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Topic: Kettle hole

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	[No title] (Site not responding. Last check: 2007-10-07)
		Later, as the ice block melted, the overlying sediment collapsed and left a depression in the ground surface.
		Some of these kettle holes have ponds of lakes in them kettle lakes).
		Kettle holes may be as small as a car, or as big as a house or city block.
	www.science.uwaterloo.ca /earth/waton/kettle.html (158 words)

	MSN Encarta - Search Results - Kettle Hole (Site not responding. Last check: 2007-10-07)
		Kettle Hole, hollow formed when a glacier recedes, leaving behind great chunks of ice covered by debris from the retreating glacier.
		Once meltwater streams leave the snout of a glacier their ability to transport material is rapidly reduced.
		Black Hole, hypothetical body with a gravitational field that curves the space around it so strongly that nothing, including electromagnetic...
	uk.encarta.msn.com /Kettle_Hole.html (91 words)

	Quit Qui Oc Golf Club Glacial Nine (Site not responding. Last check: 2007-10-07)
		Specifically, the landscaping in the Kettle Moraine Area is related to the last advance and retreat of the glacier, approximately 30,000 to 13,000 years ago.
		A kettle is a depression formed when a block of ice in front of a retreating glacier gets buried by outwash and later melts.
		A prominent but small kettle can be observed on the right side of the path going from hole #5 to hole #6.
	www.quitquioc.com /course/glacial.htm (663 words)

	Kettle Hole
		Kettle holes are depressions left by the melting of an ice block lodged in a deposit of till or drift.
		Kettles are often found embedded in moraines and on outwash plains.
		Kettle lakes occur where the kettle hole is filled with water.
	www.uwsp.edu /geo/faculty/ritter/glossary/h_k/kettle_hole.html (73 words)

	Science Education Goals (Site not responding. Last check: 2007-10-07)
		The location that I chose, the "Kettle Hole Trail", is part of the Long Island Greenbelt Pine trail system that winds through the Pine barrens, and climbs from a glacial topography of outwash plain to a hummocky terminal moraine.
		The Kettle Hole trail begins on the northern edge of the outwash plains and eventually climbs onto the Ronkonkoma Moraine, in an area that has been described at classically knob and kettle (Fuller, 1914).
		Kettles are formed when large blocks of ice, left behind from the receding glacier, are covered by outwash sediments.
	pbisotopes.ess.sunysb.edu /esp/589_98/griffin (3766 words)

	Welcome to Captains Golf Course
		A scenic par three with a green framed by bunkers that was considered by many to be the signature hole of the original Captains, this downhill hole may require one less club than you think off the tee.
		Another hole where accuracy off the tee is more important than length, especially when you factor in a green that is guarded by a mature oak short and left and a yawning bunker right front.
		Take the hint of the fairway bunkers for the second hole in a row in order to avoid the mature trees that infringe on the left side of the fairway between the landing area and the green.
	www.captainsgolfcourse.com /starboard.html (928 words)

	Kettle Hole Trail (Site not responding. Last check: 2007-10-07)
		The Kettle Hole Trail is a pathway through one of the most ecologically significant ecosystems in the United States.
		The trail divides at the outer rim of the Kettle Hole.
		The Kettle Hole is an irregularly shaped depression that is formed when large chunks of ice are left behind by a receding glacier.
	pbisotopes.ess.sunysb.edu /esp/589_98/griffin/guide.html (2627 words)

	Welcome to Captains Golf Course
		Relatively flat, this starting hole bends slightly left and requires a mid to short iron into a two level green flanked by bunkers.
		Playing longer than its length due to the sidehill nature of the landing area and the decidedly uphill shot to the green, a par on the second is a great score.
		The drive zone is guarded left by a long bunker and the second landing area features a kettle hole along its right side.
	www.captainsgolfcourse.com /port.html (842 words)

