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MTTC Earth/Space Science (020) Practice Tests & Test Prep by Exam Edge - Review



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MTTC Earth/Space Science - Reviews


   Excellent
Based on 145 reviews

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"The questions weren't even close to what was asked on the MTTC 056 exam. Very disappointed and a waste of my money."

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See why our users from 154 countries love us for their exam prep! Including 145 reviews for the MTTC Earth/Space Science exam.

Exam Edge is an industry leader in online test prep. We work with institutional partners to offer a wide array of practice tests that will help you prepare for your big exam. No matter how niche your field of interest might be, we're here to help you prepare for test day.

   Excellent -- Based on 145 reviews

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MTTC Earth/Space Science - Test Reviews Sample Questions

There are several mechanisms that can cause mountain-building. All the processes that form mountain ranges are called:

Correct Answer:
orogeny.
the process responsible for the formation of mountain ranges is known as orogeny. this geological phenomenon involves the structural deformation of the earth's crust and uppermost mantle due to tectonic forces that cause the land to be pushed up, forming mountains. these tectonic forces typically arise from the movements and interactions of earth's lithospheric plates, such as convergence, where two plates move towards each other, often leading to one plate being forced over or beneath another. this can result in the folding, faulting, and uplift of rock layers.

isostasy, on the other hand, refers to the gravitational equilibrium between the earth's lithosphere (the crust and the upper part of the mantle that makes up the tectonic plates) and the asthenosphere (the denser, viscous layer beneath the lithosphere). the principle of isostasy is crucial in understanding how the earth's crust maintains its balance over time, especially after orogenic events have altered the surface, such as through the formation of mountain ranges. when the crust is thickened by mountain building, it will eventually reach a state of isostasy by thickening and extending deeper into the mantle.

it is important not to confuse orogeny with ontogeny or oscillation, as these terms relate to entirely different concepts. ontogeny refers to the development of an individual organism from embryo to adult, tracing out the various stages of morphological transformations in its life cycle. oscillation, conversely, describes a movement back and forth at a regular speed, commonly used in physics to describe wave movements or the periodic motion of objects.

in summary, orogeny is the correct term when discussing the processes that lead to the formation of mountain ranges, involving complex interactions and movements of the earth's crust driven by tectonic forces. isostasy plays a supporting role in maintaining the balance of the crust post-orogeny, whereas ontogeny and oscillation are unrelated to geological mountain-building processes.