Short Beach (Oregon)
Short Beach is a 1,000-meter stretch of beach on the northern Oregon Coast in the United States. Locals guess that both the beach and the creek that runs onto it—Short Creek, several miles in length—were named after an early resident of the area. Just south of Cape Meares State Park, and a bit north of Oceanside, the beach is hidden from the land except for a brief stretch of road which crosses the dam across Short Creek. The seasonal Short Beach Other attractions are the mussels, which can be gathered from offshore rocks at low tides, surf fishing, and beach fires. An occasional surfer may be seen, as well as paragliders who, now that there is safe access, sometimes land on the beach. Offshore, and partly onshore, are a number of rocks belonging to the Oregon Islands National Wildlife Refuge. In recent years, both these and the higher land around Short Beach have suffered significant erosion — collapse of rock faces and shoreward erosion along the bluff of over five f ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Beach
A beach is a landform alongside a body of water which consists of loose particles. The particles composing a beach are typically made from Rock (geology), rock, such as sand, gravel, shingle beach, shingle, pebbles, etc., or biological sources, such as mollusc shells or coralline algae. Sediments settle in different densities and structures, depending on the local wave action and weather, creating different textures, colors and gradients or layers of material. Though some beaches form on inland freshwater locations such as lakes and rivers, most beaches are in coastal areas where wind wave, wave or Ocean current, current action deposition (geology), deposits and reworks sediments. Coastal erosion, Erosion and changing of beach geologies happens through natural processes, like wave action and Extreme weather, extreme weather events. Where wind conditions are correct, beaches can be backed by coastal dunes which offer protection and regeneration for the beach. However, th ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Oregon Coast
The Oregon Coast is a coastal region of the U.S. state of Oregon. It is bordered by the Pacific Ocean to its west and the Oregon Coast Range to the east, and stretches approximately from the California state border in the south to the Columbia River in the north. The region is not a specific geological, environmental, or political entity, and includes the Columbia River Estuary. The Oregon Beach Bill of 1967 allows free beach access to everyone. In return for a pedestrian easement and relief from construction, the bill eliminates property taxes on private beach land and allows its owners to retain certain beach land rights. Traditionally, the Oregon Coast is regarded as three distinct sub–regions: * The North Coast, which stretches from the Columbia River to Cascade Head, Oregon, Cascade Head. * The Central Coast, which stretches from Cascade Head to Reedsport, Oregon, Reedsport. * The South Coast, which stretches from Reedsport to the U.S. Route 101 in Oregon#Brookings to C ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Cape Meares State Park
Cape Meares is a small headland on the Pacific coast in Tillamook County, Oregon, United States. The cape forms a high steep bluff on the south end of Tillamook Bay, approximately five miles (8 km) northwest of the city of Tillamook. Much of the cape is part of the Oregon Parks and Recreation Department-administered Cape Meares State Scenic Viewpoint with three miles of hiking trails, which includes Cape Meares Light and the Octopus Tree. The cape is named after John Meares, a British explorer. Geography Immediately north of the cape is the community of Cape Meares, next to Cape Meares Lake. Cape Meares beach extends north of the community of Cape Meares, along a sand spit, or peninsula, that encloses Tillamook Bay. The peninsula is alternatively known as Bayocean, after a popular upscale resort town that occupied the beach in the early 20th century, until beach erosion began to destroy the town beginning in the 1930s. Today, no significant remnant of the resort ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Oceanside, Oregon
Oceanside is a census-designated place (CDP) and unincorporated community in Tillamook County, Oregon, United States. The population was 361 at the 2010 census. Oregon Route 131's northern terminus is in the community, which is just north of Netarts. Symons State Park is in Oceanside, while Three Arch Rocks National Wildlife Refuge lies just offshore. Geography According to the United States Census Bureau, the CDP has a total area of , all of it land. The area is located above sea level. Demographics As of the census of 2000, there were 326 people, 193 households, and 99 families residing in the CDP. The population density was . There were 522 housing units at an average density of . The racial makeup of the CDP was 96.63% White, 0.61% African American, 1.84% Asian, and 0.92% from two or more races. Hispanic or Latino of any race were 1.23% of the population. There were 193 households, out of which 5.2% had children under the age of 18 living with them, 48.7% were marr ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Shingle Beach
A shingle beach, also known as either a cobble beach or gravel beach, is a commonly narrow beach that is composed of coarse, loose, well-rounded, and waterworn gravel, called ''shingle''. The gravel (shingle) typically consists of smooth, spheroidal to flattened, pebbles, cobbles, and sometimes small boulders, generally in the size range. Shingle beaches typically have a steep slope on both their landward and seaward sides. Shingle beaches form in wave-dominated locations where resistant bedrock cliffs provide gravel-sized rock debris. They are also found in high latitudes and temperate shores where the erosion of Quaternary glacial deposits provide gravel-size rock fragments. This term is most widely used in Great Britain.Neuendorf, Klaus K.E. Mehl, James P., Jr. Jackson, Julia A., 2011. ''Glossary of Geology'' (5th Edition). American Geosciences Institute. Narayana, A. C., 2016. ''Coastal landforms''. in Kennish, M.J., ed., pp. 143–157, ''Encyclopedia of Estuaries''. Spr ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mussel
