YOSEMITE VALLEY. GENERAL CHARACTERISTICS Yosemite means ‘grizzly bear’ 7 miles in length 1-2 miles in width Elevation almost exactly 4,000’

Slides:



Advertisements
Similar presentations
The Illustrated History of GLACIAL EROSION
Advertisements

GLACIERS In the following presentation you are going to see some actual pictures of glaciers and landforms resulting from glacial movement. Some key words.
How Glaciers Move ___________________ ____________ ______ __________
Geography Presentation America's National Parks. This is the Roosevelt Arch. President Teddy Roosevelt placed the cornerstone here. Yellowstone National.
The Glacial History of Michigan
GLACIAL LANDFORMS SHAPE MOUNTAINS
1. Common Things 2. Plant and Animal Life 3. Geology 4. Tourism and Sport Activities.
The Grand Canyon. The Grand Canyon in Arizona was carved out of the Earth by erosion. Erosion is the process by which weathered rock and soil are moved.
Glacial Erosion This type of erosion is called abrasion. Ice
Glaciation of Canada.
Erosion: Deposition: AIM: Erosional and Depositional systems
How Yosemite Valley was formed 470 million years ago to today a story of uplift, erosion, glaciation, and sedimentation.
Yosemite National Park By: Griffin Simmons Earth Scientists – look at this playground! Come and research! Come and enjoy! Help us keep the beauty!
Pleistocene Glaciation of North America. Pleistocene Ice Ages.
YOSEMITE VALLEY. GENERAL CHARACTERISTICS Yosemite means ‘grizzly bear’ 7 miles in length 1-2 miles in width Elevation almost exactly 4,000’
Chapter 7: Erosion and Deposition
How do Glaciers affect the land? WED V17. What is a glacier? 0 A large, long-lasting mass of ice which forms on land and moves downslope because of gravity.
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.
Interesting Facts It was lifted above sea level and flexed into a mountain range surmounted by a chain of volcanoes much like today’s cascade range. The.
CHAPTER 5 HONORS EARTH SCIENCE
Glaciers. Glaciers are massive streams of ice flowing down across the landscape. Gravity pulls them downward and their weight causes them to move, ever.
GLACIERS CHAPTER 5 HONORS EARTH SCIENCE. What is a glacier? a thick mass of moving ice
Chapter 5: Section 2 Surface Processes and Landscapes
Fluvial Morphology: Landforms Made by Running Water
Running water: The major force of erosion acting on Earth today. If it weren’t for the mountain- building activity of plate tectonics, Earth would be completely.
‘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.
Nature’s Bulldozers CGF3M Wed. Nov. 6, Glacial Erosion As glaciers move, they erode the land in two ways: plucking and abrasion. - Plucking occurs.
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.
Glacial Erosion.
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 & Streams Part 2 Mr. King. How Glaciers Move Mountain Side.
Chapter 21: The Glacier Systems and the Ice Age Presentation.
GLACIERS A glacier is: Any large mass of ice that moves slowly over land Any large mass of ice that moves slowly over land.
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.
Erosion and Deposition by Glaciers Chapter 4: Topic 8.
Guided Notes For Glaciers Section 8.3. Glaciers shape the landscape by eroding, transporting, and depositing huge volumes of rock and sediment.
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.
Glaciers Section 9.4. Glaciers are any large mass of ice that moves over land Continental Glaciers - cover much of a continent or large island (10% of.
Ansel Adams’ Landscape Photography Mrs. Bartles. Ansel Adams Ansel Adams was a photographer and conservationist born in San Francisco, California.
Name of Province: Sierra Nevada. Sierra Nevada Color in province Put color in legend Write province name in legend.
LITHOSPHERE LANDSCAPE FEATURES RESULTING FROM GLACIAL AND FLUVIOGLACIAL ACTION Glacial Action by iceFluvioglacial Action by Meltwater Erosion Deposition.
Glaciated Landscapes Corrie Deep rounded hollows with a steep back wall. After the ice has melted a lake will be formed behind the rock lip, the lake is.
Glacier photos. When the climate cooled… Ice advanced over the land, moving southward from Canada over the Great Lakes Region.
AIM: How do Glaciers change the landscape? Do Now:
GLACIERS AND GLACIATION. GLACIER A body of ice Formed on land Recrystallization of snow=> Firn => Ice Evidence of movement Alpine (valley) glaciation.
Glaciers.
North America’s National Parks. This is the Roosevelt Arch. President Teddy Roosevelt placed the cornerstone here. Yellowstone National Park, in Wyoming,
How The Last Ice Age Shaped Canada
Chapter 3 Erosion and Deposition Section 4 Glaciers
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.
Come See Half Dome and the Sierra Nevada Batholith! Mrs. Donovan Example Date, Teacher YOSEMITE NATIONAL PARK.
Glaciers & Ice Ages. Davidson Glacier near Haines, Alaska.
Lab: How do glaciers shape the land? 12/08/09 Topic: Glacier DN: How do glaciers erode the land?
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.
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.
The Illustrated History of GLACIAL EROSION
2. The dark bands are called
LANDSCAPE FEATURES RESULTING FROM GLACIAL AND FLUVIOGLACIAL ACTION
Landscape Development
Erosional Features 2 The Glacial Trough.
The Illustrated History of GLACIAL EROSION
How Glaciers Modify the Landscape
The Illustrated History of GLACIAL EROSION
LANDSCAPE FEATURES RESULTING FROM GLACIAL AND FLUVIOGLACIAL ACTION
Presentation transcript:

