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Bedded Range
The Bedded Range is a mountain range in the Hozameen Range subdivision of the Canadian Cascades, which are the extension of the Cascade Range into British Columbia, Canada. Located between the Coquihalla and Tulameen Rivers, the Bedded Range is a dioritic plug related to the Chilliwack batholith. Ecology A diverse flora and fauna exist in the Bedded Range. Fauna include mammals, amphibians and birds. In the case of amphibians, one of the species present is the Rough-skinned newt, ''Taricha granulosa'', whose populations exhibit an adult perennibranchiate Perennibranchiate, in zoology, is the condition of an organism retaining branchae, or gills, through life. This condition is generally said of certain amphibia, such as the mudpuppy. The term is opposed to caducibranchiate. In some cases only a sma ... form in approximately 90 percent of the population.C. Michael Hogan. 2008 References * Fred W. Beckey. 1995. ''Cascade Alpine Guide: Rainy Pass to Fraser River'', Published by T ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hozameen Range
The Hozameen Range (spelled Hozomeen Range in the United States) is a mountain range in southwestern British Columbia and northern Washington, straddling the division between the Coast and Interior regions of that province. It is a subrange of the North Cascades and is neighboured on the east by the Okanagan Range and on the northwest by the unofficially-named Coquihalla Range, which lies between that river and the Fraser. In the northwest part of the range is the one named subrange, the Bedded Range. There are differences of opinion about the location and boundaries of the subranges of the northern Cascades, although early geologists and topographers had a fundamental agreement on the topic. The Hozomeen Range was seen as bounded by the Skagit River on the west and extending east to the Pasayten River (east of the Sumallo River) and Coquihalla River. The core of the Hozomeen Range under this definition marks the divide between streams in British Columbia that flow west to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Diorite
Diorite ( ) is an intrusive igneous rock formed by the slow cooling underground of magma (molten rock) that has a moderate content of silica and a relatively low content of alkali metals. It is intermediate in composition between low-silica (mafic) gabbro and high-silica ( felsic) granite. Diorite is found in mountain-building belts (''orogens'') on the margins of continents. It has the same composition as the fine-grained volcanic rock, andesite, which is also common in orogens. Diorite has been used since prehistoric times as decorative stone. It was used by the Akkadian Empire of Sargon of Akkad for funerary sculptures, and by many later civilizations for sculptures and building stone. Description Diorite is an intrusive igneous rock composed principally of the silicate minerals plagioclase feldspar (typically andesine), biotite, hornblende, and sometimes pyroxene. The chemical composition of diorite is intermediate, between that of mafic gabbro and felsic grani ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Perennibranchiate
Perennibranchiate, in zoology, is the condition of an organism retaining branchae, or gills, through life. This condition is generally said of certain amphibia, such as the mudpuppy. The term is opposed to caducibranchiate. In some cases only a small proportion of a given amphibian population is perennibranchiate, but in other instances a preponderance of the individuals have an adult gill retention. For example, in the case of the Rough-skinned Newt in the Cascade Mountains populations, approximately ninety percent of the adult population is perennibranchiate.C. Michael Hogan, 2008 See also * Neoteny Neoteny (), also called juvenilization,Montagu, A. (1989). Growing Young. Bergin & Garvey: CT. is the delaying or slowing of the physiological, or somatic, development of an organism, typically an animal. Neoteny is found in modern humans compared ... References * William Benjamin Carpenter (1854) ''Principles of Comparative Physiology'', Published by Blanchard and Lea, 752 pages * ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taricha Granulosa
The rough-skinned newt or roughskin newt (''Taricha granulosa'') is a North American newt known for the strong toxin exuded from its skin. Appearance A stocky newt with rounded snout, it ranges from light brown to olive or brownish-black on top, with the underside, including the head, legs, and tail, a contrasting orange to yellow. The skin is granular, but males are smooth-skinned during breeding season. They measure 6 to 9 cm in snout-to-vent length, and 11 to 18 cm overall. They are similar to the California newt (''Taricha torosa'') but differ in having smaller eyes, yellow irises, V-shaped tooth patterns, and uniformly dark eyelids. Males can be distinguished from females during breeding season by large swollen vent lobes and cornified toe pads. Distribution and subspecies Habitats of rough-skinned newts are found throughout the Pacific Northwest. Their range extends south to Santa Cruz, California, and north to Alaska. They are uncommon east of the Cascade ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Rough-skinned Newt
The rough-skinned newt or roughskin newt (''Taricha granulosa'') is a North American newt known for the strong toxin exuded from its skin. Appearance A stocky newt with rounded snout, it ranges from light brown to olive or brownish-black on top, with the underside, including the head, legs, and tail, a contrasting orange to yellow. The skin is granular, but males are smooth-skinned during breeding season. They measure 6 to 9 cm in snout-to-vent length, and 11 to 18 cm overall. They are similar to the California newt (''Taricha torosa'') but differ in having smaller eyes, yellow irises, V-shaped tooth patterns, and uniformly dark eyelids. Males can be distinguished from females during breeding season by large swollen vent lobes and cornified toe pads. Distribution and subspecies Habitats of rough-skinned newts are found throughout the Pacific Northwest. Their range extends south to Santa Cruz, California, and north to Alaska. They are uncommon east of the Cascade ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Amphibian
