Inman Valley, South Australia | Selwyn Rock, South Australia-an exhumed Glacial striation | glacial pavement of Permian age

* Glacial striation

# REDIRECT Glacial striation

# REDIRECT Glacial striation

# REDIRECT Glacial striation

# REDIRECT Glacial striation

Glacial deposits probably filled the canyon at one time, but have since been eroded away, leaving little or no evidence of their presence.

Their presence caused lakes ( Glacial Lake Tight, Glacial Lake Monongahela, etc.

Glacial erratics such as this boulder are common on Baltic beaches.

Glacial polish, striations and grooves commonly found on erratics of this size have for the most part been effaced by the normal process of decomposition called weathering.

Glacial features along the trail include kettles, potholes, eskers, and glacial erratics.

Glacial erratics such as this boulder are as common on today's Baltic beaches as they were in the past.

Category: Glacial erratics

Glacial transport has deposited large quantities of glacial erratics ( rocks ) in the area.

Category: Glacial erratics

Category: Glacial erratics

Category: Glacial erratics

Category: Glacial erratics

Glacial ice that filled Mill Creek ( whose canyon is mostly post-glacial ), Blue Lake Canyon, Kings Creek Meadows, Flatiron Ridge, Warner Valley and the valley of Manzanita, Hat and Lost Creeks originated from there.

Significant canyon-shaping events occurred as recently as 15, 000 years ago during a massive outburst flood from Glacial Lake Bonneville in Utah.

Glacial meltwater from the Anglian ice sheet, caused the Thames to divert southwards into the valley of the Mole-Wey river, thus adopting its present route through London.

It is believed that a small human population of at most a few thousand survived the Last Glacial Maximum in Beringia, isolated from its ancestor populations in Asia for at least 5, 000 years, before expanding to populate the Americas sometime after 16, 500 years ago, during the Late Glacial Maximum as the American glaciers blocking the way southward melted.

* Lake Chicago, a prehistoric lake from the Wisconsin Glacial Period

Periglacial ( Glacial ) loess is derived from the floodplains of glacial braided rivers that carried large volumes of glacial meltwater and sediments from the annual melting of continental icesheets and mountain icecaps during the summer.

Glacial loess from the Matanuska Glacier blown into Matanuska Valley created the fertile soil conditions that motivated the Matanuska Colony resettlement experiment in Alaska during the Great Depression.

According to e-mails sent from Glacial Pace which responded to fans confused about the large gaps between albums, Modest Mouse is indeed currently writing and recording material and have been for quite some time.

South from Stevens Point, the meltwater would have flowed into Glacial Lake Wisconsin, a prehistoric proglacial lake that existed in the central part of the state.

Ice cores from Sajama in Bolivia span ~ 25 ka and help present a high resolution temporal picture of the Late Glacial Stage and the Holocene climatic optimum .< ref name = Thompson1 >

Ice cores from Huascarán in Peru like those from Sajama span ~ 25 ka and help present a high resolution temporal picture of the Late Glacial Stage and the Holocene climatic optimum.

Glacial Lake Wisconsin was a prehistoric proglacial lake that existed from approximately 18, 000 to 14, 000 years ago, at the end of the last ice age, in the central part of present-day Wisconsin in the United States.

Oneida Lake is a remnant of Glacial Lake Iroquois, a large prehistoric lake formed when glaciers blocked ( from downstream ) the flow of the St. Lawrence River, the outlet of the Great Lakes to the Atlantic Ocean.

A typical scene along the Passaic River which results from the drainage of the Great Swamp National Wildlife Refuge | Great Swamp, a remnant of the Glacial Lake Passaic

The potholes were initially carved out during the Pleistocene by flood waters originating from Glacial Lake Missoula.

Laminated claystone from Glacial Lake Missoula, Montana.

In other cases, such as Glacial Lake Missoula and Glacial Lake Wisconsin in the United States, the sudden rupturing of the supporting dam caused glacial lake outburst floods, the rapid and catastrophic release of dammed water resulting in the formation of gorges and other structures downstream from the former lake.

Image: Glacial Dust off Alaska. jpg | Wind picks up fine sediment from the riverbank and carries it over the ocean.

The peninsula was not deglaciated until 6, 500 years ago ( 11, 500 years after the Last Glacial Maximum ) and is believed to have been the prehistoric centre from which the vast Laurentide Ice Sheet spread over most of North America during the last glacial epoch.

After the glaciers of the Vistula Glacial Stage retreated from Pomerania during the Allerød oscillation, a warming period that falls within the Early Stone Age, they left a tundra.

Most of Manitoba's inhabited south lies in the prehistoric bed of Glacial Lake Agassiz.

The city, both lakes, and the river lie in the Traverse Gap, the bed of ancient, south-flowing Glacial River Warren, the outlet to Glacial Lake Agassiz which, when drained, became the valley of the north-flowing Red River of the North.

** Glacial features: Sandstone buttes that were former islands in Glacial Lake Wisconsin and the former lake bed

Tonawanda Creek flows through the ancient lake bed of Glacial Lake Tonawanda, a prehistoric lake that existed approximately 10, 000 years ago at the end of the last ice age ; many of the swamp lands surrounding Tonawanda Creek also date back to this lake.

The remnants of the Glacial Lake Passaic lake bed are found in several swamps in northern New Jersey, most notably, the Great Swamp that is south of Morristown through Chatham Township, lying in extreme southern Morris County and northeastern Somerset County.

* Glacial Lake Iroquois, a prehistoric lake in the bed of present-day Lake Ontario in North America.

In 1910 Joseph T. Pardee described a great Ice Age lake, " Glacial Lake Missoula ", a glacier dammed lake with water up to deep, in northwest Montana and in 1940 he reported his discovery that giant ripple marks high and 200 – 500 feet apart had formed the lake bed.

Glacial River Warren, in whose bed the Minnesota River now flows, entered the Driftless Area just downriver from present-day Minneapolis-Saint Paul, at Fort Snelling, over River Warren Falls, " an impressive 2700 feet ( 823 m ) across and 175 feet ( 53 m ) tall, over 10 times as wide as Niagara falls " ( this has since receded to become Saint Anthony Falls ).

Plains which were once the bed of Glacial Lake Wisconsin dominate the south central part of the region.

Above Carlton travelers proceeded upstream through quieter stretches to the location of Floodwood, Minnesota, where they turned southwest up the sluggish East Savanna River in the bed of Glacial Lake Upham.