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Type of moraine that forms at the terminal of a glacier
A terminal moraine, also called an end moraine, is a type of moraine that forms at the terminal (edge) of a glacier, marking its maximum advance. At this
Terminal_moraine
Glacially formed accumulation of debris
sometimes called glacial flour. Lateral moraines are those formed at the side of the ice flow, and terminal moraines are those formed at the foot, marking
Moraine
Northern of two ridges along the "backbone" of Long Island, NY, USA
The Harbor Hill Moraine, skirting the North Shore, represents the terminal moraine of the most recent advance of the Wisconsinian glaciation, which reached
Harbor_Hill_Moraine
United States National Natural Landmark in Douglas County, Washington
Douglas County, Washington state, United States. Withrow Moraine is the only Ice Age terminal moraine on the Waterville Plateau section of the Columbia Plateau
Withrow Moraine and Jameson Lake Drumlin Field
Withrow_Moraine_and_Jameson_Lake_Drumlin_Field
Period of major glaciations of the Northern Hemisphere (115,000–11,700 years ago)
terminal moraines that form Long Island, Block Island, Cape Cod, Nomans Land, Martha's Vineyard, Nantucket, Sable Island, and the Oak Ridges Moraine in
Last_Glacial_Period
Landform shaped by erosion and deposition from glacial meltwater
ridges. The shape of a terminal represents the shape of the glacier snout or terminus. Terminal moraine refers to the moraine occurring at the point of
Fluvioglacial_landform
Type of lake formed by glaciation
A moraine-dammed lake, occurs when the terminal moraine has prevented some meltwater from leaving the valley. When a glacier retreats, there is a space
Moraine-dammed_lake
Moraine in the midwestern United States
The Valparaiso Moraine is a recessional moraine (a landform left by receding glaciers) that forms an immense U around the southern Lake Michigan basin
Valparaiso_Moraine
Glaciation in North America during the Last Glacial Period
margin and a terminal moraine is called an outwash plain . The materials left under the glacier when it melts back is called the ground moraine or till plain
Wisconsin_glaciation
preglacial river valleys, while some of it was heaped into belts of hills (terminal moraines) at the margin of the glacier. The chief result of glaciation has
Glacial_history_of_Minnesota
Lake located in Sauk County, Wisconsin
materials and then melted, leaving a terminal moraine blocking the river, forming an earthen dam. Another moraine was deposited at the north end of the
Devil's_Lake_(Wisconsin)
Time period c. 12,900–11,700 years ago
Superior and southeast Quebec, leaving behind a layer of rock debris (moraine) dated to this period. Southeastern Alaska appears to have escaped glaciation;
Younger_Dryas
Geological region in the Midwestern US
Cross Plains State Park. In addition, the Ice Age Trail follows the terminal moraine of the maximum glacial extent from the last ice age and enters the
Driftless_Area
Highest point on Long Island
(122.2 m) above sea level. It is situated on the Harbor Hill moraine, a terminal moraine that makes up the northern spine of Long Island, in West Hills
Jayne's_Hill
Piece of rock that has been moved by a glacier
in rows, trains or clusters along the lateral moraines as opposed to being located on the terminal moraine or in the general glacial field. Erratics provide
Glacial_erratic
Long-distance hiking trail in the United States
location of the terminal moraine from the last Ice Age. As the route traverses the moraine, it sometimes meanders into areas west of the moraine, including
Ice_Age_Trail
Plain formed from glacier sediment transported by meltwater
over the outwash plain, with larger boulders being deposited near the terminal moraine, and smaller particles travelling further before being deposited. Sandurs
Outwash_plain
Historical region in Germany and Poland
Geierswalder See to Sedlitzer See (Sedlišćański jazor) The Muskau Morainic Arch is a terminal moraine formed during the Elster glaciation, which together with
Lusatia
Archipelagic region off the southern coast of New England in the United States
The Outer Lands is the prominent terminal moraine archipelagic region off the southern coast of New England in the United States. This eight-county region
