Your Tour Guide… Welcome! I’ll be your tour guide on your virtual trip through the beautiful, and once glaciated, state of Michigan. Enjoy your trip and.

Slides:



Advertisements
Similar presentations
Glaciers Chapter 8, Section 2.
Advertisements

Wisconsin: Physical History. Wisconsin Ice Age 110,000 to 12,000 years ago Most recent advance of North American Laurentide ice sheet Several miles thick.
GLACIAL LANDFORMS SHAPE MOUNTAINS
Chapter 13: Glacial Processes, Patterns and Associated Landforms
Glaciation of Canada.
Erosion: Deposition: AIM: Erosional and Depositional systems
Glacial Landforms. Continental Glaciers Striations Erosion of soil.
Form in high mountains where snow accumulates to sufficient depths so that it is compressed, compacted and recrystallized. For this reason glacial.
Landforms Resulting from Fluvio Glacial Deposition What happens when the glacier melts?
What is a Glacier? REVIEW = An accumulation of compacted snow & ice
Glaciers and Glacial Landforms
 As glaciers travel over land, glacial ice can erode the underlying bedrock.  This erosion can happen by:  Plucking  Abrasion.
Chapter 7: Erosion and Deposition
Surface Processes weathering, mass wasting, erosion, deposition.
CHAPTER 5 HONORS EARTH SCIENCE
CHAPTER 5 HONORS EARTH SCIENCE
Glaciers. A GLACIER forms when yearly snowfall in a region far exceeds the amount of snow and ice that melts during the summer months. Most of the world's.
Glacial landforms in Michigan: A Roscommon Prospective.
GLACIERS CHAPTER 5 HONORS EARTH SCIENCE. What is a glacier? a thick mass of moving ice
‘S‘S. VOCABULARY GLACIER - LARGE MOVING MASS OF ICE THAT FORMS NEAR EARTH’S POLES AND IN MOUNTAINOUS REGIONS AT HIGH ELEVATIONS. GLACIER - LARGE MOVING.
Aim: What are Glaciers? I. Glacier – found at high altitudes and high latitudes. These are locations where more snow falls during the winter than melts.
Erosion by Glaciers. Index Types of Glaciers Features Deposition Formation of Long Island.
Glaciers.
Glaciers and Erosion Glacier = Large moving mass of ice and snowmovingice Alpine vs. Continental Glaciers.
Unit 1: Land and Water Forms Glaciers as Agents of Erosion
What is erosion? -Erosion is the removal of rock particles and soil from an area -Erosion requires energy (usually supplied by gravity)
Ch 15: p  Enormous masses of moving ice created by the accumulation and compaction of snow.  Powerful agents of erosion ~ have carved some.
Glaciers Glaciers formed much of the landscape that exists presently in the northern United States and elsewhere in the world. Glaciers Today, scientists.
Glaciers We wouldn’t be here without them.. A Glacier is an accumulation of snow that is large enough to survive the summer melt. These large ice masses.
Glacial Erosion and Deposition. Erosion Glaciers have the capacity to carry huge rocks and piles of debris over large distances They grind out parallel.
How do Glaciers Effect the Land? By erosion & deposition.
Geologic Features of Glaciation
Glacial Landscapes Glacier = large moving mass of ice. Glacier = large moving mass of ice. Glaciers erode, transport and deposit massive amount of sediment.
3.3 Erosion and Deposition of Ice Done By: Laura, Elizabeth, Erin, and Gabby.
Glaciers. Geologists define a glacier as any large mass of ice that moves slowly over land. There are two types of glaciers: Continental glaciers Valley.
LITHOSPHERE LANDSCAPE FEATURES RESULTING FROM GLACIAL AND FLUVIOGLACIAL ACTION Glacial Action by iceFluvioglacial Action by Meltwater Erosion Deposition.
AIM: How do Glaciers change the landscape? Do Now:
Continental Claciation
LITHOSPHERE GLACIATION 1 Lesley Monk Balfron High School Session 2005/6.
How The Last Ice Age Shaped Canada
Glaciers We wouldn’t be here without them.. A Glacier is an accumulation of snow that is large enough to survive the summer melt. What are glaciers?
Glaciers Explain how glaciers move.
Chapter 8 Erosional Forces Section 8-2 Glaciers Note Guide.
Erosion & Deposition Notes…Part 2…Glaciers! M. Manzo
Study Guide Chapter What is a glacier? 2.Distinguish between alpine and continental glaciation. 3.Explain how a glacier moves. Explain how a crevass.
CGC 1D1 Mr. Zapfe.  Final changes occurred which gave Canada’s landforms their present shape  Continuing collision of North American and Pacific Plates.
Glacial Landforms. Continental Glaciers Striations Erosion of soil.
LITHOSPHERE GLACIATION 1 Materials carried by the glaciers are deposited in two main ways;  Glacial Deposits (unsorted) and  Fluvio-glacial deposits.
D. Evan Stribling  a larger mass of compacted snow and ice that moves under the force of its own gravity (weight)  They erode in some places deposit.
Glaciers once covered most of the Earth –in total there have been up to 22 times when glaciers covered large areas of the Earth… including Alberta the.
Chapter 7.1b Glaciers.
What happens to the eroded debris? Glaciers pick up and transport a huge load of debris as they slowly advance across the land. Ultimately, these materials.
Alaska from space.
Glacier Review.
AIM: How do Glaciers change the landscape? Do Now:
Like running water, gravity is the driving force
LANDFORMS OF GLACIAL DEPOSITION
III. Deposition-the process by which sediments
Erosion and Depistion BY GLACIERS!.
How Glaciers Modify the Landscape
Title: Glacial Erosion and Deposition Page: 82 Date: 3/5/2013
Glaciation – Extent in North America 10,000 Years Ago
Glacier Terms.
Glaciation of Canada.
Deposits by Glaciers material carried by glaciers is deposited by melting deposits of glacial origin are called drift. 2 kinds of drift: Till and outwash.
Deposits by Glaciers Most of the material carried by glaciers is deposited by melting, called drift. 2 kinds of drift: Till is left under or along the.
Erosion and Depistion BY GLACIERS!.
Earth Science Chapter 8 Section 3
A Virtual Tour Focusing on Glacial Features in Michigan
Fjords: Glacial valleys/ troughs filled with ocean water
Presentation transcript:

