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Cape Alava
Cape Alava is a cape in the Pacific Northwest region of the United States. Located in Clallam County, Washington. The cape is situated within Olympic National Park and the Makah Indian Reservation, and is accessible via a 3-mile boardwalk hike from a ranger station in the park. Cape Alava Trail was designated a National Recreation Trail in 1981. Name The cape was named after the Basque Don José Manuel de Álava (born in Vitoria, Álava, January 1, 1743) for his role as commissioner during the solution of the conflict of Nootka in 1794. Westernmost location Cape Alava is the westernmost point in the contiguous United States, with a longitude of (during low tide and walking out to the west side of Tskawahyah Island). Nearby Cape Flattery and Cape Blanco in southern Oregon are also very close longitudinally to being the westernmost points in the contiguous 48 states, which are at and respectively. History In early 1834, a mastless and rudderless Japanese rice trans ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cape Alava Ozette Island
A cape is a clothing accessory or a sleeveless outer garment which drapes the wearer's back, arms, and chest, and connects at the neck. History Capes were common in medieval Europe, especially when combined with a hood in the chaperon. They have had periodic returns to fashion - for example, in nineteenth-century Europe. Roman Catholic clergy wear a type of cape known as a ferraiolo, which is worn for formal events outside a ritualistic context. The cope is a liturgical vestment in the form of a cape. Capes are often highly decorated with elaborate embroidery. Capes remain in regular use as rainwear in various military units and police forces, in France for example. A gas cape was a voluminous military garment designed to give rain protection to someone wearing the bulky gas masks used in twentieth-century wars. Rich noblemen and elite warriors of the Aztec Empire would wear a tilmàtli; a Mesoamerican cloak/cape used as a symbol of their upper status. Cloth and clothing ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Oregon
Oregon () is a state in the Pacific Northwest region of the Western United States. The Columbia River delineates much of Oregon's northern boundary with Washington, while the Snake River delineates much of its eastern boundary with Idaho. The 42° north parallel delineates the southern boundary with California and Nevada. Oregon has been home to many indigenous nations for thousands of years. The first European traders, explorers, and settlers began exploring what is now Oregon's Pacific coast in the early-mid 16th century. As early as 1564, the Spanish began sending vessels northeast from the Philippines, riding the Kuroshio Current in a sweeping circular route across the northern part of the Pacific. In 1592, Juan de Fuca undertook detailed mapping and studies of ocean currents in the Pacific Northwest, including the Oregon coast as well as the strait now bearing his name. Spanish ships – 250 in as many years – would typically not land before reaching Cape Mendoci ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alluvium
Alluvium (from Latin ''alluvius'', from ''alluere'' 'to wash against') is loose clay, silt, sand, or gravel that has been deposited by running water in a stream bed, on a floodplain, in an alluvial fan or beach, or in similar settings. Alluvium is also sometimes called alluvial deposit. Alluvium is typically geologically young and is not consolidated into solid rock. Sediments deposited underwater, in seas, estuaries, lakes, or ponds, are not described as alluvium. Floodplain alluvium can be highly fertile, and supported some of the earliest human civilizations. Definitions The present consensus is that "alluvium" refers to loose sediments of all types deposited by running water in floodplains or in alluvial fans or related landforms. However, the meaning of the term has varied considerably since it was first defined in the French dictionary of Antoine Furetière, posthumously published in 1690. Drawing upon concepts from Roman law, Furetière defined ''alluvio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Moraine
A moraine is any accumulation of unconsolidated debris ( regolith and rock), sometimes referred to as glacial till, that occurs in both currently and formerly glaciated regions, and that has been previously carried along by a glacier or ice sheet. It may consist of partly rounded particles ranging in size from boulders (in which case it is often referred to as boulder clay) down to gravel and sand, in a groundmass of finely-divided clayey material sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines were formed at the foot, marking the maximum advance of the glacier. Other types of moraine include ground moraines ( till-covered areas forming sheets on flat or irregular topography) and medial moraines (moraines formed where two glaciers meet). Etymology The word ''moraine'' is borrowed from French , which in turn is derived from the Savoyard Italian ("mound of earth"). ''Morena'' in this case was derived from Pr ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sediment
Sediment is a naturally occurring material that is broken down by processes of weathering and erosion, and is subsequently transported by the action of wind, water, or ice or by the force of gravity acting on the particles. For example, sand and silt can be carried in suspension in river water and on reaching the sea bed deposited by sedimentation; if buried, they may eventually become sandstone and siltstone ( sedimentary rocks) through lithification. Sediments are most often transported by water ( fluvial processes), but also wind (aeolian processes) and glaciers. Beach sands and river channel deposits are examples of fluvial transport and deposition, though sediment also often settles out of slow-moving or standing water in lakes and oceans. Desert sand dunes and loess are examples of aeolian transport and deposition. Glacial moraine deposits and till are ice-transported sediments. Classification Sediment can be classified based on its grain size, grain s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Erosion
Erosion is the action of surface processes (such as water flow or wind) that removes soil, rock, or dissolved material from one location on the Earth's crust, and then transports it to another location where it is deposited. Erosion is distinct from weathering which involves no movement. Removal of rock or soil as clastic sediment is referred to as ''physical'' or ''mechanical'' erosion; this contrasts with ''chemical'' erosion, where soil or rock material is removed from an area by dissolution. Eroded sediment or solutes may be transported just a few millimetres, or for thousands of kilometres. Agents of erosion include rainfall; bedrock wear in rivers; coastal erosion by the sea and waves; glacial plucking, abrasion, and scour; areal flooding; wind abrasion; groundwater processes; and mass movement processes in steep landscapes like landslides and debris flows. The rates at which such processes act control how fast a surface is eroded. Typically, physical ero ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Geologic Formation
