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Clarkia, Idaho
Clarkia is a small unincorporated community in the southwestern corner of Shoshone County, Idaho. It is surrounded by publicly and privately managed forest lands of Douglas-fir, Ponderosa Pine, and Western Larch. Located just to the east of State Highway 3, the town is in the drainage area of the West Fork of the St. Maries River. History The Coeur d’Alene people inhabited this area for thousands of years prior to the coming of white settlers. The native name of the area is Chatnna or Meadow. Clarkia is named for Capt. William Clark of the Lewis and Clark expedition. The first residents of the town of Clarkia harvested the Western White Pine in the area for lumber. Clarkia's population was 60 in 1909, and was estimated at 200 in 1960. Demographics The 2000 census recorded a population of 97 with an average household income of $39,375. The median age in Clarkia is 37.8 and the average household size is 2.68. In 2000 the agriculture industry made up 40.5% of the jobs in ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
United States
The United States of America (U.S.A. or USA), commonly known as the United States (U.S. or US) or America, is a country primarily located in North America. It consists of 50 states, a federal district, five major unincorporated territories, nine Minor Outlying Islands, and 326 Indian reservations. The United States is also in free association with three Pacific Island sovereign states: the Federated States of Micronesia, the Marshall Islands, and the Republic of Palau. It is the world's third-largest country by both land and total area. It shares land borders with Canada to its north and with Mexico to its south and has maritime borders with the Bahamas, Cuba, Russia, and other nations. With a population of over 333 million, it is the most populous country in the Americas and the third most populous in the world. The national capital of the United States is Washington, D.C. and its most populous city and principal financial center is New York City. Paleo-Americ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Avery, Idaho
Avery is a small unincorporated community in the northwest United States, located in the St. Joe River Valley in Shoshone County, Idaho. Avery is located in the middle of the St. Joe District of the Idaho Panhandle National Forest, and is a tourist attraction in the Idaho Panhandle known for its wilderness and outdoor recreation. It is upstream and east of St. Maries, the county seat of Benewah County. Geography Avery is located at a latitude of 47.25 ºN, longitude 115.81 ºW, and an elevation of 2562 ft (781m) above sea level. Climate This climatic region is typified by large seasonal temperature differences, with warm to hot (and often humid) summers and cold (sometimes severely cold) winters. According to the Köppen Climate Classification system, Avery has a humid continental climate, abbreviated "Dfb" on climate maps. Demographics As of 2013, Avery had a population of 25 permanent residents. The temporary population is higher in the summer though due to s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Humid Continental Climate
A humid continental climate is a climatic region defined by Russo-German climatologist Wladimir Köppen in 1900, typified by four distinct seasons and large seasonal temperature differences, with warm to hot (and often humid) summers and freezing cold (sometimes severely cold in the northern areas) winters. Precipitation is usually distributed throughout the year but often do have dry seasons. The definition of this climate regarding temperature is as follows: the mean temperature of the coldest month must be below or depending on the isotherm, and there must be at least four months whose mean temperatures are at or above . In addition, the location in question must not be semi-arid or arid. The cooler ''Dfb'', ''Dwb'', and ''Dsb'' subtypes are also known as hemiboreal climates. Humid continental climates are generally found between latitudes 30° N and 60° N, within the central and northeastern portions of North America, Europe, and Asia. They are rare and is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Climate
Climate is the long-term weather pattern in an area, typically averaged over 30 years. More rigorously, it is the mean and variability of meteorological variables over a time spanning from months to millions of years. Some of the meteorological variables that are commonly measured are temperature, humidity, atmospheric pressure, wind, and precipitation. In a broader sense, climate is the state of the components of the climate system, including the atmosphere, hydrosphere, cryosphere, lithosphere and biosphere and the interactions between them. The climate of a location is affected by its latitude/longitude, terrain, altitude, land use and nearby water bodies and their currents. Climates can be classified according to the average and typical variables, most commonly temperature and precipitation. The most widely used classification scheme was the Köppen climate classification. The Thornthwaite system, in use since 1948, incorporates evapotranspiration along wit ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bitterroot Mountains
