The Cullasaja River is a short river that flows from Lake Sequoyah which is fed by Mirror Lake and other creeks and streams originating on the western side of the demarcation of two watersheds of what?
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Cullasaja River The Cullasaja River is a short river located entirely in Macon County, North Carolina. It is a tributary of the Little Tennessee River (and in turn the Tennessee River, Ohio River and Mississippi River), into which it flows near the county seat of Franklin. It originates to the southeast, near Highlands, the county's only other town. It flows from Lake Sequoyah, which is fed by Mirror Lake and other creeks and streams originating on the western side of the Eastern Continental Divide, which runs through the east side of Highlands.
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Eastern Continental Divide The Eastern Continental Divide (ECD) or Appalachian Divide or Eastern Divide, in conjunction with other continental divides of North America, demarcates two watersheds of the Atlantic Ocean: the Gulf of Mexico watershed and the Atlantic Seaboard watershed. As can be readily seen from the first map at the right, the Gulf watershed demarcated by the Great Divide in red begins along the spine of the mountains of Central America and runs through the American Rockies where is terminates in the triple divide at Triple Divide Peak in Glacier National Park along the U.S.-Canadian border where the Laurentian Divide blocks the waters from traveling south to the Gulf of Mexico.
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Blanco Canyon Blanco Canyon is a canyon located in the U.S. state of Texas. Eroded by the White River into the Caprock Escarpment on the east side of the Llano Estacado, the canyon runs for 34 mi in a southeasterly direction, gradually widening from its beginning in southwestern Floyd County to 10 mi across at its mouth in southeastern Crosby County. It also gradually deepens from 50 ft at its beginning to 300 to 500 feet (91 to 150 m) at its mouth. There is one side canyon, five-mile long Crawfish Canyon, which was cut by Crawfish Creek as it feeds into the White River from the west.
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Duck Creek (Ohio) Duck Creek is a tributary of the Ohio River, approximately 30 mi (50 km) long, in southeastern Ohio in the United States. Via the Ohio River, it is part of the Mississippi River watershed. It drains an area of the Unglaciated Allegheny Plateau, between the watersheds of the Muskingum and Little Muskingum Rivers.
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Nevada Basin The Nevada Basin is the Great Basin area surrounded by river basins and, to the east, the Great Salt Lake basin (Pleistocene Lake Bonneville basin). The bounding river basins include those of the following (clockwise from south-southeast): Sevier River, Muddy River (Meadow Valley Wash, White River), Las Vegas Wash, Colorado River, Mojave River, Amargosa River, Owens River, Lake Lahontan basin (Walker River, Carson River, Humboldt River, Reese River), and Snake River. The 1850 diagonal California state lines with the Utah Territory & New Mexico Territory are along the general direction of the Nevada Basin's southwest drainage divide (rim), while the north-to-south rim on the east is through the area of the three meridians (1861, 1862, & current 1864) used for the Nevada-Utah state line.
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Selkirk Mountains The Selkirk Mountains are a mountain range spanning the northern portion of the Idaho Panhandle, eastern Washington, and southeastern British Columbia. They begin at Mica Peak near Spokane and extend approximately 320 km north (200 miles) from the border to Kinbasket Lake, at the now-inundated location of the onetime fur company post Boat Encampment. The range is bounded on its west, northeast and at its northern extremity by the Columbia River, or the reservoir lakes now filling most of that river's course. From the Columbia's confluence with the Beaver River, they are bounded on their east by the "Purcell Trench", which contains the Beaver River, Duncan River, Duncan Lake, Kootenay Lake and the Kootenay River. The Selkirks are distinct from, and geologically older than, the Rocky Mountains. Together with the neighboring Monashee and Purcell Mountains, and sometimes including the Cariboo Mountains to the northwest, the Selkirks are part of a larger grouping known as the Columbia Mountains. A scenic highway loop, the International Selkirk Loop, encircles the southern portions of the mountain range.