Your Tour Guide… Welcome! I’ll be your tour guide on your virtual trip through the beautiful, and once glaciated, state of Michigan. Enjoy your trip and don’t forget to fill out your journal (aka worksheet) ! Next

The Last Ice Age… Next Nearly 1.5 million years ago an ice age helped create glaciers that covered our state. Our Great Lakes didn’t even exist at that point! In fact, they were likely just rivers. Back The glaciers that shaped Michigan went as far south as the Ohio River valley. These glaciers left Michigan just over 10,000 years ago (that is a relatively short time in the scheme of history).

Features left by Glaciers Next There are lots of features left behind by glaciers, including: Back Moraines Outwash Plains Till Kettles Erratics Eskers Drumlins Striations Kames Great Lakes

Moraines Next There are lots of features left behind by glaciers. Moraines are features that can be found all over Michigan. They formed at the melting edges and front of the glacier. Moraines are ridges of till and basically look like hills. Back Notice the moraines in Montcalm County. Can you picture where these are?

Moraines Next Although moraines can be found all over the state, not all moraines are equal. One of the more popular moraines is Boyne Mountain, a ski resort near Petoskey. An outwash plain occurs at the base of the moraine. Back Boyne Mountain, Michigan

Outwash Plains Next There are many outwash plains in Michigan. They are flat plains in front of moraines formed by deposits left behind by the glacial meltwater. They make excellent farm fields because of these fertile deposits. Back Battle Creek, Michigan

Till Next Unsorted mixtures of clay, silt, sand, gravel, and boulders are known as till. Till is a common deposit left all over the state by glaciers. For instance, moraines are composed of till. Back

Kettles Next Kettles are depressions left behind after partially-buried ice blocks melt. Many are filled with water, and are called kettle lakes. Many of our small, deep lakes in Michigan are kettle lakes. For instance, our own Baldwin Lake is a kettle. Back Greenville, Michigan

Erratics Next Erratics are boulders that are usually found near moraines. They were transported by ice, streams are not powerful enough to move the boulders. Erratics are commonly found in fields. At right is an erratic from the Keweenaw Peninsula. Back Keweenaw Peninsula, Michigan

Eskers Next Eskers were formed from rivers inside a glacier. The water of the river deposited materials along the river path when the mouth of the river became clogged. The most famous esker in Michigan is the Mason Esker, near Mason, Michigan. Back Mason, Michigan

Drumlins Next There are limited numbers of drumlin fields in Michigan. However, a prominent one is located near Traverse City. These teardrop shaped landforms are made of till and signal the direction of glacial movement. Back Traverse City, Michigan

Striations Next Striations are created when rocks at the bottom of the glacier plow through bedrock, scraping and scarring the land. Finer grain material carried by the glacier scrapes and polishes the rock. These striations are located in Calumet. Back Calumet, Michigan

Kames Next Conical hills, called kames (some are 350 feet high), were formed by surface rivers flowing down to the ground through cracks in the ice, depositing heaps of cone- shaped debris along the way. Back Mt. Pleasant, Michigan

Great Lakes Next The Great Lakes, our most recognizable glacier feature, were formed by the advancing and retreating of major ice lobes. The meltwater from these lobes filled in the depressions left by the glacial ice lobes, thus forming the Great Lakes. Back Animation of the Great Lakes forming over time. These are NOT kettle lakes.

Benefits of Glaciers Next All of these features created by the glaciers have benefitted Michigan’s economy. The Great Lakes, tourism, agriculture, industry, and mineral resources are just some of the glacier related items that have positively affected the production, distribution, and consumption of goods and services in our area.. Back

Great Lakes Next The Great Lakes are the largest sources of fresh water in the world. In addition, they provide important waterways for the transportation of goods not only in Michigan, but around the world. Back

Tourism Next The immense number of lakes, rivers, forests, rolling moraines, and dunes provide ample beauty for vacationers to enjoy. Tourism is an important source of revenue for our state. Back

Agriculture Next Due to the rich, sorted soils created by glaciers, farming is an important part of Michigan’s economy. Just think of all the soybeans, corn, potato fields, and orchards in our region! Back

Industry Next Many industries rely on our glacial artifacts. The auto industry began in our state due to the availability of water transportation and iron deposits used to produce steel. Also, the rivers provide an important source of energy for industry. Back

Mineral Resources Next Glaciers left behind many mineral resources like sand and gravel used in construction. Clay is used to make pottery. The discovery of gypsum, salt, shales, iron, copper, and oil have brought many booms to Michigan’s economy. Back

As you have seen glaciers have left their mark all over Michigan. Not only did they shape our state, but they provide us with beautiful landscapes, sources of entertainment, tourism, agricultural, industry, and mineral opportunities. Next

Itinerary Itinerary Back Last Ice Age Moraines Drumlins Eskers Kames Kettles Thank you for visiting! If you would like to return to any of the “places” you have visited, use the links to the right. Erratics Striations Outwash Plains Till Agriculture Tourism Great Lakes Industry Minerals