Outer_Lands
Moraine in the midwestern United States
wider terminal moraine called the Valparaiso Moraine, which is located farther from the lake than the Tinley Moraine. Compared to the Valparaiso Moraine, the
Tinley_Moraine
Glacier in Alaska, US, and Yukon, Canada
Bert Point. It pushed a terminal moraine ahead of its face and closed the opening again in July. On August 14, the terminal moraine was washed away after
Hubbard_Glacier
Lake formed by the action of ice
a proglacial lake is a lake formed either by the damming action of a moraine during the retreat of a melting glacier, a glacial ice dam, or by meltwater
Proglacial_lake
State Park in Sauk County, Wisconsin
(150 ha) Devil's Lake, which was created by a glacier depositing terminal moraines that plugged the north and south ends of the gap in the bluffs during
Devil's Lake State Park (Wisconsin)
Devil's_Lake_State_Park_(Wisconsin)
Environmental Biome in Central Europe
and complete glacial series are: a ground moraine with a tongue-like basin, the Zungenbecken a terminal moraine chain that lies in an arc around the Zungenbecken
Glacial_series
Fjord in South Georgia
Moraine Fjord is an inlet 3.5 nautical miles (6 km; 4 mi) long with a reef (a terminal moraine) extending across its entrance, forming the west head of
Moraine_Fjord
Glacial till landform above Lake Ontario, Canada
Oak Ridges Moraine is an ecologically important geological landform in the Mixedwood Plains of south-central Ontario, Canada. The moraine covers a geographic
Oak_Ridges_Moraine
Geographic and geologic area of North America
Depositional Drumlin Erratic block Moraine Pulju moraine Rogen moraine Terminal moraine Till plain Veiki moraine Glacifluvial Diluvium Esker Giant current
Canadian_Shield
Species of reptile
the copperhead has mostly not re-established itself north of the terminal moraine after the last glacial period (the Wisconsin glaciation), though it
Eastern_copperhead
River in the United States
advanced rapidly, leaving a terminal moraine parallel to the modern Sangamon River. The ice stagnated and melted behind this moraine, without the meltwater
Sangamon_River
Depression formed by glaciers or floodwaters
fauna. The Kettle Moraine, a region of Wisconsin covering an area from Green Bay to south-central Wisconsin, has numerous kettles, moraines and other glacial
Kettle_(landform)
Type of outburst flood that occurs when the dam containing a glacial lake fails
glacier, is called a jökulhlaup. The dam can consist of glacier ice or a terminal moraine. Failure can happen due to erosion, a buildup of water pressure, an
Glacial_lake_outburst_flood
Long, narrow inlet with steep sides or cliffs, created by glacial activity
their mouth caused by the previous glacier's reduced erosion rate and terminal moraine. In many cases this sill causes extreme currents and large saltwater
Fjord
Moraine in Long Island, New York, U.S.
Moraine, in the geography of Long Island, forms the southern of two ridges along Long Island's "backbone." The Ronkonkoma Moraine, a terminal moraine
Ronkonkoma_Moraine
Large lake in central North America at the end of the last glacial period
postulates that the lake was a 'terminal lake' with water inflows and evapotranspiration being equal. Dating of the glacial moraines shows that the Clearwater
Lake_Agassiz
Continental glacier in North America during the last ice age
the northern United States, leaving behind glacially scoured valleys, moraines, eskers and glacial till. It also caused many changes to the shape, size
Laurentide_ice_sheet
Period of long-term reduction in temperature of Earth's surface and atmosphere
Esmark discovered the similarity between moraines near Haukalivatnet lake near sea level in Rogaland and moraines at branches of Jostedalsbreen. Esmark's
Ice_age
Terminal moraine at Lake Michigan
The Marseilles moraine is a terminal moraine that encircles the southern tip of Lake Michigan in North America. It begins near Elgin, Illinois, and extends
Marseilles_moraine
Region of Ohio
closely to the terminal moraine of an ancient glacier that runs southwest to northeast through the state. Areas south and east of the moraine are characterized
Appalachian_Ohio
Climatic cooling after the Medieval Warm Period (16th–19th centuries)
