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Sunrise Mountain (New Jersey)

Kittatinny MountainsMountains of New JerseyMountains of Sussex County, New JerseyNew Jersey geography stubsPapakating Creek watershed

Sunrise Mountain is a peak of the Kittatinny Mountains in Sussex County, New Jersey, United States. The mountain is 1,650 feet (503 m) tall, and overlooks Beemerville to the east. It lies along the Appalachian Trail in Stokes State Forest. The crest of Sunrise Mountain is one of the most frequently visited sites in Stokes State Forest. The thin soil and harsh climate characteristic of Sunrise Mountain is a difficult environment in which few plants can survive. Mountain laurel, blueberry, pitch pine and bear oak are among the natural vegetation found throughout the area. The pavilion at the summit was built in the late 1930s by the Civilian Conservation Corps.

Excerpt from the Wikipedia article Sunrise Mountain (New Jersey) (License: CC BY-SA 3.0, Authors).

Sunrise Mountain (New Jersey)
Appalachian Trail, Frankford Township

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Geographical coordinates (GPS)

Latitude Longitude
N 41.2181512 ° E -74.7204422 °
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Sunrise Mountain Pavillon (Civilian Conservation Corps Pavilion)

Appalachian Trail
07826 Frankford Township
New Jersey, United States
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Rutan Hill
Rutan Hill

Rutan Hill (also called Volcanic Hill) is the local name for a hill on the United States Geological Survey Branchville 7.5-minute map. It is located about 2.46 miles (3.96 km) south-southwest of Colesville, New Jersey in Wantage Township, of Sussex County, New Jersey in the United States. Rutan Hill rises about 270 feet (82 m) above the adjacent creek valley to an elevation of just over 1,020 feet (310 m). This hill lies entirely within private, posted property. This nondescript hill is the surface expression of a diatreme that is the northern part of the Late Ordovician Beemerville Alkaline Complex.The surface exposures of the Beemerville Alkaline Complex consist of two large nepheline syenite plutons; a nearby diatreme (Rutan Hill); and several other nearby and much smaller dikes, sills, and diatremes. The two large nepheline syenite plutons are located south-southwest of Rutan Hill along the contact between the Martinsburg and Shawangunk formations and on the southeast side of Kittatinny Mountains. The dikes or sills consist either of phonolite, tinguaite, lamprophyre micromalignite, lamprophyre micromelteigite, or carbonatite. The Beemerville Alkaline Complex also includes several lamprophyric diatremes that contain xenoliths of sedimentary rocks and gneiss and autoliths of carbonatite, potassic syenite, and lamprophyre micromelteigite.Rutan Hill is the surface expression of the largest of the lamprophyric diatremes within the Beemerville Alkaline Complex. This diatreme contains a small plug-like body of nepheline syenite that is about 30 meters (98 ft) in diameter and is choked with variety of angular to subangular xenoliths and autoliths. The xenoliths consist of shale and graywacke, fine-grained pale-blue dolomite, cream-colored fine-grained limestone, and gneiss. The autoliths consist of nepheline syenite, micromelteigite, and carbonatite. The matrix consists of an extremely fine-grained groundmass with fine-to coarse-grained megacrysts of biotite, diopside, aegerine-augite, orthoclase, magnetite, apatite, and nepheline.Rutan Hill and the associated Beemerville Alkaline Complex are the surface exposures of a much larger alkaline igneous intrusion that underlies the area of Beemerville, New Jersey. This igneous intrusion is part of the larger Cortlandt-Beemerville magmatic belt. They occur at the western end of the Cortlandt-Beemerville magmatic belt, which spans parts of northern New Jersey and southeastern New York. The Cortlandt complex, New York, defines the eastern end of this belt. Between the Beemerville alkaline complex and the Cortlandt igneous complex, this magmatic belt consists of a linear, almost east–west trending, zone of lamprophyre and felsic dikes.The currently accepted age for the emplacement Beemerville Alkaline Complex is 420 ± 6 Ma. This age is derived by the fission track dating of titanite. Mean apatite fission-track age of 156 ± 4 Ma is interpreted to represent the time the rocks of the complex were last at temperatures of 60 °C to 100 °C. Previously, Rb-Sr and K–Ar dating of biotite from the nepheline syenite at Beemerville yielded ages of about 435 ± 20 Ma (444 Ma. using current decay constants) for the Beemerville Alkaline Complex. All of these dates are consistent with the observations that the dikes of the Beemerville Alkaline Complex crosscut folded and foliated strata of the Martinsburg Formation as young as early Late Ordovician but are not known to intrude younger rocks.Based upon emplacement models for diatremes it can be inferred that the diatreme that forms Rutan Hill is the throat of an ancient, extinct volcano. However, erosion following its eruption has either completely destroyed the volcanic cone and any superficial volcanic deposits associated with it or any remaining volcanic deposits lie deeply buried as none have been mapped at the surface within the Beemerville area.This igneous complex was emplaced and the volcanic activity, which was presumably associated with it, occurred during the end of the Taconic Orogeny in the late Ordovician period. The temporal association with this Ordovician tectonism suggests that this magmatic activity may be related to fracturing of mantle rock at the junction of two Taconic age tectonic salients that intersect in the New York region. The tectonic setting of the intrusive belt is unusual because it is associated in space and time within the zone of compressional mountain building that defined the Taconic Orogeny. At that time, the western half of the Iapetus Ocean lying along the east coast of Laurentia was closing, being subducted beneath the Taconic (or Bronson Hill) Island Arc.

