Glaciers
What is a glacier? Glacier- A large moving mass of snow and ice
Where are glaciers found?
How are glaciers formed? Snow falls on the side of a mountain and begins to collect
As more and more snow piles up, it creates pressure The snow is packed down into ice and accumulates as a large sheet of ice As more and more snow piles up, it creates pressure The snow is packed down into ice and accumulates as a large sheet of ice
Snow into Ice Snow becomes packed As its packed, it turns to ice
Pressure and Gravity As more snow falls, glaciers become thicker and heavier Gravity pulls glaciers downward with great pressure against the ground
Movement Glaciers move very slowly Glaciers slide, or creep over the ground
Calving Calving occurs when pieces of a tidewater glacier break off and fall into the sea
Calving
Crevasses As Glaciers move, the ice on top bends and cracks These cracks are called Crevasses
Crevasses
Glacier Snout Front end of a glacier. Also called the terminus.
Erosion As Glaciers move, they pick up debris Stones and boulders are picked up and carried along Using these stones and their weight, glaciers grind and carve the landscape
Erosion
A glaciated valley in the Mount Baker- Snoqualmie National Forest showing the characteristic U-shape and flat bottom.
Erosion The Llanberis Pass in Snowdonia National Park, north Wales, is typical of a U-shaped valley formed by glacial erosion.
Icebergs
Most of the icebergs are found under water, making them very dangerous to ships.
Calving of a Glacier
Melting Glaciers
Glacier Fun When glaciers melt they deposit materials, creating terminal moraines Let’s see if we can use a model to show what this looks like. Read C10 on Terminal Moraines When glaciers melt they deposit materials, creating terminal moraines Let’s see if we can use a model to show what this looks like. Read C10 on Terminal Moraines
Terminal Moraines A massive terminal moraine marks the greatest advance of a glacier, during the last centuries, in Cordillera Huyhuash, Peru. A lake has formed between the terminal moraine and the glacier front. The tall peak is Nevado Yerupaja. Photo J. Alean 1979.
Picture References 3/ JPG&imgrefurl= /Science/Earth-Sciences/Geology/Landform-Evolution/Glaciers-and-Ice- Sheets/Features/Features-6.html&usg=__0OxwO-5rZGMLp8b- t8R7NM2pfwg=&h=909&w=1136&sz=362&hl=en&start=1&sig2=uw2VFJeSEzViDxRebtnd3 A&um=1&tbnid=PdZUweB8OcexvM:&tbnh=120&tbnw=150&ei=JU8nSdDdBY628AS1jN3_Ag &prev=/images%3Fq%3Ddiagram%2Bof%2Ba%2Bglacier%26um%3D1%26hl%3Den%26r lz%3D1T4DKUS_enUS252US253%26sa%3DN 3/ JPG&imgrefurl= /Science/Earth-Sciences/Geology/Landform-Evolution/Glaciers-and-Ice- Sheets/Features/Features-6.html&usg=__0OxwO-5rZGMLp8b- t8R7NM2pfwg=&h=909&w=1136&sz=362&hl=en&start=1&sig2=uw2VFJeSEzViDxRebtnd3 A&um=1&tbnid=PdZUweB8OcexvM:&tbnh=120&tbnw=150&ei=JU8nSdDdBY628AS1jN3_Ag &prev=/images%3Fq%3Ddiagram%2Bof%2Ba%2Bglacier%26um%3D1%26hl%3Den%26r lz%3D1T4DKUS_enUS252US253%26sa%3DN g g 3/ JPG&imgrefurl= /Science/Earth-Sciences/Geology/Landform-Evolution/Glaciers-and-Ice- Sheets/Features/Features-6.html&usg=__0OxwO-5rZGMLp8b- t8R7NM2pfwg=&h=909&w=1136&sz=362&hl=en&start=1&sig2=uw2VFJeSEzViDxRebtnd3 A&um=1&tbnid=PdZUweB8OcexvM:&tbnh=120&tbnw=150&ei=JU8nSdDdBY628AS1jN3_Ag &prev=/images%3Fq%3Ddiagram%2Bof%2Ba%2Bglacier%26um%3D1%26hl%3Den%26r lz%3D1T4DKUS_enUS252US253%26sa%3DN 3/ JPG&imgrefurl= /Science/Earth-Sciences/Geology/Landform-Evolution/Glaciers-and-Ice- Sheets/Features/Features-6.html&usg=__0OxwO-5rZGMLp8b- t8R7NM2pfwg=&h=909&w=1136&sz=362&hl=en&start=1&sig2=uw2VFJeSEzViDxRebtnd3 A&um=1&tbnid=PdZUweB8OcexvM:&tbnh=120&tbnw=150&ei=JU8nSdDdBY628AS1jN3_Ag &prev=/images%3Fq%3Ddiagram%2Bof%2Ba%2Bglacier%26um%3D1%26hl%3Den%26r lz%3D1T4DKUS_enUS252US253%26sa%3DN g g
Picture References sgrooves2.jpg sgrooves2.jpg sgrooves2.jpg sgrooves2.jpg
Picture References paper/Landscapes/Iceberg.jpg paper/Landscapes/Iceberg.jpg om/data/wximagenew/a/anghy85/465.jpg&imgrefurl= derground.com/blog/mitzy259/comment.html%3Fentrynum%3D1%26t stamp%3D200607&usg=__lnlvCzs83BsZlOsYEUlYGvU95IY=&h=449&w =640&sz=152&hl=en&start=4&sig2=0g7VCNl-ZFNPQbL- aVRMMQ&um=1&tbnid=iWIduoGdOWAtJM:&tbnh=96&tbnw=137&ei= Rk0nSeysPIOs8ASo5riBAw&prev=/images%3Fq%3Dparts%2Bof%2Ba %2Bglacier%26um%3D1%26hl%3Den%26rlz%3D1T4DKUS_enUS252 US253%26sa%3DN paper/Landscapes/Iceberg.jpg paper/Landscapes/Iceberg.jpg om/data/wximagenew/a/anghy85/465.jpg&imgrefurl= derground.com/blog/mitzy259/comment.html%3Fentrynum%3D1%26t stamp%3D200607&usg=__lnlvCzs83BsZlOsYEUlYGvU95IY=&h=449&w =640&sz=152&hl=en&start=4&sig2=0g7VCNl-ZFNPQbL- aVRMMQ&um=1&tbnid=iWIduoGdOWAtJM:&tbnh=96&tbnw=137&ei= Rk0nSeysPIOs8ASo5riBAw&prev=/images%3Fq%3Dparts%2Bof%2Ba %2Bglacier%26um%3D1%26hl%3Den%26rlz%3D1T4DKUS_enUS252 US253%26sa%3DN