in Europe during the Little Ice Age because of the characteristics of moraines. However, applications of Quaternary dating methods such as surface exposure
Little_Ice_Age
Largest terminal moraine in Scandinavia
Raet is the largest terminal moraine in Scandinavia. It was formed during the end of the last glacial period, 12,800–11,500 years ago, in one of the latest
Raet
Nature reserve in Västra Götaland, Sweden
is a terminal moraine and is part of what is known as the central Swedish terminal moraine zone. The latter is in turn part of a series of terminal moraines
Hindens_Rev
Mound formed on a retreating glacier and deposited on land
Provincial Park. Drumlin Esker Glacial Kame culture Glacial landforms Moraine Outwash fan "Knob And Kettle | Encyclopedia.com". "kame". Oxford English
Kame
Rise of land masses after glacial period
locked up at glacial maximum. Secondly, the location and dates of terminal moraines tell us the areal extent and retreat of past ice sheets. Physics of
Post-glacial_rebound
Long, winding ridge of stratified sand and gravel associated with former glaciers
blocks, or in narrow embayments at glacier margins. Eskers form near the terminal zone of glaciers, where the ice is not moving as fast and is relatively
Esker
Lake in Teton County, Wyoming, United States
which carved Cascade Canyon during the last glacial maximum, forming a terminal moraine which now impounds the lake. The lake is estimated to be 256 feet (78 m)
Jenny_Lake
Warmer periods within an ice age
Depositional Drumlin Erratic block Moraine Pulju moraine Rogen moraine Terminal moraine Till plain Veiki moraine Glacifluvial Diluvium Esker Giant current
Interglacial
Lake in California, United States of America
southern, granitic part of the lakeshore (the cirque face). There is a terminal moraine of boulders and gravel forming a natural dam opposite the cirque face
Castle_Lake_(California)
Glacial erratic in Alberta, Canada
Depositional Drumlin Erratic block Moraine Pulju moraine Rogen moraine Terminal moraine Till plain Veiki moraine Glacifluvial Diluvium Esker Giant current
Okotoks_Erratic
Peninsula in Massachusetts, United States
rest of Massachusetts. The bulk of the land in the area is glacial terminal moraine and represents the southernmost extent of glacial coverage in southeast
Cape_Cod
Group of lakes in New York, United States
valleys to form subglacial tunnel valleys. Glacial debris, possibly terminal moraine left behind by the receding ice, acted as dams, allowing lakes to form
Finger_Lakes
River in Schleswig-Holstein, Germany
is only a few kilometers from the Baltic Sea –at Lake Schulensee– a terminal moraine –the Hornheimer Riegel– blocks its path, and the Eider from then on
Eider_(river)
Lake in Montana, United States
last ice age and thus is the site of the glacier's terminal moraine. The large size of the Polson Moraine indicates that the glacier stalled here for many
Flathead_Lake
Fjord in Norway
Depositional Drumlin Erratic block Moraine Pulju moraine Rogen moraine Terminal moraine Till plain Veiki moraine Glacifluvial Diluvium Esker Giant current
Hardangerfjord
Landform in Lower Saxony, Germany
age. The landscape consists of flat plains of ground moraines, ridges of hilly terminal moraines and also of sandar - glacial outwash plains deposited
Lüneburg_Heath
Tidal estuary on the U.S. East Coast
Connecticut coast into the sound, creating what is now Long Island (the terminal moraine). When the ice sheet stopped advancing 18,000 years ago (as addition
Long_Island_Sound
Region of hills in Wales and England
Hereford, leaving an arcuate terminal moraine in place. During its subsequent retreat the glacier left recessional moraines at Stretton Sugwas, Staunton
Black Mountains, United Kingdom
Black_Mountains,_United_Kingdom
Dutch national park
and woodlands. It is situated in the Veluwe, the area of the largest terminal moraine in the Netherlands. Most of the landscape of the park and the Veluwe
De_Hoge_Veluwe_National_Park
Major ice sheet
Depositional Drumlin Erratic block Moraine Pulju moraine Rogen moraine Terminal moraine Till plain Veiki moraine Glacifluvial Diluvium Esker Giant current
Cordilleran_ice_sheet
Village in Wales
Works) nearby. The bowling green survived. A rare example of a glacial terminal moraine in the south of the village is one of over a thousand sites in Wales
Glais