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Black Creek (Florida) Black Creek is a 13.0 mi tributary of the St. Johns River. It is located in Clay County, Florida. Black Creek has two major tributaries; North Fork Black Creek and South Fork Black Creek. North Fork originates as an outflow from Kingsley Lake and flows north and then east through Camp Blanding and Jennings State Forest, meeting South Fork in Middleburg, Florida. North Fork Black Creek has Yellow Water Creek and Big Branch as its main tributaries. South Fork Black Creek is fed by areas of wetlands and numerous small streams. The confluence of North Fork Black Creek and South Fork Black Creek near Middleburg form the main channel of Black Creek.
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Seboeis Lake Seboeis Lake extends from Lake View Plantation, Maine, north into Maine township 4, range 9. The lake is enclosed by rocky headlands and sandy beaches and contains several pine-covered islands. The inlet at the north end receives several tributaries from Long A township including Dean Brook, Jordan Brook, and West Seboeis Stream. Bear Brook flows into the northwest corner of the lake, and Northwest Pond overflows into the west side of the Lake. West Branch Sebois Stream overflows the east side of the lake through Dudley Rips into Endless Lake; and Endless Lake overflow reaches the Piscataquis River 15 mi downstream, just 3 mi upstream of the Piscataquis and Penobscot River confluence at Howland.
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Boardman Creek Boardman Creek is a stream in the Sawtooth National Forest in Camas County, Idaho in the United States. It is a tributary of the South Fork Boise River, which in turn is tributary to the Snake River and Columbia River.
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Deadman Creek (Owens River) Deadman Creek is the mainstream creek that becomes the Owens River where Big Springs enters the Deadman Creek channel, ""two miles east of the "[CalTrans]" US395 Crestview maintenance station"", near Deadman Summit. The Sierra Crest demarcates the creek's drainage from the drainage of the Middle Fork San Joaquin River on the west.
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Feather Headwaters The Feather Headwaters are 3 watersheds totaling 3450 sqmi and which drain to Lake Oroville. The North Fork Feather Watershed is 1090 sqmi —including the West Branch drainage of about 282.5 sqmi . The East Branch North Fork Feather Watershed is 1010 sqmi , and the Middle Fork Feather Watershed is 1350 sqmi —including the South Fork drainage of about 132 sqmi . Headwaters drainage is impaired by the Palermo Canal at Oroville Dam, the Hendricks Canal at the West Branch Feather River, and the Miners Ranch Canal at the South Fork's Ponderosa Reservoir. Additionally, the Pacific Gas and Electric Company releases Upper Feather water into the Hyatt Generating-Pumping Plant for hydroelectric generation during daily peak demand.
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Lake Sammamish Lake Sammamish is a freshwater lake 8 mi east of Seattle in King County, Washington, United States. The lake is 7 mi long and 1.5 mi wide, with a maximum depth of 105 ft and a surface area of 8 sqmi . It lies east of Lake Washington and west of the Sammamish Plateau, and stretches from Issaquah in the south to Redmond in the north. At Issaquah it is fed by Issaquah Creek, and at Redmond it drains to Lake Washington via the Sammamish River.
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Twomile Creek (Kanawha River) Twomile Creek is a tributary of the Kanawha River, 4.7 mi long, in West Virginia in the United States. Via the Kanawha and Ohio rivers, it is part of the watershed of the Mississippi River, draining an area of 24.4 sqmi on the unglaciated portion of the Allegheny Plateau, in the city of Charleston and its vicinity.
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Temescal Creek (Riverside County) Temescal Creek (shown on federal maps as Temescal Wash) is an approximately 29 mi watercourse in Riverside County, in the U.S. state of California. Flowing primarily in a northwestern direction, it connects Lake Elsinore with the Santa Ana River. It drains the eastern slopes of the Santa Ana Mountains on its left and on its right the western slopes of the Temescal Mountains along its length. With a drainage basin of about 1000 mi2 , it is the largest tributary of the Santa Ana River, hydrologically connecting the 720 mi2 San Jacinto River and Lake Elsinore watersheds to the rest of the Santa Ana watershed. However, flowing through an arid rain shadow zone of the Santa Ana Mountains, and with diversion of ground water for human use, the creek today is ephemeral for most of its length, except for runoff from housing developments and agricultural return flows.
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Cedar River (Washington) The Cedar River is a river in the U.S. state of Washington. About 45 mi long, it originates in the Cascade Range and flows generally west and northwest, emptying into the southern end of Lake Washington. Its upper watershed is a protected area called the Cedar River Watershed, which provides drinking water for the greater Seattle area.
