Minnesota: action of ice sheets (glaciation) Flashcards
(16 cards)
location
state in the upper midwestern region of the US
bordered by canadian Manitoba and Ontario
landscape shaped by
the Laurentide Ice Sheet
advancing and retreating numerous times in the quaternary
geology
-oldest rocks lie in alternating belts of volcanic and sedimentary rocks
-tectonic compression created a range of mountains several km high in N Minnesota
lobes
-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
last glacial maximum
-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
glacial landforms: ellipsoidal basin
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
glacial landforms:striations
the lobes of ice abraded striations in the bare rock outcrops
glacial landforms:moraines
-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
glacial landforms:end morraine
Prairie Coteau
glacial landforms:periglacial lakes
-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
glacial landforms:knocks and lochans
the areal scouring associated with this ice sheet resulted in thousands of low lying knocks and intervening lochans
glacial landforms:River Warren
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
change over time:sediments
-sediments during this time that were deposited mask nearly all of minnesotas previous geological history
change over time:mountains
-the high mountains were eroded down so they are now 500-700 m
change over time:lakes
-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
change over time:by 1000 years ago
by 1000 years ago it was mostly ice free however the Rainy Lobe and the St. louis sun lobe were still present