Amphibians are tetrapod, four-limbed and ectothermic vertebrates of the Class (biology), class Amphibia. All living amphibians belong to the group Lissamphibia. They inhabit a wide variety of habitats, with most species living within terrestrial animal, terrestrial, fossorial, arboreal or freshwater aquatic ecosystems. Thus amphibians typically start out as larvae living in water, but some species have developed behavioural adaptations to bypass this. The young generally undergo metamorphosis from larva with gills to an adult air-breathing form with lungs. Amphibians use their skin as a secondary respiratory surface and some small terrestrial salamanders and frogs lack lungs and rely entirely on their skin. They are superficially similar to reptiles like lizards but, along with mammals and birds, reptiles are amniotes and do not require water bodies in which to breed. With their complex reproductive needs and permeable skins, amphibians are often ecological indicators; in re ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mammal
Mammals () are a group of vertebrate animals constituting the class Mammalia (), characterized by the presence of mammary glands which in females produce milk for feeding (nursing) their young, a neocortex (a region of the brain), fur or hair, and three middle ear bones. These characteristics distinguish them from reptiles (including birds) from which they diverged in the Carboniferous, over 300 million years ago. Around 6,400 extant species of mammals have been described divided into 29 orders. The largest orders, in terms of number of species, are the rodents, bats, and Eulipotyphla (hedgehogs, moles, shrews, and others). The next three are the Primates (including humans, apes, monkeys, and others), the Artiodactyla ( cetaceans and even-toed ungulates), and the Carnivora (cats, dogs, seals, and others). In terms of cladistics, which reflects evolutionary history, mammals are the only living members of the Synapsida (synapsids); this clade, together with Saur ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Chilliwack Batholith
The Chilliwack Batholith is a large batholith that forms much of the North Cascades in southwestern British Columbia, Canada and the U.S. state of Washington. The geological structure is named after the Chilliwack River Valley, where it outcrops in many places. It does not outcrop anywhere near the City of Chilliwack. The Chilliwack Batholith is part of the Pemberton Volcanic Belt and is the largest mass of exposed intrusive rock in the Cascade Volcanic Arc The Cascade Volcanoes (also known as the Cascade Volcanic Arc or the Cascade Arc) are a number of volcanoes in a volcanic arc in western North America, extending from southwestern British Columbia through Washington and Oregon to Northern Calif .... The age of the Chilliwack batholith ranges from 26 to 29 million years old. References Pemberton Volcanic Belt Igneous petrology of Washington (state) Batholiths of North America Igneous petrology of British Columbia Paleogene magmatism {{US-geology-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tulameen River
The Tulameen River is a tributary of the Similkameen River in the Canadian province of British Columbia. The Tulameen River is part of the Columbia River drainage basin, being a tributary of the Similkameen River, which flows into the Okanagan River, which flows into the Columbia River. Course The Tulameen River originates in E. C. Manning Provincial Park with headwaters at Punchbowl Lake, in the North Cascades part of the Cascade Range. it flows generally north then east, passing Tulameen, British Columbia before joining the Similkameen River at Princeton. It is the only place in the world where both gold and platinum can be found alongside each other, however all significant deposits have been mined. Ecology The watershed holds a number of diverse flora and fauna species. Fauna include mammals, amphibians, reptiles and birds. Among the amphibians of the watershed is the Rough-skinned newt, '' Taricha granulosa'', whose populations in the North Cascades exhibit an adult p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coquihalla Mountain
Coquihalla Mountain is an extinct stratovolcano in Similkameen Country, southwestern British Columbia, Canada, located south of Falls Lake and west of Tulameen between the Coquihalla and Tulameen rivers. With a topographic prominence of , it towers above adjacent mountain ridges. It is the highest mountain in the Bedded Range of the northern Canadian Cascades with an elevation of and lies near the physiographic boundaries with the Coast Mountains on the west and the Interior Plateau on the east. Geology Coquihalla Mountain is a major preserved feature in the Miocene age Pemberton Volcanic Belt that was erupting about 21 to 22 million years ago. Like the Pemberton Volcanic Belt, Coquihalla Mountain formed as result of Cascadia subduction. See also * Jim Kelly Peak *Volcanism of Canada *Volcanism of Western Canada Volcanism of Western Canada has produced lava flows, lava plateaus, lava domes, cinder cones, stratovolcanoes, shield volcanoes, greenstone belts, submarine volc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coquihalla River
The Coquihalla River (originally or more recently and popularly ) is a tributary of the Fraser River in the Cascade Mountains of the Canadian province of British Columbia. It originates in the Coquihalla Lakes and empties into the Fraser River at Hope. The Coquihalla River forms the northern boundary of two portions of the Cascades, the Skagit Range and the Hozameen Range. The river flows through a deep, narrow valley, dropping in , a tumultuous course that creates an incessant roar. ''Kw'ikw'iyá:la'' in the Halkomelem language of the '' Stó:lō'', is a place name meaning "stingy container" or "stingy place". It refers specifically to a deep pool named ''Skw'éxweq'' or ''Skw'exwáq'', near the mouth of what is now known as the Coquihalla River. The ''Stó:lō'' would go to this pool to spear suckerfish, which were plentiful there. According to ''Stó:lō'' oral history, the ''s'ó:lmexw'' (black-haired, 2-foot tall, dark-skinned underwater people) would grab the spears, prev ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Canada
Canada is a country in North America. Its ten provinces and three territories extend from the Atlantic Ocean to the Pacific Ocean and northward into the Arctic Ocean, covering over , making it the world's second-largest country by total area. Its southern and western border with the United States, stretching , is the world's longest binational land border. Canada's capital is Ottawa, and its three largest metropolitan areas are Toronto, Montreal, and Vancouver. Indigenous peoples have continuously inhabited what is now Canada for thousands of years. Beginning in the 16th century, British and French expeditions explored and later settled along the Atlantic coast. As a consequence of various armed conflicts, France ceded nearly all of its colonies in North America in 1763. In 1867, with the union of three British North American colonies through Confederation, Canada was formed as a federal dominion of four provinces. This began an accretion of provinces an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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