Glaciers form U-shaped valleys. They make striations, drumlins, kettlelakes, eratics, moraines and cirque.
Glaciers are typically found at altitudes above 2,500 meters (about 8,200 feet) in tropical regions, while in temperate areas, they can appear at elevations as low as 1,000 meters (about 3,300 feet). The specific altitude at which glaciers form depends on local climate conditions, including temperature and precipitation. In polar regions, glaciers can extend to sea level due to consistently cold temperatures.
so we can see back into the past later on in life to see whats developed of humans. also it is to pick out features of your body <3
Very seldom, but here is one example is his drawing called Valley of the Arno from 1473 Click link below to see it!
There are online features you can complete time trials and post your times online for others to see and if ouy want you can race the ghost of other people online and tyr and beat there time, its a great way to see alternate routes
See related links for lots of "secrets" and interesting places found in Google Earth.Also try searching for "secrets google earth" in any search engine (like Google) and you'll see lots of hits.If you mean "secret" or hidden features in Google Earth (also known as "easter eggs") then see related questions.
Erosional features in areas with valley glaciers include U-shaped valleys, cirques (bowl-shaped hollows at the head of glaciers), arêtes (sharp ridge between cirques), and hanging valleys (smaller valleys that join a main glacier valley). Glacial striations (scratches on bedrock caused by moving glacier ice) and moraines (piles of debris deposited by glaciers) are also common erosional features.
Along an erosional coast, you would typically find features such as sea cliffs, wave-cut platforms, and coastal caves. These formations occur due to the relentless action of waves eroding the land. Additionally, you might see features like sea stacks and blowholes, which result from the differential erosion of rock layers. Overall, the landscape tends to be rugged and steep, reflecting the dynamic processes of erosion at work.
A valley has likely formed in Keswick due to geological processes such as erosion by water, glaciers, and tectonic movements. Over time, these processes have shaped the landscape, creating the valley that we see today.
The Matterhorn was shaped primarily by glacial erosion during the last ice age. As glaciers moved and scoured the rock, they carved the distinctive pyramid shape of the mountain we see today. Subsequent weathering and smaller-scale erosional processes continue to modify its shape.
well all glaciers are gone except for some icebergs and kettles or moraines at anokijig will teach you what the glaciers did
In the air!
A U-shaped valley is formed by the scouring action of advancing glaciers.Please see the related link for more information.u-shaped valleys are formed by glacial erosion.u-shaped valleys often begin their life as v-shaped valleys with rivers in. the glacier follows the exsisting path, deepening, widening and eventually straightening the path. u-shaped valleys are also known as glacial troughs.the process of plucking frezes bits of rock to the glacier, as the ice moves the rocks are plucked out. the pieces of rocks or moraine are pulled along, they smooth and erode the walls and floor of the valley by the process of abrasion. the valley widens over time.after the glacier has retreated or melted a u-shaped valley is formed, usually with steep sides and a realitivly flat floor.for examples of u-shaped valleys type in 'u-shaped valleys' in Google images. The lake district in England has good examples.
Latitudes that are most likely to see glaciers are maritime areas north of 35˚N and south of 35˚S
Looking at glaciers, walking on glaciers, going to ski resorts, see icebergs, going fishing, and lots more
The Appalachian Mountains were worn down by the processes of erosion, including water, wind, and glaciers over millions of years. These erosional forces gradually smoothed out the peaks and created the rolling landscape we see today.
Visitors to Alaska may see the glacier at Glacier Bay National Park and Preserve, located in the southeastern part of the state. This park features numerous glaciers, including the famous Margerie Glacier, which is a popular attraction for tourists seeking to witness the grandeur of Alaska's icy landscapes.
You could see evidence the glacier was melting as the sun shone upon it.