Kittatinny Mountains
From Wikipedia, the free encyclopedia
The Kittatinny Mountains are a long ridge across northwestern New Jersey running in a northeast-southwest axis. It is the first major ridge in the Ridge and Valley province of the Appalachian Mountains.
Contents |
[edit] History and Geology
The name comes from a Lenape Native American word meaning "endless hill" or "great mountain".[1] The highest peak in the range is High Point at 1,803 feet (550 meters), which is also the highest point in the state of New Jersey. This peak is located in High Point state park and has a road leading to the top The second highest mountain is Sunrise Mountain, located within Stokes State Forest. The elevation here is 1653 feet and has a road leading almost to the top. At the top there is a shelter with a roof with no sides.
The Kittatinny Mountain is of the Silurian Shawangunk Conglomerate which is mainly composed of quartz. Due to the hardness of the quartz, makes the mountain extremely resistant to weathering. Near the base of the west side of the mountain is the Silurian High Falls formation, which is red and green shale and sandstone. The east side of the mountain near the base is of the Ordovician Martinsburg Formation which contains slate, shale and sandstone. The top of the mountain has a fairly even elevation ranging between 1400 feet and 1600 feet. There are two exceptions. One is Culver's Gap, which was created by an ancient stream which was diverted and is now a wind gap. The base of Culver's Gap is at least 400 feet below the top of the mountain. Culver's Gap is located near Culver's Lake, just west of Branchville.
Culver's Gap was a route used by Paleo Indins and the Lenape Native Americans to go through the mountain to trade and hunt. The second is a groove or depression in the mountain ridge near Catfish Pond. This is about 100 feet deep. The top of the mountain ranges from 50 meters wide to nearly 4 miles or 7 km wide.
West of the the Kittatinny Mountain is the Port Jervis trough or a wide valley, called the Minisink Valley. From Delaware Water Gap to the New York line is 21 miles but the ridges continues into New York State where it is know as the Shawangunk Mountain. The ridge continues to nearly Kingston, New York.
The Wisconsin glacier covered the entire mountain about 21,000 BC, and melted about 13,000 BC. The terminal moraine is located near Belvidere. The glacier has left end moraines at the northern end of the mountain in Stokes State Forest.
The area was a Tundra biome after the glacier melted and then became a Taiga biome as the climate warmed. At that time coniferous trees such as spruce and pine inhabited the area.
[edit] Paleo Indians
Paleo Indians inhabited the Delaware River Valley around 10,500 BC. They hunted, fished and gathered plants to eat in the Delaware Valley and on Kittatinny Mountain. They had no permanant camps and traveled often in search of food. The area was coniferous and deciduous forests mixed with grasslands in the valleys. The Marshall Creek Mastadon found just north of the Gap was dated at 10,210BC+ or - 180 years. Other big game existed at the time such as caribou and musk ox.
[edit] Native Americans
The Lenape Native Americans that came to the area two thousand years ago, traveled on the mountain in search of food and game. There was a deciduous forest with many varieties of nut trees, Native Americans collected these foods. They collected acorns, walnuts, hickory nuts, beech nuts, chestnuts, and butternuts. Fresh water streams were used to collect water. Game such as deer, elk, and bear was hunted on the mountain.
[edit] Waterfalls, Cliffs and Lakes
There is one waterfall on the western side of the mountain known as Buttermilk Falls. This is about 4 miles south of Route 206, in which a dirt road leads to the base of it. A wooden stair case has been built near it, so people can climb to the top. A second falls is seasonable during heavy rains next to Route 80 near the Big Cliffs. Water slides over the rocks and drops over a small ledge before going under Route 80.
There are several cliffs on the mountain. The largest is located at the Delaware Water Gap. The cliff is up to 300 feet high and starts at Route 80 and extends about 400 meters along the mountain The second largest cliff is located 6 miles north of the Gap, on the eastern side. Small rock faces exist on the western face and eastern face along the mountain. The southeastern face of the mountain has a steeper pitch than the northwestern face.
The top of the mountain has 14 lakes and ponds. Sunfish Pond, Catfish Pond, Mountain Ridge Lake, Blue Mountain Lake, Long Pine Pond, Lake Success, Crater Lake, Hemlock Lake, Kittatinny Lake, Steeny Kill Lake and Lake Marcia are some of them. Lake Marcia is the lake with the highest elevation on the mountain, 1574 feet (479 meters) above sea level. This lake is located in High Point State Park which is at the northern end of Kittatinny Mountain.
[edit] Flora and Fauna
The mountain is a northern deciduous forest comprised of various oaks, hickories, maples, birches, as well as walnut, elm, ash, birch, sycamore, cherry, beech, chestnut, and sweet gum. Wild blueberries and rhodendrum also grow on the mountain. Animals such as whitetailed deer, gray squirrel, chipmunks, gray fox, beaver, black bears as well as a large variety of birds inhabit the mountain. Turkey Vultures and Red Tail Hawks are also common.
[edit] Mining
Copper mining began around 1740 at the Pahaquarry Mines which is 8 miles north of the Gap, off Old Mine Road. This mine is located in the Silurian High falls Formation on the west side of the mountain. This sandstone is very hard and made mining very difficult. The copper was between 2 to 3 percent in the ore which made mining unprofitable. Mining was done in the 1800's by various companies which went bankrupt and sold the mine to another company.
[edit] Kittatinny and Flatbrook Valleys
To the east of the Kittatinny Mountain, is the Great Kittatinny Valley. This is drained by the Paulinskill river in the south and the Wallkill River in the north. The Big Flatbrook drains the mountain on the northwestern end beginning at Sawmill swamp and flows in a southwesterly direction which drains into the Delaware River near Flatbrookville. This area is known as the Flatbrook Valley. The Delaware River flows near the mountain at the south end, finally cutting across the ridge at the Delaware Water Gap just south of Mount Tammany.
The Kittatinnies are part of the Ridge and Valley province of the Appalachian Mountains. In Pennsylvania, the ridge forming the Kittatinnies becomes known as Blue Mountain and runs southwest for 150 miles, nearly to Maryland. In Franklin County, PA, however, a parallel ridge to Blue Mountain is named "Kittatinny Mountain"; the Pennsylvania Turnpike tunnels through both ridges (a very short distance apart) with the western tunnel named "Kittatinny Mountain" and the eastern one "Blue Mountain." To the north in New York, the ridge is known as the Shawangunk Mountains.
[edit] See also
[edit] References
- ^ What's in a name, Spanning the Gap newsletter of the Delaware Water Gap National Recreation Area, Summer 1984
[edit] External links
 |
This New Jersey state location article is a stub. You can help Wikipedia by expanding it. |
