White Deer Hole Creek
West Branch Susquehanna River
['Allegheny River', 'Lake Onega', 'Columbia River', 'Adour', 'Beaver River', 'Nechako River', 'Ganga', 'Fraser River', 'Ganga River', 'Terek River', 'Minnesota River', 'Oka', 'Skeena River', 'Rondout Creek', 'Santiam River', 'Yamuna River', 'San Joaquin River', 'Piscataqua River', 'River Trent', 'Solway Firth', 'Volga River', 'Irish Sea', 'Lake Maggiore', 'Nescopeck Creek', 'Lorraine', 'Yellow River', 'Conestoga River', 'Prut', 'Dniester', 'Rybinsk Reservoir', 'Loyalsock Creek', 'Godavari', 'Baskatong Reservoir', 'Syr Darya', 'Saskatchewan River', 'Abitibi River', 'Illinois', 'Chilko River', 'Ottawa River', 'Rappahannock River', 'Vecht', 'Blue Nile', 'Olifants River', 'Mediterranean Sea', 'Albemarle Sound', 'river Weser', 'Ural River', 'Paraguay River', 'Moscow River', 'Lake Beloye', 'River Westbourne', 'Ussuri River', 'Pripyat River', 'Similkameen River', 'Ruhr River', 'Murrumbidgee River', 'Hawkesbury River', 'Mezen', 'Garonne', 'Elbe', 'Chesapeake Bay', 'Altamaha River', 'River Rhine', 'Kansas River', 'Saginaw River', 'Sava River', 'Rhine', 'Kanawha River', 'Klamath River', 'River Swale', 'Connecticut River', 'Bristol Bay', 'River Niger', 'Pacific', 'Tennessee', 'Northern Dvina', 'Baltic Sea', 'Innerste', 'Red River', 'Neckar', 'San Pedro River', 'Clutha', 'Gariep River', 'Yangtze River', 'Hudson River', 'Amu Darya', 'river Tigris', 'Cooks River', 'Santa Maria River', 'Mobile River', 'Ganges River', 'Murray River', 'Northern Dvina River', 'Prypiat', 'River Tawe', 'Vardar', 'Narew river', 'Orange River', 'Juniata River']
White Deer Hole Creek
White Deer Hole Creek is a 20.5-mile (33.0 km) tributary of the West Branch Susquehanna River in Clinton, Lycoming and Union counties in the U.S. state of Pennsylvania. A part of the Chesapeake Bay drainage basin, the White Deer Hole Creek watershed drains parts of ten townships. The creek flows east in a valley of the Ridge-and-valley Appalachians, through sandstone, limestone, and shale from the Ordovician, Silurian, and Devonian periods. As of 2006, the creek and its 67.2-square-mile (174 km2) watershed are relatively undeveloped, with 28.4 percent of the watershed given to agriculture and 71.6 percent covered by forest, including part of Tiadaghton State Forest. The western part of White Deer Hole Creek has very high water quality and is the only major creek section in Lycoming County classified as Class A Wild Trout Waters, defined by the Pennsylvania Fish and Boat Commission as "streams which support a population of naturally produced trout of sufficient size and abundance to support a long-term and rewarding sport fishery." The rest of the creek and its major tributary (Spring Creek) are kept stocked. There are opportunities in the watershed for canoeing, hunting, and camping, and trails for hiking and horseback riding. Historically, two paths of the native indigenous peoples ran along parts of White Deer Hole Creek. Settlers arrived by 1770, but fled in 1778 during the American Revolutionary War. They returned and the creek served as the southern boundary of Lycoming County when it was formed on April 13, 1795. A logging railroad ran along the creek from 1901 to 1904 for timber clearcutting, and small-scale lumbering continues. During World War II a Trinitrotoluene (TNT) plant, which became a federal prison in 1952, was built in the watershed. Most development is in the eastern end of the valley, with two unincorporated villages, a hamlet, and most of the farms (many Amish).