	Settlements of the Hamburgian and Federmesser Cultures at Slotseng, South Jutland - PalaeoWiki
		Implements should be precisely plotted in already during the reconnaissance phase and the small probes supplemented with excavation of larger holes, of 1 sq.m., for example, in the centre of the concentrations, in order to obtain sufficiently characteristic material for this purpose.
		In connection with these, a kettle hole was found with well-preserved organic material, including reindeer bones and a flint implement about 70 m north-west of the settlement heap (fig.
		The trial trench in the kettle hole with finds of reindeer bones and flint implement (it is possible to give only the approximate position of the latter.
	palaeo.wikidev.net /Settlements_of_the_Hamburgian_and_Federmesser_Cultures_at_Slotseng,_South_Jutland (5146 words)

	Port Jefferson (Site not responding. Last check: 2007-10-07)
		As the kettle hole is beyond the Harbor Hill Moraine the ice chunk had to be ripped from the glacier and itself deposited beyond the moraine.
		As it is just as likely that the kettle hole was formed over an extended period from minor flood events since an ice chunk of this size is capable of existing in the permafrost region just beyond the ice sheet for a great deal of time.
		Fuller, 1914, identified several of the kettle holes in the Port Jefferson region and made the assertion that the outwash fan in question rested on the glacial ice.
	ribart.net (6487 words)

	Regional Landscape (Site not responding. Last check: 2007-10-07)
		BEDROCK GEOLOGY: The Kettle moraine is underlain by Silurian-age dolomite for the northeastern two-thirds of its length and by Ordovician dolomite for the southwestern third, beginning in Waukesha County (Ostrom 1981, Morey et al.
		LANDFORMS: The Kettle moraine is steep ice-disintegration topography, with numerous kettle lakes on steep ridges of fluvial sand and gravel.
		Farther to the north, where strings of kettle lakes and steep moraines created fire barriers, sugar maple-basswood forests were largely unbroken on the landscape, except where conifer swamps occupied small wetlands.
	www.npwrc.usgs.gov /resource/1998/rlandscp/s5-2-4.htm (431 words)

	Glacial Cape Cod, Geologic History of Cape Cod by Robert N. Oldale
		Figure 9 shows the relationship between buried ice and collapse morphology in kettle holes and the ice-contact head of outwash.
		The original kettle hole was far from round, but wave erosion and deposition along the shore have trimmed off headlands and closed off embayments in the shoreline much as they do along the ocean shore.
		Other kettle pond basal sediments are much younger and appear to indicate the time when the rising water table, caused by the rising sea level, first intersected the floor of the kettle hole.
	pubs.usgs.gov /gip/capecod/glacial.html (2790 words)

	In Search of The Bunyip of the Billabong
		A kettle hole is a hollow created when buried blocks of glacier ice melt out.
		Kettle holes are formed by blocks of ice that are separated from the main glacier as the glacier melted back.
		The pond on the left is actually a kettle pond.
	www.chuckstraub.com /Letterboxing/bunyip.htm (806 words)

	Dean Cardasis - Projects - A Kettle Hole Garden
		As viewed from the bedroom balcony, an ancient kettle hole has been modified for contemporary use into a series of three descending garden terraces.
		The kettle hole basin has been transformed into a place where garden and woodland meet.
		The Kettle Hole Garden has received an Honor Award for residential design from the Boston Society of Landscape Architects and has been published in several periodicals and books, including the book, Landscape Architecture by Stephen Moorehead (1997).
	www-unix.oit.umass.edu /~cardasis/content/projects/kettle (255 words)

	Kettle Hole Trail
		The Kettle Hole Trail in Mansfield Hollow Park restored by The Friends of Mansfield Hollow.
		From the water Pump proceed to the yellow gate and follow white and fl kettle hole trail markers on the loop that will return to the picnic grove markers are numbered 1-17 and there are signs at intersections.
		Kettles are one of the many signs of large sheets of ice, called glaciers, which covered New England thousands of years ago.
	www.psychokiwi.org /letterboxing/leaderofthepack/kettle.htm (2391 words)