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Icicle Creek Icicle Creek is a stream in the U.S. state of Washington. It originates at Josephine Lake near the crest of the Cascade Range and flows generally east to join the Wenatchee River near Leavenworth. Icicle Creek's drainage basin is mountainous and mostly undeveloped land within the Wenatchee National Forest and the Alpine Lakes Wilderness. The final six miles of the creek are moderately developed with scattered homes and pasture, a golf course, children's camp, a small housing development called Icicle Island Club, and the Leavenworth National Fish Hatchery. Some water is diverted from the creek for municipal use by the City of Leavenworth at Icicle Creek river mile 5.6. Near Leavenworth, the wheelchair-accessible Icicle Creek Nature Trail, a National Recreation Trail designated in 2005, runs 1.0 mi along a historic creek channel.
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Frog Lakes The Frog Lakes are a group of lakes, drained eastward by an unnamed stream feeding the Frog River, a tributary of the Kechika River in the Stikine Ranges of the Northern Interior of British Columbia. Though "not" the hydrological source of the Frog River, the lakes are notably located in an east-west aligned valley which forms the divide between the basins of the Stikine River and that of the Liard, and are therefore located on the Continental Divide between the Pacific and Arctic drainages. Draining from their west is the Pitman River, a Stikine tributary, from an unnamed lake just to their west( which also drains east to feed the Frog Lakes themselves), while the Kechika is a major tributary of the Liard, which is a tributary of the Mackenzie. The Frog Lakes Pass, as dubbed by the "Canadian Mountain Encyclopedia" and at an elevation of 1015 m (3330 ft), is the prominence col for 2668 m (8753 ft) Sharktooth Mountain, giving it a prominence of 1653m.
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Sancho Creek Sancho Creek is a tributary of Middle Island Creek, 9.6 mi long, in northwestern West Virginia in the United States. Via Middle Island Creek and the Ohio River, it is part of the watershed of the Mississippi River, draining an area of 22.2 sqmi in a rural region on the unglaciated portion of the Allegheny Plateau.
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Deer Creek (Tulare County, California) Deer Creek, formerly More's Creek, is a creek in Tulare County, California. Its source is in the on the west slope of the Greenhorn Mountains, in the Sierra Nevada Mountain range. From there Deer Creek runs west to terminate at the Lakeland and Homeland Canals in the San Joaquin Valley just east of the Tulare - Kings County border. Originally it ran into Tulare Lake before it was diverted for agriculture.
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Lochsa River The Lochsa River is in the northwestern United States, in the mountains of north central Idaho. It is one of two primary tributaries (with the Selway to the south) of the Middle Fork of the Clearwater River in the Clearwater National Forest. "Lochsa" is a Nez Perce word meaning "rough water". The Salish name is Ep Smɫí, "It Has Salmon."
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North Fork Clackamas River The North Fork Clackamas River is a tributary, about 11 mi long, of the Clackamas River in the U.S. state of Oregon. Originating at nearly 4000 ft above sea level on the west side of the Cascade Range, it flows westward through Mount Hood National Forest. It joins the Clackamas at North Fork Reservoir, about 32 mi from the larger river's confluence with the Willamette River. From source to mouth, the following tributaries enter the river: Dry Creek from the right bank, Boyer Creek from the left bank, then Whiskey, Bedford, Bee, and Fall creeks, all from the right.
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Lake Erie Basin Lake Erie Basin consists of Lake Erie and surrounding watersheds, which are typically named after the river, creek, or stream that provides drainage into the lake. The watersheds are located in the states of Indiana, Michigan, New York, Ohio, and Pennsylvania in the United States, and in the Province of Ontario in Canada. The basin is part of the Great Lakes Basin and Saint Lawrence River Watershed, which feeds into the Atlantic Ocean. 80% of the lake's water flows in from the Detroit River, with only 9% coming from all of the remaining watersheds combined. (The remainder (11%) is derived from direct precipitation into the lake.) A littoral zone serves as the interface between land and lake, being that portion of the basin where the lake is less than 15 ft in depth.