
The adult leaves are needle-like, in whorls of three, jointed at the base. Juniperus sect. Juniperus subsect. Juniperus: Cones with 3 separate seeds. Juniperus communis – Common juniper Juniperus communis subsp. Alpina – Alpine juniper Juniperus conferta – Shore juniper Juniperus rigida – Temple juniper or needle juniper Juniperus sect. Juniperus subsect. Oxycedrus: Cones with 3 separate seeds. Juniperus brevifolia – Azores juniper Juniperus cedrus – Canary Islands juniper Juniperus deltoides – Eastern prickly juniper Juniperus formosana – Chinese prickly juniper Juniperus lutchuensis – Ryukyu juniper Juniperus navicularis – Portuguese prickly juniper Juniperus oxycedrus – Western prickly juniper or cade juniper Juniperus macrocarpa – Large-berry juniper Juniperus sect. Juniperus subsect. Caryocedrus: Cones with 3 seeds fused together. Juniperus drupacea – Syrian juniperJuniperus sect. Sabina: Scale-leaf junipers; the adult leaves are scale-like, similar to those of Cupressus species, in opposite pairs or whorls of three, the juvenile needle-like leaves are not jointed at the base.
Provisionally, all the other junipers are included here. Old World species Juniperus chinensis – Chinese juniper Juniperus convallium – Mekong juniper Juniperus excelsa – Greek juniper Juniperus excelsa polycarpos – Persian juniper Juniperus foetidissima – Stinking juniper Juniperus indica – Black juniper Juniperus komarovii – Komarov's juniper Juniperus phoenicea – Phoenicean juniper Juniperus pingii – Ping juniper Juniperus procera – East African juniper Juniperus procumbens – Ibuki juniper Juniperu