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Geology of Jersey. The geology of Jersey is characterised by the Late Proterozoic Brioverian volcanics, the Cadomian Orogeny, and only small signs of later deposits from the Cambrian and Quaternary periods. The kind of rocks go from conglomerate to shale, volcanic, intrusive and plutonic igneous rocks of many compositions, and metamorphic rocks ...
The diabase rock was used as building material in growing areas like Jersey City. The remnant of the hill is the defining feature of Laurel Hill County Park. The high point, a 203-foot (62 m) graffiti-covered inselberg rock formation, is a familiar landmark to travelers on the New Jersey Turnpike's Eastern Spur, which skirts the hill's southern ...
Les Pierres de Lecq (Jèrriais: Les Pièrres dé Lé) or the Paternosters are a group of uninhabitable rocks or a reef in the Bailiwick of Jersey between Jersey and Sark, 6 km (3.7 mi) north of Grève de Lecq in Saint Mary, and 22.4 km (13.9 mi) west of the Cotentin Peninsula in Normandy.
Le Pinacle is a protruding pinnacle of rock, at the coastal edge of a Les Landes in the north-west of Jersey, [1] with remains and ruins at its base dating from five periods including the Neolithic and Chalcolithic periods, the Bronze Age, and the Iron Age. There is also evidence of a rectangular Gallo-Roman temple. [2]
Zion, New Jersey was a village located at Long Hill Road and Rock Brook. A mill was built along Rock Brook, giving the village the name of Rock Mill and later Rock Mills. The village had numerous houses, a saw-mill, a store, a blacksmith, wheelwright shops and the Boozer School.
Rock Lodge pond swimming lake. Rock Lodge Club is a naturist club located on 145 acres (59 ha) of privately owned land located in the Stockholm area of the Hardyston Township, New Jersey, which is situated on the New Jersey Highlands of North Jersey, about 40 miles (64 km) from Manhattan, New York.