Millicoma River
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Millicoma River
__NOTOC__ The Millicoma River is a coast stream, about long, east of Coos Bay in the U.S. state of Oregon. Formed by the confluence of the East Fork Millicoma River and the West Fork Millicoma River at Allegany, it meanders across relatively flat land to meet the South Fork Coos River, with which it forms the Coos River. Oregon Route 241 (Coos River Highway) runs along the right bank of the river from Allegany to the mouth. The Millicoma meanders generally southwest, receiving Woodruff Creek from the left slightly downstream from Allegany. Deton Creek enters from the right at Rooke Higgins County Park near river mile (RM) 3.5 or river kilometer (RK) 5.6. About a half-mile later, Hendrickson Creek enters from the left. The Millicoma receives Matt Davis Creek from the right just before meeting the South Fork Coos River to form the Coos River about from the larger stream's mouth on Coos Bay. The Millicoma supports a large run of shad as well as runs of Chinook salmon ...
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Coos People
Coos people are an indigenous people of the Northwest Plateau, living in Oregon. They live on the southwest Oregon Pacific coast. Today, Coos people are enrolled in the following federally recognized tribes: * Confederated Tribes of the Coos, Lower Umpqua and Siuslaw Indians of Oregon * Confederated Tribes of Siletz Indians of Oregon * Coquille Indian Tribe. Language The Coos language is dormant. It belongs to the Coosan language family, and is divided into two dialects: Hanis language and Miluk language. The Confederated Tribes of Coos, Lower Umpqua and Siuslaw has a language program to revitalize the language. History Their neighbors were Siuslauan, Kalapuyan, and the Umpqua Indians. The total population of Hanis and Miluk Coos in 1780 has been estimated to be around 2,000. On February 8, 1806 the Coos people were first mentioned by Euro-Americans. William Clark, wintering at Fort Clatsop near the Columbia with Meriwether Lewis and the Corp of Discovery, reported t ...
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South Fork Coos River
The South Fork Coos River is a tributary, about long, of the Coos River in the U.S. state of Oregon. Formed by the confluence of the Williams River and Tioga Creek, it begins in eastern Coos County near the Douglas County line and flows generally northwest through the Southern Oregon Coast Range. East of the city of Coos Bay, it joins the Millicoma River to form the Coos River. This larger river, only about long, empties into the eastern end of Coos Bay, which connects to the Pacific Ocean. Course From its source, the river flows north through forests, receiving Mink Creek from the left. About further downstream, the river turns west, and Fall Creek enters from the right. Over the next stretch, Coal and Fannin creeks enter from the left and Elk Creek from the right. The river then turns south before Rock Crusher and Burma creeks enter from the left at about river mile (RM) 20 or river kilometer (RK) 32. Turning west, the river receives Cox Creek from the left. Afte ...
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List Of Rivers Of Oregon
This is a partial listing of rivers in the state of Oregon, United States. This list of Oregon rivers is organized alphabetically and by tributary structure. The list may also include streams known as creeks, brooks, forks, branches and prongs, as well as sloughs and channels. A list of rivers of the Americas and a list of Pacific Ocean coast rivers of the Americas are also available, as is a list of Oregon lakes. __TOC__ Alphabetical listing * Abiqua Creek * Agency Creek (South Yamhill River) * Alsea River *Amazon Creek * Ana River *Applegate River * Ash Creek * Ashland Creek *Balch Creek * Bear Creek *Big Butte Creek * Big Marsh Creek * Big River * Birch Creek * Blue River * Breitenbush River *Bridge Creek (John Day River) * Buck Hollow River * Bull Run River * Bully Creek * Burnt River * Butte Creek *Calapooia River *Catherine Creek * Chetco River *Chewaucan River *Clackamas River *Clatskanie River * Clear Fork * Clearwater River * Coast Fork Willamette River * Collawash R ...
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Coho Salmon
The coho salmon (''Oncorhynchus kisutch;'' Karuk: achvuun) is a species of anadromous fish in the salmon family (biology), family and one of the five Pacific salmon species. Coho salmon are also known as silver salmon or "silvers". The scientific species name is based on the Russian language, Russian common name ''kizhuch'' (кижуч). Description During their ocean phase, coho salmon have silver sides and dark-blue backs. During their spawning phase, their jaws and teeth become hooked. After entering fresh water, they develop bright-red sides, bluish-green heads and backs, dark bellies and dark spots on their backs. Sexually maturing fish develop a light-pink or rose shading along the belly, and the males may show a slight arching of the back. Mature adults have a pronounced red skin color with darker backs and average and , occasionally reaching up to . They also develop a large kype (hooked beak) during spawning. Mature females may be darker than males, with both showing ...
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Rainbow Trout
The rainbow trout (''Oncorhynchus mykiss'') is a species of trout native to cold-water tributaries of the Pacific Ocean in Asia and North America. The steelhead (sometimes called "steelhead trout") is an anadromous (sea-run) form of the coastal rainbow trout or Columbia River redband trout that usually returns to freshwater to spawn after living two to three years in the ocean. Freshwater forms that have been introduced into the Great Lakes and migrate into tributaries to spawn are also called steelhead. Adult freshwater stream rainbow trout average between , while lake-dwelling and anadromous forms may reach . Coloration varies widely based on subspecies, forms, and habitat. Adult fish are distinguished by a broad reddish stripe along the lateral line, from gills to the tail, which is most vivid in breeding males. Wild-caught and hatchery-reared forms of the species have been transplanted and introduced for food or sport in at least 45 countries and every continent ex ...