	Travel: For hiking, biking, try Walden Pond
		Today, Thoreau's Walden Pond is a popular swimming hole about an hour west of Boston, in Concord -- the ultimate destination of Paul Revere's fabled midnight ride.
		Lined with thick oak and pine woods, Walden Pond is a 102-foot-deep "kettle hole," about 2 miles in circumference, fringed with hiking and biking trails.
		Kettle holes were formed by melting glaciers during the last days of the Ice Age, about 12,000 years ago.
	www.sptimes.com /News/090901/news_pf/Travel/For_hiking__biking__t.shtml (763 words)

	The Earliest Settlement of Denmark - PalaeoWiki
		It should be supplemented by the excavation of larger holes at the centre of the concentrations, since this will give a greater chance of recording types of implement that are characteristic of the culture.
		It is informative in this context to mention the situation of a distinct forced passage, a fairly large lake and a kettle hole, and the abundant occurrences of unworked flint on the hillside immediately to the east of the settlements.
		It is hoped that some of these questions will be resolved in conjunction with future investigations, which will involve further studies of the kettle hole and its immediate surroundings and the taking of core samples in the Late Glacial lacustrine deposits further to the north.
	palaeo.wikidev.net /The_Earliest_Settlement_of_Denmark (4839 words)

	Coastal Processes
		Numerous kettle ponds and spring sapping valleys are shown throughout Cape Cod.
		Kame: a knoll or hill underlain by stratified glacial drift that was deposited in a hole in the ice.
		Kettle hole: a topographic depression marking the site of a formerly buried ice block that is usually surrounded by glacial stream deposits.
	www.whoi.edu /science/seagrant/coastalprocesses/poster.html (1206 words)

	WDNR - Kettle Hole Woods State Natural Area
		Description: Located in southeastern Wisconsin's glacial kettle topography is Kettle Hole Woods, an isolated hill forested with southern mesic and dry-mesic hardwoods.
		The mature forest features an excellent canopy of very large trees, primarily red oak and sugar maple with associated beech, basswood, white ash, white oak, and bitternut hickory.
		Kettle Hole Woods is owned by the DNR and was designated a SNA in 1992.
	www.dnr.state.wi.us /org/land/er/sna/sna254.htm (241 words)

	Guide Book: CHAPTER 10 - ASH STREET CONSERVATION LANDS (Site not responding. Last check: 2007-10-07)
		I believe that this pond is a kettle hole pond.
		A kettle hole results when a buried block of glacial ice melts away, leaving a depression.
		The ice block that formed this kettle rested against the bluff which was a southerly shore of glacial Lake Sudbury.
	www.westonforesttrail.org /guides/chapter10.html (1449 words)

	Mastodon mania
		Other materials in the 12,100-year-old burial site -- a geological feature called a kettle hole that was left by melting ice from glaciers -- turned the Cornell-Gilbert Mastodon into a multidisciplinary project.
		There was well preserved wood from 17 species of trees for dendrochronologists, the tree-ring counters, as well as seeds and cones from all kinds of plants for paleobotanists to puzzle over.
		Anaerobic conditions in the kettle hole that became a bog had also preserved parts of muskrats and other mammals.
	www.news.cornell.edu /chronicle/01/2.1.01/mastodon.html (955 words)

	106 Atlantic Street (Site not responding. Last check: 2007-10-07)
		The depression which occupies a large part of Kendall Park in North Quincy is an outstanding example of a feature known as a kettle hole to geologists and glaciologists.
		It is on this symmetry that the Kendall Kettle Hole bases its chief claim to world distinction.
		The Kendall Kettle Hole is located on the former estate of Dr. Walter G. Kendall who deeded Kendall Park to the City of Quincy in 1938.
	ci.quincy.ma.us /tcpl/htm/24.htm (223 words)

	The Watershed V3 N2 P3
		Even the very bottom layer of water in the deepest kettle hole has lost half its salt content: at 6 m it has dropped from about 22 ppt in 1988-1991 to about 15 ppt in 1997.
		In fact, SEA students sampled the deep kettle hole in early October 1998 after a stretch of very windy days and found a salinity of 1.4 ppt from top to the very bottom: the whole pond had gotten turned over, probably for the first time since hurricane Bob in 1991.
		It was found this summer at 4 m even in -the northern kettle hole, where in previous years no trace of it had been detectable.
	www.opet.org /html/wtrshv3n2p3.html (744 words)

