How The Last Ice Age Shaped Canada

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.
The Glacial History of Michigan
Glaciation of Canada.
Glacial Landforms. Continental Glaciers Striations Erosion of soil.
Glaciers and the Great Ice Ages
Chapter 7: Erosion and Deposition
Glaciers and the Great Ice Ages. Pleistocene Epoch: the Great Ice Ages 2.0 Ma to 10,000 years ago Four (or more) distinct episodes expansion and melting.
Day #2-Processes That Shape Ocean Basins and Drainage Section 2.3.
Canadian Landforms.
GLACIERS CHAPTER 5 HONORS EARTH SCIENCE. What is a glacier? a thick mass of moving ice
Chapter 5: Section 2 Surface Processes and Landscapes
The Great Lakes Brandon Dunn, Kate Thometz, Vince Amicon.
The Geological History of Toronto and the GTA. Toronto’s Geological History The oldest rocks in southern Ontario are up to 1.5 billion years old and are.
Glaciers.
Chapter 3 Section 4 Glaciers. Moving mass of ice and snow Form when more snow falls than melts Agent of erosion.
Glacial Erosion.
Glaciers Glaciers formed much of the landscape that exists presently in the northern United States and elsewhere in the world. Glaciers Today, scientists.
Erosion and Deposition
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.
Glacial Landscapes Glacier = large moving mass of ice. Glacier = large moving mass of ice. Glaciers erode, transport and deposit massive amount of sediment.
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.
Mysterious rock formations…….. What could have caused these formations? GLACIERS!!!!!
Glacier photos. When the climate cooled… Ice advanced over the land, moving southward from Canada over the Great Lakes Region.
How The Last Ice Age Shaped Canada
CGC 1D1 Mr. Zapfe.  Final changes occurred which gave Canada’s landforms their present shape  Continuing collision of North American and Pacific Plates.
UNIT #1 Geography NOTES Wisconsin’s Landforms. Chapter UNIT #1 Geography NOTES Wisconsin’s Landforms Glaciers -Nearly 3/4 of Wisconsin was glaciated (covered.
Chapter 7.3 Glaciers. Glacier Any large mass of ice that moves slowly over land. Two kinds: – Continental Glaciers – Valley Glaciers.
 Runoff  Streams  Rivers  Water picks up particles of clay, sand, and gravel as it moves along Earth’s surface  Small grooves form – called rills.
Glacial Landforms. Continental Glaciers Striations Erosion of soil.
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.
Agenda Check In Review notes Glaciers WATER Who’d’a Thunk: Karaoke means “empty orchestra” in Japanese.
 As much as plate tectonics builds up the Earth’s surface, forces in nature are also working to wear it down. One major force of erosion happens due.
Alaska from space.
EROSION: The force that shapes the Earth!
Glacier Review.
Glaciation in Canada.
Glaciers and Glaciation
How Do Glaciers Shape the Land?
AIM: How do Glaciers change the landscape? Do Now:
Ice Ages and Glaciers Ch. 1 Lesson 1 Cont..
Glaciers Pg. 79.
Like running water, gravity is the driving force
Unit 5: Gradational Processes Ms. Thind
Glaciation of Canada.
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
How the last Ice Age shaped Canada
Glacier Terms.
Chapter 3: Changing Climates
Glaciation of Canada.
Aim: How do Glaciers affect the land?
Glacial Erosion Chapter 4.2.
Erosion and Deposition
Erosion & Deposition by Glaciers
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.
Glaciers 8.3.
Canadian Landform Regions
Glaciers.
Glacial Erosion.
Erosion & Deposition by Ice
Earth Science Chapter 8 Section 3
Glacial Erosion Chapter 4.2.
Glaciers.
A Virtual Tour Focusing on Glacial Features in Michigan
Glaciers.
Glaciers.
Presentation transcript:

How The Last Ice Age Shaped Canada

What Were The Ice Ages? The Ice Ages began 2.4 million years ago and lasted until 12,500 years ago. Glacials: cold periods during which glaciers covered large parts of the world Interglacials: very warm periods during which many of the glaciers melted.

Ice Ages Cycle

Why were there Ice Ages? Many causes have been suggested for the ice ages including: changes in solar flux changes in the shape of Earth’s orbit & the tilt of its axis Probably it was a combination of several such influences.

The Pleistocene Epoch The Pleistocene Epoch is the actual name for the time period This period is the first in which Homo sapiens evolved, and by the end of the epoch humans could be found in nearly every part of the planet.

The Last Ice Age The world's most recent glacial period began about 110,000 years ago and ended around 12,500 years ago.

Laurentide Ice Sheet A massive ice sheet that covered most of Canada and a large portion of the northern US It covered most of northern North America between 95,000 and 20,000 years ago. It created much of the surface geology of the area, leaving behind many glacial landforms

Retreat of the Laurentide Ice Sheet As the ice sheet retreated, it left behind many large glacial lakes

How Do Glaciers Form Landscapes? By scratching the surface like sandpaper Glaciers can pick up rocks and sand Then the ice sheet acts like sandpaper and scratches the land underneath Striation: a scratch mark on a rock It can also polish the rock smooth

How Do Glaciers Form Landscapes 2) The glacier will dump rocks along the way Glaciers will leave rocks and sediment as it moves It will leave little mounds and hills along its edges

Glacial Landforms Till: the sediments in a glacier Moraines, Eskers, Drumlins: hills created from the deposit of till from a glacier Kettle Hole: the hole or lake created from a leftover chunk of glacial ice

Toronto’s Ice Age

Great Lakes and Lowlands Most of the Great Lakes’ basins were carved out by the moving ice. Soil and rocks were scooped off the Canadian Shield and deposited over southern parts such as Toronto.

Formation of the Great Lakes

Toronto Drumlins Toronto has several drumlins, ridges created by glaciers. https://www.youtube.com/watch?v=677PQitX7Fk

Don Valley The deep wide lower Don valley was formed after the draining of Lake Iroquois (a huge glacial lake) Many streams, including The Don, cut deep U-shapes ravines through the previously V-shaped valley

Toronto’s Lakeshore Modern Lake Ontario is within the bed of ancient Lake Iroquois, a meltwater lake that rose while Ice Age glaciers blocked the outlet of the Saint Lawrence River to the sea.

Old Toronto

Oak Ridges Moraine North of the city The moraine's spongy wetlands and soil were deposited 12,000 years ago from the retreating glacier Now dozens of streams spring from there and 35 of them pass through the Greater Toronto Area.

The Toronto Islands The Scarborough Bluffs, for instance, are a section of the Lake Iroquois shoreline. Toronto Islands were created from sand deposits eroded from the Scarborough Bluffs The sand collected near the mouth of the Don River, forming a long, sandy spit that would eventually be the Toronto Islands. They were only a peninsula until a severe storm washed out part of the peninsula in the 1850s

Ice Age Videos http://www.youtube.com/watch?v=dJ5GYQrkvxI 2:08 “What is an Ice Age?” https://www.youtube.com/watch?v=er9DqviC5XE 44:04 “North American Ice Age”