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Landscapes

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Landscapes. Landscape Development. Landscapes: A region on Earth’s surface in which various landforms are related by a common origin. Factors That Impact Landscape Development. Climate Local Bedrock Geologic Structures Human Activities. Types of Landscape Regions. Mountains : - PowerPoint PPT Presentation

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Page 1: Landscapes

Landscapes

Page 2: Landscapes

Landscape Development

• Landscapes:• A region on Earth’s surface in which

various landforms are related by a common origin.

Page 3: Landscapes

Factors That Impact Landscape Development

• Climate

• Local Bedrock

• Geologic Structures

• Human Activities

Page 4: Landscapes

Types of Landscape Regions• Mountains:• Has the greatest relief between the highest peak and the

deepest valley.• Relief: (change in elevation from the highest point to the

lowest point)• RELIEF:

10m

0m

10m - 0m = 10m

Page 5: Landscapes

HOW ARE MOUNTAINS CREATED?

• A daddy mtn and a mommy mtn fall in love and because they love each other so much…….

•MR. O’D!!!!!!!!!!!!!!!!!!!!!!!!!!!!

Hey Mama!!!!

Page 6: Landscapes

HEHEHE• Tectonic forces push Earth up to create a

mtn.

• Convergent plate boundary

Page 7: Landscapes

Plateau

• A plateau landscape is often relatively flat or rolling uplands that streams have cut valleys into.

• Rock structure:• “It’s sedimentary my dear Watson” • Smaller relief than mtns• Larger than plains• Examples of plateaus: • Colorado Plateaus near the Grand Canyon

Page 8: Landscapes
Page 9: Landscapes

Plains

• Plains are generally flat and are at a lower elevation.

• Rock Structure: flat layers of sedimentary rocks.

• Midwest and Florida

Page 10: Landscapes

Landscapes and Culture

• Landscapes help shape the culture of an area.

• Physical boundaries can help bring together communities for a common need or shut off a community.

Page 11: Landscapes

Climate and Landscapes• Landscapes in moist environments are

generally rounded.

• (Chemical Weathering, Good Soil)

• Those is arid environments show sharp angles and steeper slopes.

• (Physical Weathering, Not Enriched Soil)

Page 12: Landscapes
Page 13: Landscapes

Drainage Patterns

• Drainage Patterns: The way water runs off of a landscape.

• Rule of thumb:

• Streams will tend to follow zones of weaker rocks.

Page 14: Landscapes

Four Types of Drainage Patterns1. Dendritic:

• Branching

• Usually found on flat laying rock or uniform rock.

• Ex. Appalachian Plateau near Oneonta

Page 15: Landscapes

2. Radial• Rolls off of a dome

• Usually found by a circular volcano or dome mountain.

• Ex. The rim of the Adirondacks

Page 16: Landscapes

3. Rectangular• Follows zone of weaker rocks in

rectangular patterns.

• Usually found in faulted, tilted or folded rock layers.

• Ex. Finger Lakes and the Central Adirondacks.

Page 17: Landscapes

4. Annular• Circles, then down, circles, then down.

• Usually found when you have a dome with upturned layers.

• Ex. Esopus Creek near Phoenicia, NY.

Page 18: Landscapes

New York and the Ice Ages• New York was covered with glaciers

• Alpine glaciers: valley glaciers, these are the ones that make U shaped valleys and move due to their weight and the slope of the land they are on.

• Continental glaciers: ice sheets that move solely on their own weight.

• The Finger Lakes were created by advancing glaciers.

Page 19: Landscapes

Erosion and Deposition by Glaciers

• Erosion: takes away from the land

• Ex. Finger Lakes

• Deposition: adds to the land

• Ex. Drumlin: tear shaped hills created in front of the advancing glacier.

• Ex. Moraines: plies of unsorted soil and rocks left where the glacier stopped advancing. (Long Island shows this)

Page 20: Landscapes

Drumlin

Page 21: Landscapes
Page 22: Landscapes

Terminal Moraine

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Page 24: Landscapes
Page 25: Landscapes

Kettle Lakes• : when buried blocks of ice cause a

depression in the ground and it fills with water.