Minnesota: action of ice sheets (glaciation) Flashcards

(16 cards)

1
Q

location

A

state in the upper midwestern region of the US
bordered by canadian Manitoba and Ontario

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2
Q

landscape shaped by

A

the Laurentide Ice Sheet
advancing and retreating numerous times in the quaternary

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3
Q

geology

A

-oldest rocks lie in alternating belts of volcanic and sedimentary rocks
-tectonic compression created a range of mountains several km high in N Minnesota

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4
Q

lobes

A

-around 75000 years ago a series of lobes or tongues of ice extended from the main laurentide ice sheet and spread across minesota
-advanced and retreated a number of times transporting and depositing till
-over 1km thick in some places

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5
Q

last glacial maximum

A

-ice sheet covered 13 million km^2
-lasted over 800000 years and eroded extensivly
-ice radiated outward from two high points
-changes in climate and precipitation caused these domes to shift periodically changing the direction of ice flow

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6
Q

glacial landforms: ellipsoidal basin

A

the ice eroded high mountains so a large ellipsoidal basin was created and is now studded with thousands of lakes such as Upper and Lower Red lakes

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7
Q

glacial landforms:striations

A

the lobes of ice abraded striations in the bare rock outcrops

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8
Q

glacial landforms:moraines

A

-Wadena alone advance from NE canada and the till deposited by this is red & sandy from being derived from red sandstone & shales
-it deposited the Alexandria moraine forming the drumlin fields spanning Ottertail, Wadena and Todd counties
-formed the Itasca Morraine

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9
Q

glacial landforms:end morraine

A

Prairie Coteau

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10
Q

glacial landforms:periglacial lakes

A

-the edge of the giant ice sheet damned the natural drainage of the area creating a number of periglacial lakes
-eg Lake Agassiz-300000 sq km

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11
Q

glacial landforms:knocks and lochans

A

the areal scouring associated with this ice sheet resulted in thousands of low lying knocks and intervening lochans

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12
Q

glacial landforms:River Warren

A

water from the glacial Lake Agassiz drained southward from this lake in glacial River Warren
this raging river created the large valley in which the Minnesota river now flows

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13
Q

change over time:sediments

A

-sediments during this time that were deposited mask nearly all of minnesotas previous geological history

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14
Q

change over time:mountains

A

-the high mountains were eroded down so they are now 500-700 m

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15
Q

change over time:lakes

A

-when the Lake Agassiz finally drained it left behind fertile silt deposits producing the rich farmland of the Red River Valley
-as the ice retreated for the last time the variable topography left behind resulted in numerous lows that filled with water becoming the “1000” lakes seen today

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16
Q

change over time:by 1000 years ago

A

by 1000 years ago it was mostly ice free however the Rainy Lobe and the St. louis sun lobe were still present