Geomorphology is the Study of Landforms. Usually by Erosion, Transportation and Deposition
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1 Geomorphology is the Study of Landforms and the Processes that t Create Them, Usually by Erosion, Transportation and Deposition Fluvial = running water, rivers and floodplains Glacial = flowing ice in cold environments, moraine Aeolian = wind, usually in deserts, sand dunes Shoreline = wave action, beach and cliff Lacustrine = lakes are temporary features, peat bog
2 Rivers Flood in a Perfectly Natural Process. Its Just Inconvenient for People
3 TheySpend Billions $$$ Trying to Control Rivers
4 The River Floods the Floodplain, the Flat Area on Either Side of theriver So, people build levees to protect the floodplain
5 In Spite of All the Money Spent, They Still Flood When the Big One Happens.
6 The Colorado River is One of the Most Manipulated Rivers on Earth, Pi Primarily il for Water Supply for Growing Cities and Agricultural Interests ofthe Southwest.
7 Aeolian Processes Occur Primarily in Deserts
8 The Classic Image of a Desert is a Sea of Sand called an Erg as in this Part of the Sahara. On the Left is a Rock Desert called a Reg.
9 Winds Can Move Tons of Sand Each Day
10 The Exact Form of the Sand Dune Is Determined by Type/Amount of Sand and Type of Prevailing Winds. Transverse where winds prevail from one direction i only Parabolic where sand is anchored by vegetation
11 The Star Dune Forms Where the Direction of the Winds Change with theseasons Seasons. It Can Look Like a Starfish on an Air Photo
12 Sand Dunes Have Been Compared to Ocean Waves. Both are Formed by Wind But the Processes are Very Different
13 Action of Waves Along a Shoreline Can Erode Rock Making a Cliff and Deposit Sand Making a Beach
14 Coastal Landforms Are Usually Due to a Combination i of Local ltopography and Wave Action
15
16 Two Types of Glaciers Continental Glaciers Can Cover Thousands of Square Miles of Land to Depths of Thousands of Feet. The Antarctic Glacier and the Former North American Glacier Are Examples. The Alpine Glacier is Smaller and Creates the Spectacular Landforms of Some Mountains. Each Creates Their Own Characteristic Set of Landforms
17 18 Thousand Years Ago, This Glacier Covered 1/3 of the Continent. Some Depths of Ice Were 2 Miles Thick, Comparable to Antarctica Today
18 In the U.S., the Glacier Pushed South to the Ohio River and then Melted, Retreating Northward Leaving Glaciofluvial Landforms Including the Great Lakes
19 Glacialofluvial landforms Are Still Evident on the Landscape of the Mid west.
20 An Alpine Landscape Formed By Water Has a Rounded, d Smooth happearance
21 Alpine Landscapes formed by Glaciers Has a Sharp Jagged, CraggyAppearance
22 The Horn is a Classic Feature of Alpine Glaciers
23 Alpine Glaciers Flow Slowly Down Valleys Until They Melt. They Erode and Transport Tremendous Amounts of Rock and Soilcalled Till. Often Till Is Deposited at the End of the Glacier as a Terminal Moraine. These Can Be Hundreds of Feet Tall.
24 Moraines Are Deposits of Rock and Mud Scraped Up and Moved dby a Glacier.
25 Alpine Landscapes Modified by Glacial Action Are Instantly Recognizable. The Horn, U Shaped Valley and Hanging Valley All Examples.
26 The U Shaped Valley with Flat Bottom and Steep Side Walls is a Classic Feature of Alpine Glaciers
27 Yosemite National Park Is Famous for Its Spectacular Glacial l Landforms. The Valley Was Filled with Ice as High as the Cliff
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