Frankford Township, New Jersey
Frankford Township, New Jersey

Frankford Township is a township in Sussex County, in the U.S. state of New Jersey. As of the 2020 United States census, the township's population was 5,302, a decrease of 263 (−4.7%) from the 2010 census count of 5,565, which in turn reflected an increase of 145 (+2.7%) from the 5,420 counted in the 2000 census.Frankford Township was formed on April 10, 1797, from portions of Newton Township, and was incorporated on February 21, 1798, as one of New Jersey's initial 104 townships by an act of the New Jersey Legislature. Portions of the township were taken to form Lafayette Township and Sparta Township (both established on April 14, 1845), along with Branchville (March 9, 1898), which is completely surrounded by the township. The township was said to have been named after Frankford, a neighborhood of Philadelphia, after a visitor who hailed from that area came to help out at the rural school in the township.Since 1976, the township has been the home of the Farm and Horse Show, which expanded after it was relocated from Branchville. The New Jersey State Fair / Sussex County Farm & Horse Show has evolved as the site of numerous activities and events throughout the year. The township's Skylands Park, a 4,300-seat baseball park, was home to the New Jersey Cardinals of the New York–Penn League from 1993 to 2005, and the Sussex Skyhawks of the Can-Am League from 2006 to 2010. Since 2005, the stadium is the home of the Sussex County Miners, which plays as part of the Frontier League.

Montague Township, New Jersey
Montague Township, New Jersey

Montague Township is a township in Sussex County, in the U.S. state of New Jersey, in the New York City Metropolitan Area. As of the 2020 United States census, the township's population was 3,792, a decrease of 55 (−1.4%) from the 2010 census count of 3,847, which in turn reflected an increase of 435 (+12.7%) from the 3,412 counted in the 2000 census. High Point, within Montague Township, is the highest elevation within New Jersey at an altitude of 1,803 feet (550 m) above sea level. Montague is also the northernmost municipality in the state of New Jersey. Most of the area of Montague Township is public lands, primarily High Point State Park, Stokes State Forest, and Delaware Water Gap National Recreation Area. Montague is known for its scenery and wildlife; summer sports in the area include hiking, biking, camping (both public and private campgrounds are available), and fishing. The derivation of the township's name is uncertain, though suggestions include that it was named after the George Montagu, 4th Duke of Manchester, as suggested by King George II, who approved the royal patent on March 26, 1759; for Lady Mary Wortley Montagu, an author who was popular at the time; or for solicitor John Montague. Montague was incorporated on February 21, 1798, by an act of the New Jersey Legislature as one of New Jersey's initial group of 104 townships.The township borders both New York and Pennsylvania, the only municipality in New Jersey to border both states; it is a rural community that does not have any traffic lights. Before Montague Township was granted its own post office in the 1980s, residents had all of their mail delivered through the 12771 ZIP code for Port Jervis, New York, leading to situations where residents had New Jersey driver's licenses with a New York State mailing address.

Culver's Lake
Culver's Lake

Culver's Lake (formerly Round Pond) is a lake located in Frankford Township, in Sussex County, New Jersey. Fed by Lake Owassa and Bear Swamp, Culver's Lake is the source of the West Branch of the Paulins Kill (also known as the "Culver Brook"). In the late 19th and early 20th century, the lake was used for seasonal recreation. Today, it is a private year-round community owned and operated by the Normanoch Association, a homeowners' association.The lake has a surface area of approximately 555 acres (225 ha) and a shoreline roughly six and a half miles long. It has a maximum depth of 50 feet (15 m) and is located at an elevation of 830 feet (250 m) above sea level. It is located near the Culver Gap, a wind gap in Kittatinny Mountain, and where the Appalachian Trail intersects with U.S. Route 206. Culver Gap near Culver's Lake in Sussex County, New Jersey, was an important route through the Kittatinny Mountain from about 10,000 years ago to present. The gap is more than 400 feet (120 m) below the top of the mountain. Lenape Native Americans used the gap to hunt and trade on both sides of the mountain. Early settlers from Pennsylvania used the water drop from Culvers Lake to Branchville for a wide assortment of mills. Turnpikes followed the route of Lenape trails through the gap. The lake is named for a local clergyman, the Reverend Jabez Collver (1731-1818), who led the Congregational Church in Wantage Township, New Jersey. On September 14, 1774, he purchased 163 acres of land east of Kittatinny Mountain near the lake. However, after the American Revolution, Collver fled to Ontario, Canada after the American Revolution due to his loyalist sympathies.