Pochuck Mountain

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Pochuck Mountain
White Birch Road within the Scenic Lakes community leading down one of the southwestern peaks of Pochuck Mountain.
Highest point
Elevation1,194 ft (364 m)
Prominence695 ft (212 m)
Coordinates41°12′40″N 74°31′50″W / 41.21111°N 74.53056°W / 41.21111; -74.53056
Geography
LocationSussex County, New Jersey / Orange County, New York, U.S.
Parent rangeAppalachian Mountains
Topo mapUSGS Pochuck Mountain

Pochuck Mountain is a

New York-New Jersey Highlands region of the Appalachian Mountains. Pochuck Mountain's summit and most of its peaks lie within Vernon Township, Sussex County, New Jersey, although the south-western portion of the ridge lies within Hardyston Township, and the north-eastern tip of the ridge extends over the New York state line into Orange County. The ridge marks the eastern edge of the Great Appalachian Valley, and it divides the watersheds of the Wallkill River and its tributary Pochuck Creek
. The two rivers meet at Pochuck Neck, marking the terminus of the ridge.

Etymology

The name Pochuck is a

prominence
of approximately 695 feet.

Geography

Pochuck Mountain and Wawayanda Mountain to the east form the borders of the Vernon Valley, an important farming and mining area of New Jersey drained by Pochuck Creek. Immediately to the northwest of the ridge lies the Black Dirt Region, which is drained by the Wallkill River. Both valleys are part of an elongated lowland region known as the Great Appalachian Valley that divides the Appalachian Mountains for hundreds of miles. Due to the unusual positioning of Pochuck Mountain relative to the neighboring mountains, the Vernon Valley is a somewhat isolated prong of the rest of the Great Appalachian Valley.

Watershed

As the entire mountain is drained by the Wallkill River and its tributary Pochuck Creek, the region lies completely within the Wallkill River watershed. The Wallkill River flows northeast until it joins Rondout Creek near Rifton, New York. Rondout Creek then tributes the Hudson River in Kingston, New York. The Hudson River ultimately drains into the Atlantic Ocean via the New York Harbor.

Lakes on Pochuck Mountain include Lake Glenwood, Lake Pochung, Lake Wallkill, Pleasant Valley Lake, Tall Timbers Lake, Lake Panorama, Louemma Lake, and Scenic Lakes (2 manmade lakes in the

swimming, boating and ice skating
.

Mountain passes

Appalachian Trail

The Appalachian Trail runs over the top of the ridge within Wawayanda State Park, north of the summit.

Geology

Pochuck (center) seen from the north

Pochuck Mountain is part of the Reading Prong of the New England Uplands subprovince of the New England province of the Appalachian Highlands. In fact, it is the northernmost ridge of the Reading Prong in New Jersey. The rocks that form Pochuck Mountain are comprised from the same belt that make up nearby Wawayanda Mountain. This belt consists of ancient crystalline metamorphic rocks. As such, the New England province as a whole, along with the similarly composed Blue Ridge province further south, are often together referred to as the Crystalline Appalachians.

The Crystalline Appalachians extend as far north as the

Kittatinny Mountains
are representative of these sedimentary formations.

Portions of the Reading Prong in New Jersey are known to contain Uranium deposits, linked to reported Radon contamination in certain residential areas developed on the prong.[2] The naturally occurring Radon (226Ra) is a product of the decay chain of the Uranium isotope 238U.[3]

Wildlife

Mammals inhabiting Pochuck Mountain include black bear, white-tailed deer, opossum, foxes, raccoons, squirrels, skunk, bobcat, fisher, porcupine, coyote bats, chipmunks, groundhogs and field mice.

Industry

While the developed portions of Pochuck Mountain have largely been put to residential use, the mountain and its foothills have historically been a center for

habitat loss
for native and migratory species.

References

  1. ^ Hikes in the Mid-Atlantic States
  2. ^ The Pennsylvania Radon Story
  3. ^ "Principal Decay Scheme of the Uranium Series". Archived from the original on 2008-10-25. Retrieved 2008-08-01.

External links