The Northern and Central Bitterroot Range, collectively the Bitterroot Mountains ( Salish: čkʷlkʷqin), is the largest portion of the Bitterroot Range, part of the Rocky Mountains and Idaho Batholith, located in the panhandle of Idaho and westernmost Montana in the northwestern United States. The mountains encompass an area of . The mountains are bordered on the north by Lolo Creek, to the northeast by the Clark Fork, on the south by the Salmon River, on the east by the Bitterroot River and Valley, and on the west by the Selway and Lochsa Rivers. Its highest summit is Trapper Peak, at . __TOC__ Northern Bitterroot Range The Northern Bitterroot Range is the northernmost and shortest subrange of the Bitterroot Mountains. The Northern Bitterroots encompass and its two tallest peaks are the Rhodes Peak and the Quartz Benchmark. The Northern Bitterroots also contain a smaller subrange, the Grave Creek Range. The Grave Creek Range is in area and its highest peak ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Columbia River Plateau
The Columbia Plateau is a geologic and geographic region that lies across parts of the U.S. states of Washington, Oregon, and Idaho. It is a wide flood basalt plateau between the Cascade Range and the Rocky Mountains, cut through by the Columbia River. Geology During late Miocene and early Pliocene times, a flood basalt engulfed about of the Pacific Northwest, forming a large igneous province. Over a period of perhaps 10 to 15 million years, lava flow after lava flow poured out, ultimately accumulating to a thickness of more than 6,000 feet (1.8 km). As the molten rock came to the surface, the Earth's crust gradually sank into the space left by the rising lava. The Columbia River Basalt Group consists of seven formations: The Steens Basalt, Imnaha Basalt, Grande Ronde Basalt, Picture Gorge Basalt, Prineville Basalt, Wanapum Basalt, and Saddle Mountains Basalt. Many of these formations are subdivided into formal and informal members and flows. The subsidence of the cru ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saint Maries River
Saint Maries River is a river located in the U.S. state of Idaho. It is a tributary of Coeur d'Alene Lake and thus part of the Spokane River drainage basin and the Columbia River Basin. The west and middle forks of the river join near Clarkia, Idaho, and run parallel to State Highway 3 in a northwesterly direction to St. Maries, Idaho. The area is on the eastern edge of the Columbia River Plateau and is to the west of the Bitterroot Mountains. The river's discharge is estimated at 583 cubic feet per second at its mouth in the town of St. Maries. Saint Maries River flows through Benewah County, Idaho and Shoshone County, Idaho. See also *Tributaries of the Columbia River Tributaries and sub-tributaries are hierarchically listed in order from the mouth of the Columbia River upstream. Major dams and reservoir lakes are also noted. List of major tributaries The main river and tributaries are (sorted in order from ... References Rivers of Idaho Rivers of Benewah Cou ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Miocene
The Miocene ( ) is the first epoch (geology), geological epoch of the Neogene Period and extends from about (Ma). The Miocene was named by Scottish geologist Charles Lyell; the name comes from the Greek words (', "less") and (', "new") and means "less recent" because it has 18% fewer modern marine invertebrates than the Pliocene has. The Miocene is preceded by the Oligocene and is followed by the Pliocene. As Earth went from the Oligocene through the Miocene and into the Pliocene, the climate slowly cooled towards a series of ice ages. The Miocene boundaries are not marked by a single distinct global event but consist rather of regionally defined boundaries between the warmer Oligocene and the cooler Pliocene Epoch. During the Early Miocene, the Arabian Peninsula collided with Eurasia, severing the connection between the Mediterranean and Indian Ocean, and allowing a faunal interchange to occur between Eurasia and Africa, including the dispersal of proboscideans into Eurasia. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Deary, Idaho
Deary is a city in Latah County, Idaho. The population was 506 at the time of the 2010 census, down from 552 in 2000.Spokesman-Review - 2010 census - Deary, Idaho - accessed 2011-12-26 It is located east of and northeast of Lewiston. History The settlement began as a waystation on the road to the forests at Bovill, Idaho. Owned by two African-Americans, Joe and Lou Wells, the waystation location was first called "Spud Hill", and then "Anderson". The settlement was ...[...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Calder, Idaho
Calder is an unincorporated community in Shoshone County, Idaho, United States. Calder is located on the Saint Joe River east of St. Maries. Calder has a post office A post office is a public facility and a retailer that provides mail services, such as accepting letters and parcels, providing post office boxes, and selling postage stamps, packaging, and stationery. Post offices may offer additional ser ... with ZIP code 83808. History Calder's population was 75 in 1909, and was also 75 in 1960. References Unincorporated communities in Shoshone County, Idaho Unincorporated communities in Idaho {{ShoshoneCountyID-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