Post glacial seaway in eastern North America
Depositional Drumlin Erratic block Moraine Pulju moraine Rogen moraine Terminal moraine Till plain Veiki moraine Glacifluvial Diluvium Esker Giant current
Champlain_Sea
Largest natural lake in Colorado, United States
glaciation, which occurred from 30000 BC to 10000 BC. The glacial terminal moraine created a natural dam. Natural tributaries to the lake are the North
Grand_Lake_(Colorado)
County in northwestern New Jersey, United States
Allamuchy Mountains to the terminal moraine near Hackettstown. The Kittatinny Valley is situated north of the terminal moraine; it runs north of Belvidere
Warren_County,_New_Jersey
Neighborhood in New York City
Briarwood (at Parsons Boulevard to the west). It is centered on the terminal moraine that runs the length of Long Island. Originally populated with people
Jamaica_Hills,_Queens
Unincorporated community in Washington, US
Withrow Moraine is the only Ice Age terminal moraine on the Waterville Plateau section of the Columbia Plateau. It lies on the terminal moraine for the
Withrow,_Washington
Highest natural point in Brooklyn, New York
of the Heights of Guan. The hill is part of the Harbor Hill Moraine, a terminal moraine formed during the last glacial period. Among the other graves
Battle_Hill_(Brooklyn)
Canyon in the Waterville plateau region of Douglas County, Washington
Withrow Moraine and Jameson Lake Drumlin Field "contains the best examples of drumlins and the most illustrative segment of the only Pleistocene terminal moraine
Moses_Coulee
Unsorted glacial sediment
glacier. It is deposited some distance down-ice to form terminal, lateral, medial and ground moraines. Till is classified into primary deposits, laid down
Till
Prehistoric glacial lake in New England
runoff in the reemerging Connecticut River Valley was dammed by the terminal moraine, creating a long, narrow lake and trapping glacial sediment. The lake
Lake_Hitchcock
for this. Much of Staten Island is covered by the Harbor Hill moraine, the terminal moraine of the last Wisconsin Stage glacier. However, ledges of bedrock
Staten_Island_Serpentinite
A push moraine or pushed moraine is in geomorphology a moraine (a landform formed by glacial processes) that forms when the terminus advance of a lowland
Push_moraine
Circa 24,000–16,000 BCE; most recent era when ice sheets were at their greatest extent
Archipelago, glacier advance peaked 26,000 years ago, forming a long north–south moraine system along the eastern coast of Chiloé Island (41.5–43° S). By that time
Last_Glacial_Maximum
Island in the town and former whaling port of Nantucket, Massachusetts
originally formed by the terminal moraine of the last glacial episode (Wisconsin glaciation). It still retains remnants of the moraine as low hills, but the
Tuckernuck_Island
Hill near York, North Yorkshire, England
Siwards How and also known as Heslington Hill or Bunny Hill, is a terminal moraine located to the south-east of the city of York. The howe is situated
Siward's_Howe
Forest region in Brandenburg, Germany
the Schorfheide heathland. Ruppin Switzerland lies in a wide belt of terminal moraine and runs from Neuruppin in the south to the village of Binenwalde in
Ruppin_Switzerland
First epoch of the Quaternary Period
Depositional Drumlin Erratic block Moraine Pulju moraine Rogen moraine Terminal moraine Till plain Veiki moraine Glacifluvial Diluvium Esker Giant current
Pleistocene
Prehistoric lake from the Wisconsin Glacial Period
edge of the retreating glacier formed moraines, the Park Moraine in present-day Illinois and the Lake Borders Moraine in Indiana and Michigan. The ice continued
Lake_Chicago
Sandbank in the North Sea
the European Union as a Natura 2000 site. The bank originated as a terminal moraine of a glacier during one of the Ice Ages. The surface of the bank partly
Cleaver_Bank
Glacier in Alberta, Canada
has been further retreat which has left a newly formed lake at the terminal moraine at the glacial snout. Sedimentation has also increased in Bow Lake
Bow_Glacier
Estuary in Staten Island, New York
headwaters near Historic Richmond Town, on the southern end of the terminal moraine of the island. The system of streams provides recreational kayaking
Fresh_Kills
National park in Alberta, Canada
