| Stony Clove Creek | |
|---|---|
 Stony Clove Creek in Phoenicia, just above its mouth | |
  Location of the mouth of Stony Clove Creek Show map of New York Adirondack Park Stony Clove Creek (the United States) Show map of the United States | |
| Location | |
| Country | United States |
| State | New York |
| Region | Catskill Mountains |
| Counties | Ulster,Greene |
| Towns | Hunter,Shandaken |
| Physical characteristics | |
| Source | Notch Lake |
| • location | Stony Clove Notch, N ofEdgewood, New York, U.S. |
| • coordinates | 42°09′34″N74°12′15″W / 42.1595332°N 74.2040319°W /42.1595332; -74.2040319[1] |
| • elevation | 1,980 feet (600 m) |
| Mouth | Esopus Creek |
• location | Phoenicia, New York, U.S. |
• coordinates | 42°04′53″N74°18′52″W / 42.0814794°N 74.3143143°W /42.0814794; -74.3143143[1] |
• elevation | 804 ft (245 m)[1] |
| Length | 10.3 mi (16.6 km) |
| Basin size | 32.4 square miles (83.9 km2)[2] |
| Discharge | |
| • location | Chichester |
| • minimum | 3.1 cu ft/s (0.088 m3/s) |
| • maximum | 14,300 cu ft/s (400 m3/s) |
| Basin features | |
| Tributaries | |
| • left | Warner Creek |
| • right | Myrtle Brook,Hollow Tree Brook,Ox Clove Brook |
Stony Clove Creek is a 10.3-mile-long (16.6 km)[3] creek in theCatskill Mountains inNew York. It is a tributary ofEsopus Creek, which in turn is a tributary of theHudson River. It joins the Esopus in the village ofPhoenicia, and has two smaller tributaries up north of Phoenicia.
The Stony Clove starts near theStony Clove Notch in Edgewood inGreene County. It originates atNotch Lake, near the Devil's Tombstone Campsite, and flows through the small villages of Edgewood and Lanesville, enteringUlster County atChichester.
Early maps and deeds indicate that the Stony Clove flowed into the Warner Bushkill, or alternatively named, the Barber Bushkill, before flowing into the Esopus. Later cartographers have changed the nomenclature of the streams so that the Barber Bushkill or Warner Bushkill flows into the Stony Clove.
It was formed about 10,000 years ago, during the lastIce age. It was formed when the same meltwater that formed the Stony Clove Notch burst through, and flooded a valley. The water, in turn, started running down through an already gouged-out pass, forming a smallriver.
TheUnited States Geological Survey (USGS) maintainsstream gauges along Stony Clove Creek. The station in Chichester in operation since 1997, 1.8 miles (2.9 km) upstream from the Esopus, had a maximum discharge of 14,300 cubic feet (400 m3) per second on August 28, 2011, asHurricane Irene passed through the area. It had a minimum discharge of 3.1 cubic feet (0.088 m3) per second on October 3, 2014.[4] A former station in operation from February 1997 to August 2007, 1.3 miles (2.1 km) upstream from the Esopus, had a maximum discharge of 13,000 cubic feet (370 m3) per second on April 2, 2005, and a minimum discharge of 3.7 cubic feet (0.10 m3) per second from September 20–22, 2002.[5]
Stony Clove Creek is the largest source of turbidity and suspended-sediment concentration in the upper Esopus Creek, accounting for more turbidity than the rest of the upper Esopus watershed combined.[6]
The USGS station along the creek in Chichester collects turbidity data every 15 minutes. The maximum daily SSC mean was 2,860 mg/L on December 1, 2010, and the minimum was under 1 mg/L over many days in late August through September 2014. The maximum daily suspended sediment discharge was 8,860 tons (8,040 t) on September 18, 2012, and the lowest was less than 0.01 tons (0.0091 t) from January 15–17, 2012 and many days in September 2013.[4]
