The noun forms of the verb 'require' are requirement and the gerund, requiring.
The radical form is √1300. It is possible to simplify that but the question does not require simplification.
There is no universally best form. Different data sets may require different forms, and the choice will also depend on what aspect of the data you wish to highlight.
2.14 is a fraction. It is a fraction in decimal form rather than in the form of a ratio. However, that does not stop it being a fraction. Its equivalent, in rational form, is 214/100. You can simplify this rational fraction if you require.
68.75 is a fraction. It is a fraction in decimal form rather than in the form of a ratio. However, that does not stop it being a fraction. Its equivalent, in rational form, is 6875/100. You can simplify this rational fraction if you require.
Yes, glacier is a noun. "Glacial" is the adjective form.
Escher's are glacial features formed when meltwater streams underneath a glacier, creating tunnels and channels that can collapse to form depressions on the glacier's surface. These features can disrupt or alter the glacier's flow and structure.
Glacial erosion can form various landforms like cirques, arêtes, and valleys. As glaciers move, they pick up rocks and debris, which can carve out shallow grooves known as striations on the underlying rock. When the glacier retreats, it leaves behind moraines made up of this debris.
The unsorted rocky debris formed by a melting glacier is known as glacial till. This mixture of rock fragments of various sizes and shapes is deposited by the glacier as it retreats, with no specific order or arrangement. Glacial till can form different landforms, such as moraines or drumlins, depending on how it is deposited.
Glacial valleys form through the process of glacial erosion, where the movement of a glacier carves and shapes the valley over time. As the glacier moves downhill, it picks up rocks and sediments, which act as abrasives that wear away the underlying rock. The downward pressure and friction of the glacier further deepen and widen the valley, creating a distinct U-shaped profile.
A terminal moraine is a glacial feature that results from deposition. Terminal moraines are long, low ridges of debris that mark the furthest advance of a glacier.
Glacial erratics aren't exactly formed. They were deposited by glaciers that were moving in that area at one time. improved= Glacial erratics are exactly formed. Because a glacier is so heavy, the glacier can pluck large rocks as the glacier moves. When the rock is too heavy for the glacier to hold, or the glacier is retreating, it then deposits the rock in a place where it wouldn't usually be found. This is what an erratic is. A large piece of rock in an unusual surrounding. i hope this helps :)
A glacial trough is a U-shaped valley carved out by a glacier as it moves downhill. It forms through a process called glacial erosion where the glacier scours and deepens the valley over time by plucking and grinding the bedrock beneath it. The vast weight and movement of the glacier cause it to scrape and shape the landscape into a distinctive U-shaped trough.
A drumlin is a land-form from glacial deposition, which was once eroded. It is formed both by erosion and deposition. A drumlin is formed when moraine deposited by a retreating glacier is subsequently reshaped by the returning glacier the following year or after the glacial interval with caused the glacier to retreat in the first place.
Glacial moraines are accumulations of rock, soil, and debris carried and deposited by a glacier. They form as the glacier flows, picking up material from the land surface and carrying it along. Once the glacier retreats, it leaves behind these deposits, creating distinctive ridges and mounds.
The debris of boulders eroded and carried down by glaciers will eventually form moraines (mounds) where the front of the glacier melts and retreats, leaving the debris behind. Moraines can be high and wide enough to form a dam, behind which glacial melt water is trapped and lakes are formed.
Glacier erosion is when the ground below the glacier is removed. Glacial deposition is when the debris (eroded ground) is left behind when a glacier melts and the face retreats.