Mussel () is the common name used for members of several families of bivalve molluscs, from saltwater and Freshwater bivalve, freshwater habitats. These groups have in common a shell whose outline is elongated and asymmetrical compared with other edible clams, which are often more or less rounded or oval. The word "mussel" is frequently used to mean the bivalves of the marine family Mytilidae, most of which live on exposed shores in the intertidal zone, attached by means of their strong Byssus, byssal threads ("beard") to a firm substrate. A few species (in the genus ''Bathymodiolus'') have colonised hydrothermal vents associated with deep ocean ridges. In most marine mussels the shell is longer than it is wide, being wedge-shaped or asymmetrical. The external colour of the shell is often dark blue, blackish, or brown, while the interior is silvery and somewhat nacreous. The common name "mussel" is also used for many freshwater bivalves, including the freshwater pearl mussels. F ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Sea Stack
A stack or sea stack is a geological landform consisting of a steep and often vertical column or columns of rock in the sea near a coast, formed by wave erosion. Stacks are formed over time by wind and water, processes of coastal geomorphology. britannica.com They are formed when part of a is by hydraulic action, which is the force of the sea or water crashing against the rock. The force of the water weakens cracks in the headland, causing them to later collapse, ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Oregon Islands National Wildlife Refuge
Oregon Islands National Wildlife Refuge is a U.S. National Wildlife Refuge off the southwestern Oregon Coast. It is one of six National Wildlife Refuges comprising the Oregon Coast National Wildlife Refuge Complex. The Oregon Islands provides wilderness protection to 1,853 small islands, rocks, and reefs plus two headlands, totaling spanning of Oregon's coastline from the Oregon–California border to Tillamook Head. There are sites in six of the seven coastal counties of Oregon. From north to south they are Clatsop, Tillamook, Lincoln, Lane, Coos, and Curry counties. ( Douglas County is the only coastal Oregon county not included in the refuge.) The area is managed by the United States Fish and Wildlife Service. History The Oregon Islands National Wildlife Refuge was created in 1935 by the federal government. Haystack Rock off Cannon Beach was added to the refuge in 1968, which became a wilderness area in 1978. The first mainland addition to the refuge came in 1991 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Erosion
Erosion is the action of surface processes (such as Surface runoff, water flow or wind) that removes soil, Rock (geology), rock, or dissolved material from one location on the Earth's crust#Crust, Earth's crust and then sediment transport, transports it to another location where it is deposit (geology), 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 Solvation, 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 Wind wave, waves; glacier, glacial Plucking (glaciation), plucking, Abrasion (geology), abrasion, and scour; areal flooding; Aeolian processes, wind abrasion; groundwater processes; and Mass wastin ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Columbia River
The Columbia River (Upper Chinook language, Upper Chinook: ' or '; Sahaptin language, Sahaptin: ''Nch’i-Wàna'' or ''Nchi wana''; Sinixt dialect'' '') is the largest river in the Pacific Northwest region of North America. The river headwater, forms in the Rocky Mountains of British Columbia, Canada. It flows northwest and then south into the U.S. state of Washington, then turns west to form most of the border between Washington and the state of Oregon before emptying into the Pacific Ocean. The river is long, and its largest tributary is the Snake River. Columbia River drainage basin, Its drainage basin is roughly the size of France and extends into seven states of the United States and one Canadian province. The fourth-largest river in the United States by River flow, flow, the Columbia has the greatest flow of any river into the eastern Pacific. The Columbia and its tributaries have been central to the region's culture and economy for thousands of years. They have been use ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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List Of National Wildlife Refuges
As of 2022, there are 588 National Wildlife Refuges in the United States, with the addition of the Green River National Wildlife Refuge. Refuges that have boundaries in multiple states are listed only in the state where the main visitor entrance is located. The newest refuge replaces the Cherry Valley National Wildlife Refuge in Pennsylvania. Refuges are listed regardless of whether or not they are open to the public, which many are not. The United States is divided into eight regions for administrative purposes: See also * List of largest National Wildlife Refuges * Klamath Basin National Wildlife Refuges Complex * Mid-Columbia River National Wildlife Refuge Complex * Oregon Coast National Wildlife Refuge Complex * Sheldon-Hart Mountain National Wildlife Refuge Complex * Willamette Valley National Wildlife Refuge Complex References External links US Fish and Wildlife Service list of National Wildlife Refuges {{USStatelists National Wildlife Refuges of the United ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Beaches Of Oregon
A beach is a landform alongside a body of water which consists of loose particles. The particles composing a beach are typically made from rock, such as sand, gravel, shingle, pebbles, etc., or biological sources, such as mollusc shells or coralline algae. Sediments settle in different densities and structures, depending on the local wave action and weather, creating different textures, colors and gradients or layers of material. Though some beaches form on inland freshwater locations such as lakes and rivers, most beaches are in coastal areas where wave or current action deposits and reworks sediments. Erosion and changing of beach geologies happens through natural processes, like wave action and extreme weather events. Where wind conditions are correct, beaches can be backed by coastal dunes which offer protection and regeneration for the beach. However, these natural forces have become more extreme due to climate change, permanently altering beaches at very rapid ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |