ビデオジャパンは、最大でランク。
X Glacier
oT: t[STwEBLyfBAiWikipediajx Source: Wikipedia The Free Encyclopedia (Wikipedia),
X ijARndARXAXB Glacier (glacier), the mountain is gravity, the continent is to smooth the flow of high pressure and the thickness of the ice, a huge chunk of ice.
Contents |
[ W ] Tv Summary
XARAXn`ANXA NkB Glacier, mountainous, or sloping terrain, snow and ice accumulated over several years, in that which is compressed snows. XZcB The bottom is still to ZKEZU are made in the last ice age. XNHAsAXn`B The glacial erosion and deposition in an active, create a unique glacial topography.
nCXWA Ci A CB Glaciers and the global temperature is closely related, advanced sea, be a source of marine regression. XAXAO[hXAv1,633kuyAn11B Glaciers are found on land, the Antarctic ice sheet, the Greenland ice sheet as a maximum, total 10,000 k u and 1633, covering about 11 percent of the total land area.
NngekAB In recent years the severe reduction in the effects of global warming is a problem. i XZQ j (And by reference to melting glaciers)
[ W ] X Classification of glacier
XBn2`mB The glacier has developed two regions known to have different forms. Rxn`RxXB One is the formation of mountain glaciers in mountain area. O[hLXB Another is the glacial continentURU a vast area of Antarctica and Greenland.
RxXxNA\XZ_tmB Temperature of the mountain glaciers throughout the year, it is known that near the melting point of ice from the surface to the bottom. AnXpAX_nB The polar ice sublimation is rapidly cooled by water, there is no meltdown in sub-zero. nX\GZ_tBAnXAXZ_B Surface of the sub-polar glacier is reached near the melting point of the season, but some of the water flow into the interior glaciers melted, the bottom of the glacier is below the melting point.
Xx\B Temperature of ice can tell by the surface state. X{\oB Where there is ice on the surface where the body is broken. AZNB Be covered in the snow is dry, there is melting even in summer is not happening. \AA\XXwBMAor the melted water to the surface, where that is flowing into the cracks, there is a layer of ice or ice gorge had been frozen and re-surface inside. AX_CB In the wet snow that has piled all the snow from last summer temperatures rose above freezing point. XdAXwAXX`B In the presence of ice on top of one another, and re-freeze in the cold layer of melted glacier water, which is being formed where the glacial ice.
XKARxnJA JX (valley glaciers)B That most small glaciers in the valley that exists in the mountains, glacial valleys (valley glaciers) is called. KA XXooX (outlet glaciers)B Slightly larger than the size of the glacier runoff flows out from the ice cap (outlet glaciers). XXRARARB Is a mass of snow, ice cap at the top of the mountain, mountain range, of course, also present on the volcano. XXXJosAoX`B Ai Tani is going to have flowed like a tongue of ice from the ice cap, to form the glacier runoff. oXAXSAKB Glacier runoff is in the eyes of the whole glacier, but that's still small. RXX`oXACBB Was formed by glacial runoff from the mountains and giant ice cap polar cap, until it reaches the sea.
XXB The largest glacier in the ice sheet. n\n`BB It is obscure to most of the terrain below the surface. XAO[hAnc^RB Ice is now only present in the Greenland and Antarctica, which is the reason why the presence of fresh water in a large number of these. AO[hX6[gCB It depends on how much and how it just melted the Greenland ice sheet 6 being called meter sea level rise. AX65[gB Also, the thaw of Antarctic ice sheets have a 65 meter rise.
XXAXXP[B Ice is similar to ice, compared to small-scale ice sheets. XWB Continental glaciers exist in the high altitude plains. ^CvXAACXhAkCXAueBbVRrABkmRAXJnB This type of many glaciers in Iceland, and Arctic Ocean islands, are present in the region between Alaska and the North Pacific Ocean from the mountains of southern British Columbia.
XC (tidewater glaciers)AXCB Coastal glaciers (tidewater glaciers) is that the glaciers flowing into the sea. CBXAAXR`B Glacier reaches the sea, or crumble, and forms an iceberg in isolation or. XCBAB Most of the glaciers reach the sea and collapsed, often cause a tremendous splash. [[AXCAXRRB If deep water, submerged in the sea hear the glacier, sometimes unexpectedlyKIGAiceberg. AXJXCAto[hX( en:Hubbard Glacier )10kmCB Coast is the longest glacier in Alaska, glaciers FUBADO (en: Hubbard Glacier) is located 10km to the sea. N^bgpXpA30mXiADKLB Yakutat Bay and Glacier Bay, the 30m-high cave scene at the glacier which is famous for being visited by cruise ship. ^CvXA^Cv]AICeB Glaciers of this type from other types of assessment, susceptible to a long-term climate change.
[ W ] X` Formation of glaciers
rIxXAZJlF( en:névé )B Glacier is a relatively high temperature, rough neve repeated freezing and melting (en: névé) and principal component called snow. B This snow is called corn snow. XXAXwZAtBXB Glacier ice is melting under pressure and under a layer of snow and ice, changes in the firn of the ice grains. tBwNoAkXX(glacial ice)B Firn layer is constant and the years pass, the glacial ice is more compressed (glacial ice) and. AxA\nB The snow will be just some of the changes in temperature, the crystals begin to degeneration in each of the bumps on the surface within hours. (C) (With different symptoms of the vapor pressure)
pen:Glacier|B English version en: Glacier translation. en:user:GeologyguyB Author en: user: Geologyguy More.
[ W ] A See also
- Xn` Glacial landform
[ W ] ON External links
- XZ^[ Center Ice
- uGlacierv - Encyclopedia of EarthuXvipj B "Glacier" - Encyclopedia of Earth in the "ice" on the item (s).
 | u X vn`AB "Glacier" It is a writing-related topography. LME B SARU collaborators are seeking to equal corrections fill in this article. i P:nw / PJn` j (P: geography / topography PJ) |
ビデオジャパンは、最大でランク。
© Lullar