Answer:
A plateau is a raised, flat-surfaced area bound on one or more sides by cliffs or steep slopes.
Explanation:
Earth is a planet that has all sorts of different types of landforms. Some are enormous and occupy thousands of square km while some are very small and barely noticeable. One interesting landform that varries from medium to large size is the plateau.
The plateaus are flat or relatively flat areas that are on higher elevation. They differ in size, but also in elevation, and a plateau can be anywhere from 600 meters above sea level (like Pelagonija)to the highest ones that are above 4000 meters of elevation (like the Tibetan plateau). In some cases the plateaus are the highest landforms int heir surroundings and they bordered cliffs and steep slopes, in some cases it is a mixture of higher mountains on one side and cliffs and steep slopes on the other, and in some cases, they are fully surrounded by mountains, which is why people tend to confuse them with valleys if they are not very high.
Eurasian Plate moves north<span> 2 centimeters every one year. The Eurasian Plate is the third slowest moving plate, behind the </span>North American<span> and </span>South<span> American tectonic plates</span>
Answer:
The Moho is the boundary between the crust and the mantle in the earth. Also termed the Mohorovicic' discontinuity after the Croatian seismologist Andrija Mohorovicic' (1857-1936) who discovered it. The boundary is between 25 and 60 km deep beneath the continents and between 5 and 8 km deep beneath the ocean floor.
The Mohorovičić discontinuity usually referred to as the Moho discontinuity or the Moho, is the boundary between the Earth's crust and the mantle. It is defined by the distinct change in velocity of seismological waves as they pass through changing densities of rock.
The order in which the changes taking place in tectonic activity in the Martinsburg and Massanutten formation is:
- Erosion of the taconian mountains providing abundant carbonate sediment of the Massanutten formation.
- Taconian mountain building and the influx of siliciclastic sediment of the upper Martinsburg formation.
- Tectonic quiescence and the deposition of lime mud on carbonate platform of the upper Martinburg formation.
- Tectonic quiescence & the deposition of lime mud on carbonate platform of the Helderberg formation.
<h3>What order did the tectonic events happen?</h3>
As a result of the erosion of the teconian mountains, there was abundant carbonate for the Massanutten formation.
Some time later, a process of tectonic quiescence led to a deposition of lime mud on the upper Martinsburg formation, and then the Heiderberg formation.
Find out more on tectonic activity at brainly.com/question/16944828.
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