has been further retreat which has left a newly formed lake at the terminal moraine. Peyto Glacier has lost 70 percent of its volume since record keeping
Banff_National_Park
Lake in Canterbury Region, New Zealand
three lakes were formed when the terminal moraines of receding glaciers blocked their respective valleys, forming moraine-dammed lakes. The Alps2Ocean mountain
Lake_Pukaki
Hills in Alberta and Saskatchewan, Canada
the ice sheet paused periodically during its final retreat, a series of morainal ridges of glacial till built up around the hills. Rivers of meltwater cut
Cypress_Hills_(Canada)
Interglacial period which began 130,000 years ago
parastratotype was selected in the Amsterdam glacial basin in the Amsterdam-Terminal borehole and was the subject of a multidisciplinary investigation (Van
Last_Interglacial
English poet, journalist and literary critic (born 1949)
at the Vanity Fair Hitchens memorial service. His first collection, Terminal Moraine (1972) won a Gregory Award. With the proceeds he traveled to East Asia
James_Fenton
Type of moraine
A Veiki moraine (Swedish: Veikimorän) is a type of moraine found in northern Sweden, Finnmark in Norway, and parts of Canada. This moraine is characterized
Veiki_moraine
British actor (1919–2016)
Leprechaun, Donald "The Leprechaun Who Didn't Listen" "The Lion Tamer" "My Terminal Moraine" 1950 The Jack Benny Program Himself 1952 Hollywood Star Playhouse
Alan_Young
Massif in Switzerland and Italy
Depositional Drumlin Erratic block Moraine Pulju moraine Rogen moraine Terminal moraine Till plain Veiki moraine Glacifluvial Diluvium Esker Giant current
Monte_Rosa
Lake in the state of California, United States
Lake would be a bay of Lake Tahoe, similar to nearby Emerald Bay. A terminal moraine is visible at the north end of the lake on the northeast edge. Fallen
Fallen_Leaf_Lake
Abrupt climatic cooling event during the last glacial retreat
glaciers abruptly advanced into montane valleys and deposited moraines near the moraines formed during the Last Glacial Maximum. These glaciers then began
Oldest_Dryas
Former lake in North America
Depositional Drumlin Erratic block Moraine Pulju moraine Rogen moraine Terminal moraine Till plain Veiki moraine Glacifluvial Diluvium Esker Giant current
Lake_Algonquin
Lake in Wyoming, USA
River Range, in a glacially formed basin with the outlet blocked by a terminal moraine. The lake is notable for being very deep at 185 m (607 ft) feet in
Fremont_Lake
Sound, this natural waterway occupies a valley blocked by a large terminal moraine left by the retreat of a glacier during the last glacial period. In
Seno_Skyring
Municipality in Saxony-Anhalt, Germany
("collective municipality") Elbe-Havel-Land. The village is situated on a terminal moraine, stretching along the eastern bank of the Elbe River. It is located
Schönhausen
Hamlet and census-designated place in New York, United States
scrub oak and pine barrens south of the southern slope of Half Hollow terminal moraine was named Wyandanch in 1903 by the Long Island Rail Road (LIRR) to
Wyandanch,_New_York
left a terminal moraine where the glacier halted, and a ground moraine in other areas once covered by the continental glacier. The terminal moraine, known
North_Shore_Highlands
Glacial age that occurred before the Last Glacial Period
Depositional Drumlin Erratic block Moraine Pulju moraine Rogen moraine Terminal moraine Till plain Veiki moraine Glacifluvial Diluvium Esker Giant current
Penultimate_Glacial_Period
Lake in Los Lagos Region, Chile
glacial period is called Llanquihue glaciation in Chile after the terminal moraine systems around the lake. Some historians consider Llanquihue Lake to
Llanquihue_Lake
River in Germany and between Germany and Switzerland
East is the Old Rhine Bridge in Constance, near the bottleneck of the terminal moraine (see below). The current bridge was constructed in 1957, but precursors
Seerhein
Sound in Washington, United States
Inlet and the Central Basin. Puget Sound's sills, a kind of submarine terminal moraine, separate the basins from one another, and Puget Sound from the Strait
Puget_Sound
erratics and haystack rocks that occur near and on the Withrow Moraine, which is the terminal moraine of the Okanogan ice lobe. Boulder Park is located on the
Boulder_Park
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