YOSEMITE VALLEY

GENERAL CHARACTERISTICS Yosemite means ‘grizzly bear’ 7 miles in length 1-2 miles in width Elevation almost exactly 4,000’

50-10 million yrs ago - a broad valley Merced river meanders along

Valley Stage: My The land destined to become Yosemite National Park was made up of gentle, rolling hills and streams. The Merced River was a slow-moving, sluggish stream. Hardwood forests flourish

The land rises- the valley becomes a canyon 10-3 million years ago, tilting of Sierras

10-3 Ma Canyon Stage 10-3 million years ago, the Sierra Nevada, California's "backbone", rose. The Sierran block uplifted, tilting westward, increasing the Merced Rivers flow so it carved the valley into a canyon. Redwood forests flourished. 3 Ma ago the Merced River is a steep, V- shaped, riverine canyon.

The Ice Age begins, glaciers carve the valley El Portal/Sherwin glacial stage: 1 My miles in length

Major Glaciation Probably lasted about 300,000 years Glaciers filled the V-shaped Yosemite Valley, widening, deepening and carving it into a "U" shape, forming hanging valleys from which waterfalls now cascade. Gouged out basin that lies more than 1,000’ below present valley floor Half dome a nunatak

The last glacier surge- 30,000 yrs ago

Tioga Glacial Stage Yosemite Glacier entered the valley but did little to alter the landscape. Older glaciers had already excavated 2,000 feet into the bedrock. Only advanced as far as Bridalveil Falls. At this location the forward movement of the glacier was balanced by the melting of ice at its front, producing a large terminal moraine.

The ice age ends: Lake Yosemite

14,000-10,000 years ago Temperatures warmed and the last valley glacier melted. Its terminal moraine (rock debris) dammed the valley 14,000 to 15,000 years ago, creating Lake Yosemite. Sediment eventually filled the lake, which became the flat valley floor we see today.

Following pictures from the USGS site at:

El Capitan on left

Cathedral Spires

Bridal Veil Falls, Leaning Tower

Sentinel Rock

Yosemite Falls

Royal Arches, Washington’s column

Half Dome

Hetch Hetchy Canyon, next to Yosemite Valley Now Hetch Hetchy Reservoir, San Fran water supply

SUMMARY Broad-valley stage (50-10 My) Canyon stage (10-3 My) Pleistocene glaciation begins (2 My) Last glacial stage 30,000 years ago (Wisconsin/Tioga) Lake Yosemite formed by recessional moraine about 10,00 years ago El Capitan and Half Dome nunataks