	Triangle Lake Bog (Site not responding. Last check: 2007-10-07)
		Triangle Lake Bog is one of the finest and least disturbed sphagnum kettle-hole bogs in Ohio.
		The vegetational zone surrounding this glacial kettle lake follows the classic pattern of boreal bogs.
		A floating sphagnum mat with swamp loosestrife, leatherleaf and tamaracks surrounds the dark acidic waters of the bog lake.
	www.dnr.state.oh.us /dnap/location/triangle.htm (129 words)

	Mmr-2 (Site not responding. Last check: 2007-10-07)
		The 1970 cell, the post-1970 cell, and the Kettle Hole occupy a total of approximately 50 acres.
		The Kettle Hole was used primarily for disposal of demolition and construction debris (e.g., concrete, metal, wood) and was generally left exposed.
		The Kettle Hole disposal area has not been identified as a significant source of VOC contamination.
	www.mmr.org /cleanup/plumes/lf1/pas/mmr-2.htm (3314 words)

	Home Page
		Kettle Hills Golf Course is located just 1.5 miles west of Highway 41/45 on Highway 167 West (Holy Hill Rd.) in Richfield Wisconsin.
		Our snack cabana's located near the 10th tee on each course provide food and drink during prime playing hours and our roving beverage carts are on the course daily with snacks, candy, sandwiches and assorted ice cold beverages for all the golfers.
		With 45 holes of golf to choose from you are sure to find the challenge you are looking for at Zimmermann's Kettle Hills.
	www.kettlehills.com (411 words)

	WDNR - Kettle Moraine North Trails
		The Kettle Moraine State Forest--Northern Unit has more than 132 miles of trails, varying in difficulty, length, and permitted uses.
		New Fane Loop System (PDF, 625KB) On County Line Road, 1.5 miles east of Kettle Moraine Drive, the New Fane Trail is a series of moderately challenging loop trails totaling 5.5 miles.
		Greenbush Kettle - On Kettle Moraine Drive, 1 mile north of State Highway 67.
	www.dnr.state.wi.us /org/land/parks/specific/kmn/trails.html (1424 words)

	Fox State Forest, Ridge Trail
		More than 25 miles of Fox State Forest trails lead to peat bogs, wandering brooks, oak-covered hilltops, cellar holes, and virgin forests that lie within 2 miles of a major state highway and are readily accessible throughout the year.
		The Ridge Trail hike along the perimeter of the forest’s eastern quadrant is a contemplative excursion through a variety of geography and habitat, an adult adventure infused with a sense of expectant wandering.
		Special attractions: The quaking kettle hole of Mud Pond Bog, bear and deer habitat on Jones...
	www.trails.com /tcatalog_trail.asp?AffID=mz01&TrailID=HGN073-022 (147 words)

	Back 9 Hole Layout - Kettle Brook Golf Club
		The lower right fairway is shorter on this dog leg right but the trees and a trap block your 2nd shot to the green.
		Never cut the inside left corner to close or you'll loose a shot down in the woods.
		Cutting across the 10th hole to reach the green is O.B. A long 2nd shot should come in from the right side as everything rolls down the hill from right to left onto the punch bowl green.
	www.kettlebrookgolfclub.com /golf_course/layout_back.htm (424 words)

	[No title]
		It was visited by Samuel de Champlain in 1605, and his detailed descriptions and charts have helped present-day scientists to determine the rate of change of Nauset Beach Spit and Nauset marsh.
		Figure 1 explanation: Index map of Cape Cod and the Islands, Massachusetts The Pilgrims first landed in America on the tip of lower Cape Cod after they were turned back from their more southerly destination by shoals between Cape Cod and Nantucket Island.
		The islands are tied together and to the mainland by spits called 2) tombolos which are composed of sand eroded from the cliffed Cape Cod Bay shore to the north of the harbor.
	www.webroots.org /library/usahist/ma/ghoccma0.html (5555 words)

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