Bogs receive most of their water input from rain and snow; fens like Quincy Bog receive most of their water from streams and groundwater. The boardwalk features three observation decks over the … 101A. Furthest out are the upland kame ridges surrounding Flatiron Lake that are covered by mature oak-maple forests. The route is less than a mile. It illustrates characteristics of a typical sphagnum-heath bog, localized in a specialized geologic setting. About 18,000 years ago, New Hampshire was covered by a continental ice sheet almost a mile thick. Ponemah Bog Length: 0.8 mile loop Difficulty (click for info): Beginner Elevation Gain: 0 feet Rating (click for info): 7/10 Type: Kettle-Hole Bog Driving Directions: Trailhead and parking area are at the end of Rhodora Drive, in Amherst, NH. In 1972, its uniqueness was recognized by the National Park Service as a National Natural Landmark. Bogs lack drainage, and precipitation is the only source of water. . But . Bog water is acidic and lacks oxygen. There were once six kettle holes known to exist in southern New Hampshire; all but Spruce Hole have been destroyed. This kettle hole pond, named for James Smith who settled nearby in 1765, covers almost eight acres. A few years later, the Durham Conservation Commission successfully negotiated ownership of the bog. Sphagnum mosses are the dominant plants forming a thick layer of peat. A trail network leads from the abutting 172-acre Oyster River Forest to the bog. Nottingcook Forest trails are primarily used for hiking, walking, and nature trips and is accessible year-round. Address: 295 Newport Road, New London, NH 03257.
Quincy Bog was formed as a kettle hole bog over 12,000 years ago at the end of the Ice Age and gradually became a fen as decomposing plant material filled in the kettle hole. ... PO Box 90, Rumney, NH 03266-0090 . Park at the small turnout on the right (south) side of the road. The Philbrick-Cricenti Bog Trail system starts at the parking area (P) on the south side of Newport Road opposite the entrance to the Great Pines development and .3 miles west of the Hannaford Supermarket.
Mar 31, 2016 - Bonnett Pond Bog State Nature Preserve is a high-quality sphagnum kettle-hole bog. The bog’s is a “kettle hole pond” and was formed some 12,000 years ago when a large chunk of glacial ice broke off to form the bog. Kettle bogs If water in a kettle becomes acidic due to decomposing organic plant matter, it becomes a kettle bog; or, if underlying soils are lime -based and neutralize the acidic conditions somewhat, it becomes a kettle peatland. Location: Strafford County, NH Year designated: 1972. It is an acid, kettle-hole bog that displays the classic ringed zonation of bog plant communities. The bog is surrounded by wetland and forested upland natural communities. Carnivorous plants and some of the other unique flora found here are limited to bogs and found nowhere else.
Which ones will you be trying this year? One of his happy discoveries was a true kettle-hole bog within two miles of his lab in Thompson Hall. .
From exit 12 on I-89, take Newport Rd (old NH-11) east towards New London for 1 mile. The Spruce Hole Bog, locally known as Spruce Hole, is a complete ecological community occupying a true kettle hole in the town of Durham, New Hampshire.According to the National Register of Natural Landmarks: "It illustrates characteristics of a typical sphagnum-heath bog, localized in a specialized geologic setting." For permitted uses, trail lengths and history, see Trail Map (above) created by Bow Open Spaces, Inc.
Ponemah Bog Wildlife Sanctuary features a three-acre pond surrounded by a floating sphagnum mat and encircled by upland oak-pine woods. Ponemah Bog is the centerpiece of a 75-acre sanctuary in southern New Hampshire, just an hour from Boston. Known to the locals as "Spruce Hole," the bog, a unique geological formation created at the end of the last ice age, was known for its ancient beauty as well as the secrets it concealed. A kettle hole pond is created when a block of ice, buried in soil left behind by a retreating glacier, eventually melts and creates a deep, steep-sided pond.
And then, the temps were frigid and our time limited, so we only snowshoed to the Kettle Hole Bog. Then why is it called “Quincy Bog”? It blows my mind to think that kettle holes are unique features formed over 10,000 years ago when big chunks of ice became stranded and partially buried in glacial outwash or other coarse ice-contact deposits. May and June are good months to see the flowering plants in bloom.
Here are a few other boardwalks that include scenery ranging from bogs to forest to the beach!
NH Kettle Korn - PO Box 2036, North Conway, New Hampshire 03860 - Rated 5 based on 20 Reviews "Best kettle corn ever!! At the center of the property is a three-acre kettle-hole pond, encircled by a floating mass of sphagnum moss and easily accessible by a viewing boardwalk.
Kettle Hole Bog.
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