PPT-Melting of glaciers: During the last 27 years the Quelccaya

Author : kittie-lecroy | Published Date : 2016-08-04

Lonnie Thompson Ohio State University Temperate regions From 1990 to 2005 the Morteratsch glacier in the Bernina area Switzerland retracted several ten meters

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Melting of glaciers: During the last 27 years the Quelccaya: Transcript


Lonnie Thompson Ohio State University Temperate regions From 1990 to 2005 the Morteratsch glacier in the Bernina area Switzerland retracted several ten meters Kilimanjaro The Human impact. GLACIERS OF GLACIERS OF SWEDEN By VALTER SCHYTT 1 2 Abstract The most recent glacier inventory lists a total glacier area for Sweden of 314 square kilometers. The first glaciological were made in History of Sea Level Rise in Florida. 120,000 years ago 18,000 years ago Today. + 6 meters - 120 meters . Causes of Sea Level Rise. Thermal expansion of water. Finish South Asia. Nepal: Everest Region. Glacier Lake Outburst Floods. 1999 Slides. Summary of Observed Glacier Changes. Sketch Maps Due on Wednesday!. For . Next Class: Read Chapter 13 (pp. 588-598). Which describes one way that early hunter-gatherers got food?. They used language to organize. They used tools to kill animals. They grew crops on farms. They grew seeds and nuts. What was the main unit of Stone Age culture?. Erosive forces . Glacier. persistent . body of dense ice that is constantly moving under its own . weight.. It . forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many . Section 1: Glaciers – Moving Ice. Section 2: Glacial Erosion and Deposition. Section 3: Ice Ages. Section 1: Glaciers – Moving Ice. . N. atural . forces compact snow to make a large mass of moving ice called a . Prairie School. Earth Science. Glaciers: Moving Ice. When you take a handful of snow and squeeze it, you are creating a product that is similar to that of glaciers. . Glacier: fast moving, large mass of ice. . Do Now:. The material seen below was left behind by a retreating glacier. Describe the sediments seen in the picture. . . Tasman Glacial Moraine, New Zealand. Formed from the accumulation of ice and snow over thousands of years. . Glacier Movement. Deposits by Glaciers. The Ice Age. Glaciers and Global Warming. Glacial Rebound . …………………. Snow. Line. …………………... Glaciers form in areas covered by snow, where more snow falls than melts each year.. Glacier – thick ice mass that forms over hundreds or thousands of years.. 15, 000 years ago > 30 % coverage - Today 10 % coverage. Valley Glaciers. Ice Sheets. Types of Glaciers. Valley Glaciers. Agent . of . weathering, erosion, and deposition . – acquire, transport and deposit sediment. Occupy ~10% of land area. “Interrupts” hydrologic cycle by “locking up” water. Glacier. GLACIERS. It originates on land from the accumulation, compaction, and . recrystallization. of snow. .. A glacier appears to be motionless, but glaciers move very slowly.. Glaciers are dynamic weathering . and erosional . Glacier. persistent . body of dense ice that is constantly moving under its own . weight.. It . forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many . years.. 4-Seppanen . October 24. th. , 2017. Photo courtesy of Alaska.gov. How Glaciers are Formed. Glaciers are formed with snow that doesn’t melt. When snow builds up on itself the snow will build up weight and will compress and turn into ice..

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