Glaciation In Snowdonia Some Post Glacial Changes

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Glaciation in Snowdonia - Some Post-Glacial Changes to the Landscape

Snowdonia – Post Glacial Changes ,[object Object]

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1. A glacier is a large, long-lasting mass of ice formed on land that masses downhill under its way. Glacier is part of the earth’s hydrosphere. Along with the sea, ice glaciers are known as the cryosphere. 2. GROUP OF GLACIER: They fall into two general groups based on their form size and flow characteristics 3. Alphin glacier that is surrounded by mountains is called an alpine or mountain glacier. Glaciated valleys are through like U-shaped with board floors and relatively smooth, and steep sides The valleys may contain littered debris or debris shaped as moraines with a swampy appearance. There may be taken gouged out of the rocky floor or formed by debris within the valley. Cirque Glacier: Bowl-like hollow structures are called cirque glaciers. They are formed inside the mountains and tend to move towards the valley. A glacier that forms in a cirque is a cirque glacier.Piedmont Glacier: When the steep valley glaciers spill into flat plains, then a piedmont glacier occurs e.g Malaspina glacier that falls into Yakutat Bay, Alaska.Hanging glacier: When the major valley glacier thins out, that becomes a hanging glacier.Tidewater glaciers: These are valley glaciers that reach the sea, and they provide breeding habitat for seals. These glaciers are the ones that form small icebergs. 4. Continental glaciers are those vast masses of ice sheets covering stretches of land. Such glaciers flow over large areas that are unconfined, where they bury the landscapes underneath Today, continental glaciers are only present in extreme polar regions: Antarctica and Greenland Historically, continental glaciers also covered large regions of Canada Europe and Asia, and they are responsible for many distinctive topographic features in these regions. The ice sheet blankets 81% of Greenland and 90% of Antarctica. FORMATION AND FLOW: IMPORTANCE OF CONTINENTAL GLACIER: Glaciers are an essential indicator of the study of environmental change, thereby making people aware of the increasing global warming. Due to the continuously growing industrialization, and use of automobiles, there is a rising graph of air pollution triggered by the emission of carbon monoxide and other harmful greenhouse gases. The outcome of all these is the catastrophic increase in global warming and greenhouse gases. Glaciers come in a huge range of shapes and sizes. Different glaciers, and even different parts of the same glacier, can have a variety of different thermal, hydrological and dynamic characteristics. Glaciers occur in locations ranging from the poles to the equator, and most parts of the world have experienced the direct effects of glaciation at some time in the past. Glaciers currently occupy less of the planet than they have done in geological history, but nevertheless exert a profound influence on the global environment. Our developing understanding of glaciers will play an important role in our understanding of the global environmental system

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