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Published byLaurel O’Brien’ Modified over 9 years ago
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Continental Glaciers (Ice Sheets) and Illinois Glaciation
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Phanerozoic – EON Cenozoic – ERA Quaternary – PERIOD Pleistocene - EPOCH (1.8 mya - 10,000 years ago)
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2. Ice sheets (Continental glacier) Large scale – cover 10% of Earth’s land Greenland – 1.7 million km 2 Antartica – 13.9 million km 2 Glacier Types
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Continental Glaciers
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Glaciation in Illinois 1.Wisconsinan 75,000 – 10,000 ya 2.Illinoian 300,000 – 125,000 ya 3.Kansan 700,000 – 500,000 ya 4.Nebraskan 1,800,000 – 900,000 ya
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Glaciation in Illinois 1.Wisconsinan 75,000 – 10,000 ya 2.Illinoian 300,000 – 125,000 ya 3.Pre-Illinoian
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End moraines and till plains
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Glacial Deposits Drift – Sediment deposited on land or in water as a result of glaciation. Till – Unsorted debris transported by glaciers and deposited on land. Diamicton – Does not infer digenesis
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Moraine – a sediment pile composed of till deposited by a glacier Glacial Deposits
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Till – Mixture of unsorted mud, sand, pebbles, and larger rocks deposited by glaciers
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Ice Sheet Landforms Outwash – sand and gravels deposited by glacial meltwater
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Pro-Glacial Lake Sediments
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Ice Sheet Landforms – Kettle Lakes
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Ice Sheet Landforms - Eskers
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Ice Sheet Landforms - Drumlins
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Ice Sheet Landforms Drumlins
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Glaciation relocated rivers
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Pre-Illinoian Drainage
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Illinoian Glaciation & Drainage
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Wisconsinan Glaciation & Drainage
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Lobes And Moranic systems
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Chief Waupansee
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Was this change unique in time? Why did the climate change? Points to Ponder
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1. changing continental positions 2. uplift of continental blocks 3. reduction of CO2 in the atmosphere 4. changes in the Earth's orbit Why did the climate change?
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Plate Tectonics is one of the keys to paleozoic glaciation 250 million years ago
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Changes in Earth’s Orbit The Milankovitch Theory
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Eccentricity of the orbit
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Changes in Earth’s tilt The Milankovitch Theory
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Earth-Sun Relations
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Precession of the Equinoxes The Milankovitch Theory
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Cycles of Global Warming
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Snowball Earth
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