Presentation is loading. Please wait.

Presentation is loading. Please wait.

Erosion and Depistion BY GLACIERS!.

Similar presentations


Presentation on theme: "Erosion and Depistion BY GLACIERS!."— Presentation transcript:

1 Erosion and Depistion BY GLACIERS!

2 What is a Glacier? a. A glacier is ________________ ___________________________ ___________________________ Glaciers occur in the polar regions and at high altitudes a large mass of slowly flowing ice and snow that formed from the compaction and re-crystalization year after year.

3 b. Types of glaciers 1. _____________- glaciers that form in mountain valleys at high elevations Ex: _______________ , _____________ ______________ , ____________ 2. __________- glaciers that form over vast areas of land. –Like Ice Sheets Ex: ____________, _____________ Valley / Alpine Alps (Europe) Himalayas (Asia) Rockies (N.A) Andes (S.A) Continental Greenland Antarctica

4 Glacial Movement Movement occurs due to gravity
down a slope or outwards under it’s own pressure

5 Profile of a valley glacier
alpine Valley glaciers are called _________, and like a stream, valley glaciers move fastest in the ________ where the least friction occurs A MORAINE is rock and sediment debris pushed along the front edge of a glacier. middle

6 Erosion by glaciers Till 1.
2. As a glacier moves, it plucks up loose rock material (E) . ____- is all the unsorted rock material carried by a glacier. The glacier, with pieces of rock within the ice, acts like a piece of sandpaper! Can grind down mountains (E). Results: Polished and rounded mountaintops, and scratched bedrock Till

7 Deposition: When the Ice melts the till just drops on out!

8 -A MORAINE is rock and sediment debris pushed along edges of a glacier.
-typically UNSORTED sediments because they are deposited by ICE and not liquid water.

9 Moraine’s can be seen by “dirty” streaks in the glacier
medial moraine lateral moraine

10 Boulders from the last Wisconsin Ice advance are pushed as far as NYC
Boulders from the last Wisconsin Ice advance are pushed as far as NYC!- Shawangunk ridge, Gardiner NY

11 These are referred to as “Erratic's” because the geology of the boulder does not match the rock type of that area

12 Glacial Erosion: Stream Valleys vs. Glacial Valleys
V-shaped valley eroded by a __________ U-shaped valley eroded by a __________ stream glacier

13 BANFF National Park, Canada

14 Erosion in Stream Valleys vs. Glacial Valleys
U-shaped V-shaped

15 Post Glacial Landscape Features, Depositional or Erosional
Post Glacial Landscape Features, Depositional or Erosional? Formation of Long Island: Lesson Interactive: Moraines and outwash plains

16 Esker- long winding ridge of sediment.
Drumlins- elongated hills formed when a glacier slides over a pile of sediment. (looks like spoons-D) Esker- long winding ridge of sediment. - SORTED and layered because it is deposited by running melt-water under glacier

17 Kame- irregular shaped hill of unsorted sediment
Kettles & Kettle-Lakes- when a block of ice indents the soil to create a depression. If it melts it forms a “kettle” lake (D) Kame- irregular shaped hill of unsorted sediment (forms when sediment flows into cracks of glacier) (D)

18 Erratics- a large rock plucked up and dropped off by the glacier (D)
Striations - parallel lines in the bedrock caused by rock fragments scratching (E) Erratics- a large rock plucked up and dropped off by the glacier (D)

19 MORAINES: Depositional

20 Most Glaciers are retreating globally at this moment in time 


Download ppt "Erosion and Depistion BY GLACIERS!."

Similar presentations


Ads by Google