The Nooksack River is a river in the northwest part of the U.S. state of Washington. It drains an area of the Cascade Range around Mount Baker, near the Canada–US border. The lower river flows through a fertile agricultural area before emptying into Bellingham Bay and, via the Strait of Juan de Fuca and the Strait of Georgia, the Pacific Ocean. The river begins in three main forks, the North Fork, Middle Fork, and South Fork. The North Fork is sometimes considered the main river. Including the North Fork, the Nooksack is approximately 75 miles (121 km) long. All three forks originate in the Mount Baker Wilderness.
The Kern River, originally Rio de San Felipe, later La Porciuncula, is a river in the U.S. state of California, approximately 165 miles (270 km) long. It drains an area of the southern Sierra Nevada mountains northeast of Bakersfield. Fed by snowmelt near Mount Whitney, the river passes through scenic canyons in the mountains and is a popular destination for whitewater rafting and kayaking. It is the southernmost major river system in the Sierra Nevada, and is the only major river in the Sierra that drains in a southerly direction.
The Galisteo Basin is a surface basin and a closely related groundwater basin in north-central New Mexico. Its primary watercourse is the Galisteo River or Galisteo Creek, a perennial stream, for part of its course, that flows from the eastern highlands down into the Rio Grande about three miles above the Santo Domingo Pueblo. The Galisteo basin covers approximately 467,200 acres and runs from San Miguel County in the east, across Santa Fe County, and into Sandoval County at its westernmost point, the Rio Grande. Northeast of Galisteo Basin rise the Sangre de Cristo Mountains and to the southwest lie the Sandia Mountains. Because of its location lying between mountain ranges and connecting the Rio Grande Valley with the Great Plains, the Galisteo Basin was used as a trade route by prehistoric and historic indigenous and later also by the Spanish explorers.
The Whitewater River is a small permanent stream in western Riverside County, California, with a small upstream section in southwestern San Bernardino County. Its headwaters are in the San Bernardino Mountains and mouth–terminus in the Colorado Desert. The Whitewater River is in the endorheic Salton Sea drainage basin.
The San Jacinto River is a 42-mile-long (68 km) river in Riverside County, California. The river's headwaters are in San Bernardino National Forest, but the lower portion of the 765-square-mile (1,980 km2) watershed is urban and agricultural land. As a partially endorheic watershed that is contiguous with other Great Basin watersheds, the western side of the San Jacinto Basin is a portion of the Great Basin Divide.
The Quinault River is a 69-mile (111 km) long river located on the Olympic Peninsula in the U.S. state of Washington. It originates deep in the Olympic Mountains in the Olympic National Park. It flows southwest through the "Enchanted Valley" to opposite Quinault Canyon. Several miles above Lake Quinault the river is joined by its main tributary, the North Fork Quinault River. The main stem Quinault River above this confluence is sometimes called the East Fork Quinault River. Below the confluence the river marks the boundary of Olympic National Park for several miles before emptying into Lake Quinault. After the lake, the Quinault River flows southwest, reaching the Pacific at Taholah. From Lake Quinault to the ocean, the river is contained within the Quinault Indian Reservation.
Cherry Creek is a large, swift-flowing stream in the Sierra Nevada mountain range, and is the largest tributary of the Tuolumne River. The creek is 40 miles (64 km) long measured to its farthest headwaters; the main stem itself is 26 miles (42 km) long, draining a watershed of 234 square miles (610 km2) in the Stanislaus National Forest. Part of the drainage also extends into the northwest corner of Yosemite National Park.
The Rio Chama, a major tributary river of the Rio Grande, is located in the U.S. states of Colorado and New Mexico. The river is about 130 miles (210 km) long altogether. From its source to El Vado Dam its length is about 50 miles (80 km), from El Vado Dam to Abiquiu Dam is about 51 miles (82 km), and from Abiquiu Dam to its confluence with the Rio Grande is about 34 miles (55 km).
The Rio Puerco is a tributary of the Rio Grande in the U.S. state of New Mexico. From its source on the west side of the Nacimiento Mountains, it flows about 230 miles (370 km), generally south to join the Rio Grande about 20 miles (32 km) south of Belen and about 50 miles (80 km) south of Albuquerque. Its drainage basin is about 7,350 square miles (19,000 km2) large, of which probably about 1,130 square miles (2,900 km2) are noncontributing.
The Piedra River is a river in the U.S. state of Colorado. It drains parts of Archuleta, Hinsdale, and Mineral counties along a mainstem length of about 40 miles (64 km). The river flows through a series of isolated box canyons, emptying into the San Juan River at Navajo Lake. Its name stems from the Spanish word, piedra, meaning rock.
The Palix River is a stream in the U.S. state of Washington. Its tributaries include three forks, North, Middle, and South Fork Palix River, as well as the Canon River. The river's length, including the Canon River, its longest tributary, is approximately 14 miles (23 km).
The Satsop River is a stream in the U.S. state of Washington. It has three main tributary forks, the East Fork, West Fork, and Middle Fork Satsop Rivers. The main stem Satsop River is formed by the confluence of the West and East Forks. The Middle Fork is a tributary of the East Fork. The three forks are much longer than the main stem Satsop itself, which flows south from the confluence only a few miles to join the Chehalis River near Satsop, Washington. Other significant tributaries include the Canyon River and Little River, both tributaries of the West Fork Satsop, and Decker Creek, a tributary of the East Fork Satsop River. The Satsop River's major tributaries originate in the Olympic Mountains and its southern foothills, the Satsop Hills, within Grays Harbor and Mason counties. Most of the Satsop River's watershed consists of heavily wooded hill lands. The upper tributaries extend into Olympic National Forest, approaching but not quite reaching Olympic National Park.
The Rio Pueblo de Taos, also known as Rio Pueblo, is a tributary of the Rio Grande in the U.S. state of New Mexico. From its source in the Sangre de Cristo Mountains it flows about 33 miles (53 km), generally south and west, to join the Rio Grande in the Rio Grande Gorge. On the way the river passes by Taos and through Taos Pueblo.
The Rio Salado is a tributary of the Rio Grande in the U.S. state of New Mexico. From its source in northeast Catron County it flows about 86 miles (138 km) generally east to join the Rio Grande just north of Polvadera and about 15 miles (24 km) north of Socorro. The name Río Salado is Spanish for "salty river".
Jaramillo Creek is a 10 mile long stream in New Mexico with headwaters in the Jemez Mountains. Jaramillo is a tributary of the East Fork Jemez which is then a tributary of the Jemez River, a tributary of the Rio Grande. The creek is located in a graben in the Pleistocene age Valles Caldera. The Jaramillo normal event of the Matumaya Reversed Epoch was named for rocks selected and aged at the type locality near the creek.
La Vereda del Monte was a backcountry route through remote regions of the Diablo Range, one of the California Coast Ranges. La Vereda del Monte was the upper part of La Vereda Caballo,, used by mesteñeros from the early 1840s to drive Alta California horses to Sonora for sale.
The Rio San Jose is a 90-mile-long (145 km) tributary of the Rio Puerco in the U.S. state of New Mexico.
Rio San Antonio is a tributary of the Conejos River in northern New Mexico and southern Colorado. Via the Conejos River, it is part of the upper Rio Grande system. The river is used extensively for irrigation in its lower course through the southern San Luis Valley.
