The Otselic River (aht-SEEL-ik), formerly known as Otselic Creek, is a 55.4-mile-long (89.2 km) tributary of the Tioughnioga River in central New York in the United States. It drains a hilly area, mostly forested and agricultural, east of the Finger Lakes at the northern edge of the Susquehanna River watershed.
The Feather River is the principal tributary of the Sacramento River, in the Sacramento Valley of Northern California. The river's main stem is about 73 miles (117 km) long. Its length to its most distant headwater tributary is just over 210 miles (340 km). The main stem Feather River begins in Lake Oroville, where its four long tributary forks join—the South Fork, Middle Fork, North Fork, and West Branch Feather Rivers. These and other tributaries drain part of the northern Sierra Nevada, and the extreme southern Cascades, as well as a small portion of the Sacramento Valley. The total drainage basin is about 6,200 square miles (16,000 km2), with approximately 3,604 square miles (9,330 km2) above Lake Oroville.
Little Wood River is a 130-mile-long (210 km) river in south-central Idaho in the United States. It is a tributary of the Malad River, which in turn is a tributary to the Snake River and Columbia River.
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 44.6 miles (71.8 km) long measured to its farthest headwaters; the main stem itself is 27.7 miles (44.6 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.
Uvas Creek is a 29.5-mile-long (47.5 km) mainly southward-flowing stream originating on Loma Prieta peak of the Santa Cruz Mountains, in Santa Clara County, California, United States. The creek descends through Uvas Canyon County Park into Uvas Reservoir near Morgan Hill, and on through Uvas Creek Preserve and Christmas Hill Park in Gilroy. Upon passing U.S. Highway 101 it is known as Carnadero Creek, shortly before the confluence with the Pajaro River at the Santa Clara County - San Benito County boundary.
Big Butte Creek is a 12-mile-long (19 km) tributary of the Rogue River in the U.S. state of Oregon. It drains approximately 245 square miles (635 km2) of Jackson County. Its two forks, the North Fork and the South Fork, both begin high in the Cascade Range near Mount McLoughlin. Flowing predominantly west, they meet near the city of Butte Falls. The main stem flows generally northwest until it empties into the Rogue Falls was incorporated in 1911, and remains the only incorporated town within the watershed's boundaries.
Calero Reservoir, also called Calero Lake, is a reservoir in San Jose, California, located in the Calero neighborhood of Almaden Valley in South San Jose. It is the site of Calero County Park, which also includes a large area covering the lake and hundreds of acres of hills around it.
Willow Creek is a 57-mile (92 km) tributary of the Malheur River in Malheur County in the U.S. state of Oregon. The creek, which forms at 3,724 feet (1,135 m) above sea level and ends at 2,234 feet (681 m), flows generally southeast between Ironside and Vale. Willow Creek's watershed covers 787 square miles (2,040 km2) of relatively arid land.
Florida River is a 61.7-mile-long (99.3 km) tributary of the Animas River in La Plata County, Colorado.
Horse Creek is a 129-mile-long (208 km) tributary of the Arkansas River that flows from a source south of Calhan in the Holcolm Hills of El Paso County, Colorado. It flows east and south to a confluence with the Arkansas in Bent County west of Las Animas
Lovewell Reservoir is a reservoir in Jewell County, Kansas, United States. Built and managed by the U.S. Bureau of Reclamation, it is used for flood control, irrigation, and recreation. Lovewell State Park is located on its north shore.
Pacheco Creek is a 28 miles (45 km) west by southwest flowing stream which heads in the Diablo Range in southeastern Santa Clara County and flows to San Felipe Lake, the beginning of the Pajaro River mainstem, in San Benito County, California.
Guadalupe Creek is a 10.5 miles (16.9 km) northward-flowing stream originating just east of the peak of Mount Umunhum in Santa Clara County, California, United States. It courses along the northwestern border of Almaden Quicksilver County Park in the Cañada de los Capitancillos before joining Los Alamitos Creek after the latter exits Lake Almaden. This confluence forms the Guadalupe River mainstem, which in turn flows through San Jose and empties into south San Francisco Bay at Alviso Slough.
San Felipe Creek is a 14 miles (23 km) stream that originates in the western Diablo Range in Santa Clara County, California. It flows south by southeast through two historic ranchos, Rancho Los Huecos and Rancho Cañada de San Felipe y Las Animas before it joins Las Animas Creek just above Anderson Reservoir. One of the nine major tributaries of Coyote Creek, the creek's waters pass through the Santa Clara Valley and San Jose on the way to San Francisco Bay.
Quartz Creek is a stream in Gunnison County, Colorado, United States, that is a tributary of Tomichi Creek.
Little Rock Creek is a 16.7-mile (26.9 km) northwestward-flowing stream in the San Gabriel Mountains and Mojave Desert, within northern Los Angeles County, California.
Cottonwood Creek is a major stream, about 36 miles (58 km) long, in southern San Diego County, California. It is part of the Tijuana River drainage basin.
Tapeats Creek is a creek located entirely within the Grand Canyon National Park. It flows southwest from its source near the North Rim of the canyon to the Colorado River at the base of the canyon. It was named by the Second Powell Expedition in the winter of 1871–1872 for a Southern Paiute Indian who claimed ownership of the stream. It contributes the largest amount of water to the Colorado of any tributary on the north side within the Grand Canyon.
The Great Plains Reservoirs are a group of reservoirs along both sides of U.S. Highway 287 in Kiowa and Prowers counties in southeastern Colorado. Fed by canals, the reservoirs lie in naturally occurring depressions and store water for irrigation and recreational uses. The depressions vary in size from .6–5.0 square miles, and the water depths range from 13–25 feet, but the water levels vary because the reservoirs are filled in spring and drawn down during the growing season.