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Chinook Salmon
The Chinook salmon (''Oncorhynchus tshawytscha'') is the largest and most valuable species of Pacific salmon in North America, as well as the largest in the genus '' Oncorhynchus''. Its common name is derived from the Chinookan peoples. Other vernacular names for the species include king salmon, Quinnat salmon, Tsumen, spring salmon, chrome hog, Blackmouth, and Tyee salmon. The scientific species name is based on the Russian common name ''chavycha'' (чавыча). Chinook are anadromous fish native to the North Pacific Ocean and the river systems of western North America, ranging from California to Alaska, as well as Asian rivers ranging from northern Japan to the Palyavaam River in the Arctic northeast Siberia. They have been introduced to other parts of the world, including New Zealand, thriving in Lake Michigan Great Lakes of North America and Michigan's western rivers, and Patagonia. A large Chinook is a prized and sought-after catch for a sporting angler. The flesh of ...
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Shad
The Alosinae, or the shads,Alosinae
ITIS
are a of fishes in the herring family . The subfamily comprises seven genera worldwide, and about 30 species.Distribution of shad species
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Coos Bay
Coos Bay is an estuary where the Coos River enters the Pacific Ocean, the estuary is approximately 12 miles long and up to two miles wide. It is the largest estuary completely within Oregon state lines. The Coos Bay watershed covers an area of about 600 square miles and is located in northern Coos County, Oregon in the United States. The Coos River, which begins in the Oregon Coast Range, enters the bay from the east. From Coos River, the bay forms a sharp loop northward before arching back to the south and out to the Pacific Ocean. Haynes Inlet enters the top of this loop. South Slough branches off from the bay directly before its entrance into the Pacific Ocean. The bay was formed when sea levels rose over 20,000 years ago at the end of the Last Glacial Maximum, flooding the mouth of the Coos River. Coos Bay is Oregon's most important coastal industrial center and international shipping port, with close ties to San Francisco, the Columbia River, Puget Sound and other major por ...
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Left Bank
In geography, a bank is the land alongside a body of water. Different structures are referred to as ''banks'' in different fields of geography, as follows. In limnology (the study of inland waters), a stream bank or river bank is the terrain alongside the bed of a river, creek, or stream. The bank consists of the sides of the channel, between which the flow is confined. Stream banks are of particular interest in fluvial geography, which studies the processes associated with rivers and streams and the deposits and landforms created by them. Bankfull discharge is a discharge great enough to fill the channel and overtop the banks. The descriptive terms ''left bank'' and ''right bank'' refer to the perspective of an observer looking downstream; a well-known example of this being the sections of Paris as defined by the river Seine. The shoreline of ponds, swamps, estuaries, reservoirs, or lakes are also of interest in limnology and are sometimes referred to as banks. The ...
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River Delta
A river delta is a landform shaped like a triangle, created by deposition of sediment that is carried by a river and enters slower-moving or stagnant water. This occurs where a river enters an ocean, sea, estuary, lake, reservoir, or (more rarely) another river that cannot carry away the supplied sediment. It is so named because its triangle shape resembles the Greek letter Delta. The size and shape of a delta is controlled by the balance between watershed processes that supply sediment, and receiving basin processes that redistribute, sequester, and export that sediment. The size, geometry, and location of the receiving basin also plays an important role in delta evolution. River deltas are important in human civilization, as they are major agricultural production centers and population centers. They can provide coastline defense and can impact drinking water supply. They are also ecologically important, with different species' assemblages depending on their landscape posit ...
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Right Bank
In geography, a bank is the land alongside a body of water. Different structures are referred to as ''banks'' in different fields of geography, as follows. In limnology (the study of inland waters), a stream bank or river bank is the terrain alongside the bed of a river, creek, or stream. The bank consists of the sides of the channel, between which the flow is confined. Stream banks are of particular interest in fluvial geography, which studies the processes associated with rivers and streams and the deposits and landforms created by them. Bankfull discharge is a discharge great enough to fill the channel and overtop the banks. The descriptive terms ''left bank'' and ''right bank'' refer to the perspective of an observer looking downstream; a well-known example of this being the sections of Paris as defined by the river Seine. The shoreline of ponds, swamps, estuaries, reservoirs, or lakes are also of interest in limnology and are sometimes referred to as banks. The gra ...
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West Fork Millicoma River
The West Fork Millicoma River is a tributary, about long, of the Millicoma River in the U.S. state of Oregon. Rising in northeastern Coos County near the Douglas County line, it flows generally southwest through the Elliott State Forest of the Southern Oregon Coast Range to the community of Allegany. There it joins the East Fork Millicoma River to form the Millicoma. In turn, the Millicoma, which is only about long, joins the South Fork Coos River to form the Coos River. The Coos River, itself only about long, empties into the eastern end of Coos Bay, which connects to the Pacific Ocean. Course Beginning northeast of Elk Peak, the river flows generally north parallel to Umpcoos Ridge before turning west and receiving Cougar Creek from the right and then Kelly Creek from the right about from the mouth. Over the next , Panther Creek enters from the left, Fish Creek from the right, Elk Creek from the left, and Knife, Deer, and Otter creeks from the right. The river turns sout ...
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