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Preakness Range

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36: 1042: 746: 335:). Twelve other rare plants survive in forested uplands and the range's perched wetlands. Some of the rare plants are reasoned to take root in the range due to the calcareous secondary minerals in the range's trap rock which may serve to increase soil alkalinity relative to the surrounding acidic soils of the piedmont region. 246:. Mount Cecchino, the southernmost of the three and also the lowest, rises to 755 ft (230m). Immediately to the north, High Mountain reaches 879 ft (268m), becoming the highest peak of the Watchungs. Northwest of High Mountain, the second highest peak of the Watchungs, Beech Mountain, rises to 869 ft (265m). 323:
The Preakness Range may be the most environmentally sensitive section of the Watchungs, hosting a variety of ecologically diverse areas of wilderness. The New Jersey National Heritage Program has given the Preakness Range a rating of B2, meaning it has priority as a site with very high biodiversity
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The Preakness Range formed as molten rock extruded onto the surface 200 million years ago. At that time the range occupied the northern section of an active rift valley running through northern and central New Jersey and part of Pennsylvania. After the rift failed in the early Jurassic, the range
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An interesting trait of the Preakness Range is its alternating north-south valleys. These valleys, which form two major divisions, are a result of three separate eruptive events which laid down three closely spaced basalt ridges which combine to form the main section of the Preakness Range on the
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acting as buffer to hold back development from encroaching northward across the main ridge of Preakness Mountain. In the 1980s, when development began to threaten the remaining wilderness of the range, a push by local citizens to preserve the Preakness Range for the public interest was begun,
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northern end of Second Watchung Mountain. These ridges decrease in height from east to west, which mirrors the order in which the ridges, really successive sheets of lava, were formed. Here, as in the rest of the Watchungs, the easternmost ridge was extruded first.
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Thomas Francis Gordon. Gazetteer of the State of New Jersey – A General View of its Physical and Moral Condition, together with a Topographical and Statistical Account of its Counties, Towns, Villages, Canals, Railroads, &c. Published by D. Fenton, 1834.
211:, offering miles of hiking trails with vistas overlooking New Jersey and New York City. The peaks of the Preakness Range, the highest of the Watchung Mountains, shelter endangered ecosystems, including perched wetlands and rare trap rock glade communities. 227:, historically known as Totoway Mountain, flanks the Preakness Range in the east and is usually not included in the range, but it is mentioned in association with it, being part of the northern extent of First Watchung Mountain. 324:
significance. Nine different ecological communities have been cited in the Preakness Range, including globally imperiled trap rock glade communities and increasingly rare hickory-ash red cedar woodlands.
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For most of modern history the Preakness Range remained a wilderness providing recreation to the inhabitants of surrounding towns. Only the southern section of the range was particularly built up, with
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The mountains of the Preakness Range also provide significant habitat to wildlife. In particular, sixty species of birds are thought to breed in the range's various environs.
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Joseph Dowhan et al. Significant Habitats and Habitat Complexes of the New York Bight Watershed. U.S. Fish and Wildlife Service, 1997.
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was elevated as erosion removed the sandstone and shale surrounding the basalt lava flows of Preakness Mountain and Packanack Mountain.
223:. Packanack Mountain, a section of Third Watchung Mountain west of Preakness Mountain, is sometimes included in the Preakness Range. 1033: 1086: 567:
Bulletin of the United States Geological Survey No. 67 – The Relations of the Traps of the Newark System in the New Jersey Region
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The Preakness Range generally refers to the peaks of Preakness Mountain, the section of Second Watchung Mountain north of the
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Seven state-listed endangered plant species call the Preakness Range home, including a globally endangered species, Torrey's
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The Indians of New Jersey: Their Origin and Development; Manners and Customs; Language, Religion, and Government
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Note: Ethel Kauffman organized a group which blocked residential development on High Mountain.
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As with the majority of the Watchungs, the Preakness Range saw use as a lookout during the
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The Papers of George Washington: Revolutionary War Series volume 10, June – August 1777
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can be seen across a valley from a ledge near the summit of High Mountain in
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Geological Survey of New Jersey - Bulletin 14 The Geology of New Jersey
258:. Today, this Native American heritage lives on in the range's name. 765: 532:
North Jersey Record Obituaries – Ethel Kauffman, open space activist.
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The Preakness Range was originally inhabited by the Munsee (Minsi)
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USGS Mineral Resources On-Line Spatial Data – Preakness Basalt
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U.S. Geological Survey - NYC Regional Geology, Mesozoic Basins
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Available via the US FWS National Conservation Training Center
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New York-New Jersey Trail Conference – High Mountain (NJ)
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New York-New Jersey Trail Conference - Watchungs Region
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Geology of the Newark Basin and Connecticut River Basin
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The Magazine of American history with Notes and Queries
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Geographic Provinces: Piedmont - Watchung Mountains
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In October and November, 1780 1040: 744: 266:, a Lenape term thought to mean 34: 1: 511:John Austin Stevens, et al. 230:Preakness Mountain begins in 195:is a range of the trap rock 635:Geology of the Newark Basin 502:, accessed October 18, 2006 300:High Mountain Park Preserve 295:William Paterson University 209:High Mountain Park Preserve 199:on the western edge of the 1103: 578:Available via Google Books 521:Available via Google Books 467:Available via Google Books 426:Available via Google Books 392:Available via Google Books 283:American Revolutionary War 1030: 742: 515:. A. S. Barnes., 1879. 99:40.9700722°N 74.1983556°W 33: 26: 565:Nelson Horatio Darton. 137:United States of America 71:879 ft (268 m) 1087:Volcanism of New Jersey 287:General Arthur St Clair 104:40.9700722; -74.1983556 884:Hudson River Palisades 831:New Germantown/Oldwick 672:Orange Mountain Basalt 477:Hutchinson, Viola L. 1077:Ridges of New Jersey 692:Hook Mountain Basalt 1037: • 958:Buckingham Mountain 723:Lockatong Formation 677:Feltville Formation 333:Pycnanthemum torrei 240:Oakland, New Jersey 95: /  1082:Watchung Mountains 1047:Geology portal 928:Cushetunk Mountain 899:Clausland Mountain 775:Watchung Mountains 718:Stockton Formation 498:2006-10-21 at the 457:Nelson, William. 442:2008-12-26 at the 232:Totowa, New Jersey 197:Watchung Mountains 53:Highest point 28:Watchung Mountains 1054: 1053: 1026: 1025: 985: 984: 981: 980: 953:Solebury Mountain 933:Sourland Mountain 861: 860: 808:Watchung Outliers 740: 739: 736: 735: 728:Passaic Formation 713:Doswell Formation 697:Boonton Formation 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Index

Watchung Mountains

Goffle Hill
Wayne, New Jersey
Elevation
Coordinates
40°58′12.26″N 74°11′54.08″W / 40.9700722°N 74.1983556°W / 40.9700722; -74.1983556
United States of America
New Jersey
Age of rock
Triassic
Jurassic
Type of rock
extrusive igneous
trap rock
Watchung Mountains
Newark Basin
New Jersey
High Mountain Park Preserve
Passaic River
Goffle Hill
Totowa, New Jersey
Ramapo fault
Oakland, New Jersey
Wayne, New Jersey
Lenape
American Revolutionary War
General Arthur St Clair
William Paterson University
High Mountain Park Preserve

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