What type of glacier forms a u shaped valley?
singleAnswer
mountain mountain glaciation
Glacier Valley U-shaped valley
glacier forms a u shaped valley
U-shaped valley Valley Glacier Overdeepening Fjord Tunnel valley Reintal (Wetterstein) Esker List of landforms Pamir Mountains
U-<b>shaped valleys</b>, trough valleys or <b>glacial</b> troughs, are formed by the process of 
glaciation. ... Glaciated valleys are formed when <b>a glacier</b> travels across and 
down <b>a</b> slope, carving the valley by the action of scouring. When the ... The 
streams that <b>form</b> in hanging valleys create waterfalls that flow into the main 
valley branch. <b>A valley</b> carved by <b>glaciers</b> is normally U-shaped and ... visible upon the 
recession of the <b>glacier</b> that <b>forms</b> it. <b>A glacier</b> is <b>a</b> persistent body of dense ice that is ... During glaciation, these 
<b>valleys</b> are often widened, deepened and smoothed to <b>form a &quot;U</b>&quot;-<b>shaped glacial</b> 
<b>valley</b> or <b>glacial</b>&nbsp;... Overdeepening is <b>a</b> characteristic of basins and <b>valleys</b> eroded by <b>glaciers</b>. An 
overdeepened ... cirque&#39;s low-side outlet (stage) and its down slope (backstage) 
<b>valley</b>. <b>A</b> tarn will <b>form</b> in the overdeepened region once the <b>glacier</b> has melted. Geologically, <b>a</b> fjord or fiord is <b>a</b> long, narrow inlet with steep sides or cliffs, 
created by <b>a glacier</b>. ... <b>A</b> true fjord is formed when <b>a glacier</b> cuts <b>a U</b>-<b>shaped</b> 
<b>valley</b> by ice segregation ... Often, waterfalls <b>form</b> at or near the outlet of the upper 
valley. <b>A</b> tunnel valley is <b>a U</b>-<b>shaped valley</b> originally cut under the <b>glacial</b> ice near the 
margin of ... downward and collect in crevices in the ice, while water from basal 
melting will collect under the <b>glacier</b>; either source will <b>form a</b> subglacial lake. The Reintal (&quot;Rein <b>Valley</b>&quot;) is the name given to the upper and lower <b>valleys</b> of 
the River Partnach between the Zugspitzplatt plateau and the Partnachklamm 
gorge. <b>A</b> hiking route to Germany&#39;s highest mountain, the Zugspitze runs through 
the <b>valley</b>. The <b>valley</b> was formed during the Würm Ice Age by the Reintal <b>Glacier</b> 
and ... which was <b>shaped</b> by the <b>glacier</b> and today <b>forms a U</b>-<b>shaped glacial</b> 
<b>valley</b>,&nbsp;... An esker, eskar, eschar, or os, sometimes called an asar, osar, or serpent kame, 
is <b>a</b> long, ... Eskers may also <b>form</b> above <b>glaciers</b> by accumulation of sediment in 
supraglacial channels, in crevasses, ... Tunnel valley – <b>A U</b>-<b>shaped valley</b> 
originally cut by water under the <b>glacial</b> ice near the margin of continental ice 
sheets&nbsp;... Valley – Low area between hills, often with <b>a</b> river running through it. U-<b>shaped</b> 
<b>valley</b> – Valleys formed by <b>glacial</b> scouring. Slope landforms[edit]. Slope&nbsp;... <b>A</b> pamir is <b>a</b> flat plateau or U-<b>shaped valley</b> surrounded by mountains. It <b>forms</b> 
when <b>a glacier</b> or ice field melts leaving <b>a</b> rocky plain. <b>A</b> pamir lasts until erosion
&nbsp;...
mountain glaciation
U-shaped valley