A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics ( lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock exposed in a geographical region (the stratigraphic column). It is the fundamental unit of lithostratigraphy, the study of strata or rock layers. A formation must be large enough that it can be mapped at the surface or traced in the subsurface. Formations are otherwise not defined by the thickness of their rock strata, which can vary widely. They are usually, but not universally, tabular in form. They may consist of a single lithology (rock type), or of alternating beds of two or more lithologies, or even a heterogeneous mixture of lithologies, so long as this distinguishes them from adjacent bodies of rock. The concept of a geologic formation goes back to the beginnings of modern scientific geology. The term was used by Abraham Gottlob We ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Omnibus Public Land Management Act Of 2009
The Omnibus Public Land Management Act of 2009 (, ) is a land management law passed in the 111th United States Congress and signed into law by President Barack Obama on March 30, 2009. The bill designates millions of acres in the US as protected and establishes a National Landscape Conservation System. It includes funding for programs, studies and other activities by the Department of the Interior and the Department of Agriculture, and in some cases bars further geothermal leasing, oil and gas leasing, and new mining patents on certain stretches of protected land. Legislative history 110th Congress On June 26, 2008, Senator Jeff Bingaman of New Mexico introduced the Omnibus Public Land Management Act of 2008 (). Although the bill had some support from both Democrats and Republicans, including Senate Majority Leader Harry Reid of Nevada, the Senate never voted on the measure due to threats by Senator Tom Coburn (R-Oklahoma) to filibuster the bill. 111th Congress S. 22 On January ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pacific Northwest Trail
The Pacific Northwest Trail (PNT) is a 1200-mile hiking trail running from the Continental Divide in Montana to the Pacific Ocean on Washington's Olympic Coast. Along the way, the PNT crosses three national parks, seven national forests, and two other national scenic trails. It travels against the grain of several mountain ranges, including the Continental Divide, Whitefish Divide, Purcells, Selkirks, Kettles, Cascades, and Olympics. It was designated as the Pacific Northwest National Scenic Trail by Congress in 2009. History The route was first conceived by Ron Strickland in 1970. Between 1970 and 1976, extensive fieldwork was performed by Strickland and others, including early supporters along the PNT corridor who lent extensive knowledge of local trail systems to the effort. In that time, the Pacific Northwest Trail was cobbled together using preexisting trails and Forest Service roads. In 1977, Strickland founded the Pacific Northwest Trail Association (PNTA), an organ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
HistoryLink
HistoryLink is an online encyclopedia of Washington state history. The site has more than 8,100 entries and attracts 5,000 daily visitors. It has 500 biographies and more than 14,000 images. The non-profit historical organization History Ink produces HistoryLink.org, stating that it is the nation's first online encyclopedia of local and state history created expressly for the Internet. Walt Crowley was the founding president and executive director. Foundation In 1997, Crowley discussed preparing a Seattle-King County historical encyclopedia for the 2001 sesquicentennial of the Denny Party. His wife Marie McCaffrey suggested publishing the encyclopedia on the Internet. They and Paul Dorpat incorporated History Ink on November 10, 1997, with seed money from Priscilla "Patsy" Collins, by birth a member of Seattle's wealthy and prominent Bullitt family. The prototype of HistoryLink.org debuted on May 1, 1998, and attracted additional funding for a formal launch in 1999. The webs ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fort Vancouver
Fort Vancouver was a 19th century fur trading post that was the headquarters of the Hudson's Bay Company's Columbia Department, located in the Pacific Northwest. Named for Captain George Vancouver, the fort was located on the northern bank of the Columbia River in present-day Vancouver, Washington. The fort was a major center of the regional fur trading. Every year trade goods and supplies from London arrived either via ships sailing to the Pacific Ocean or overland from Hudson Bay via the York Factory Express. Supplies and trade goods were exchanged with a plethora of Indigenous cultures for fur pelts. Furs from Fort Vancouver were often shipped to the Chinese port of Guangzhou where they were traded for Chinese manufactured goods for sale in the United Kingdom. At its pinnacle, Fort Vancouver watched over 34 outposts, 24 ports, six ships, and 600 employees. Today, a full-scale replica of the fort, with internal buildings, has been constructed and is open to the public as For ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Makah
The Makah (; Klallam: ''màq̓áʔa'')Renker, Ann M., and Gunther, Erna (1990). "Makah". In "Northwest Coast", ed. Wayne Suttles. Vol. 7 of '' Handbook of North American Indians'', ed. William C. Sturtevant. Washington, D.C.: Smithsonian Institution, pg. 429 are an indigenous people of the Pacific Northwest Coast living in Washington, in the northwestern part of the continental United States. They are enrolled in the federally recognized ''Makah Indian Tribe of the Makah Indian Reservation''. Linguistically and ethnographically, they are closely related to the Nuu-chah-nulth and Ditidaht peoples of the West Coast of Vancouver Island, who live across the Strait of Juan de Fuca in British Columbia, Canada. Reservation The Makah Indian Tribe own the Makah Indian Reservation on the northwest tip of the Olympic Peninsula; it includes Tatoosh Island. They live in and around the town of Neah Bay, Washington, a small fishing village. The Makah people refer to themselves as ''K ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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