Answer:
Non-conformity
Explanation:
An unconformity is a time gap or break in stratigraphic record of sedimentary rock layers. It is usually depicted by a period of non-deposition or erosion.
There are different types of unconformity:
>Disconformity
>Non-conformity
>Para-conformity
>Angular unconformity
Non-conformity is a type of unconformity marked by different rock types. The boundary between such rock types is an unconformity surface. For example, the boundary between an igneous rock that caps a sedimentary sequence is an unconformity.
They were loosing their lands that's why we can choose a) weak leadership
This geological process is called Mantle drag .
What is Mantle drag?
According to the first driving mechanism, known as mantle drag, plate motion is the consequence of viscous drag brought on by the lateral motion of the tops of mantle convection cells in the asthenosphere on the base of the lithosphere . Convection cells would thus be mostly absent beneath continents, rising beneath oceanic ridges, and dropping beneath trenches. This idea states that the oceanic lithosphere would be in a state of tension at the ocean ridges and compression at the trenches.
Due to their connection to accretive and destructive plate boundaries, the horizontal widths of the convection cells causing mantle drag would be projected to be around half an ocean's breadth, or 3000 km.
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Answer: the task demands
Explanation:
According to Land and Hayhoe, thee most important factor in determining fixations when a person is making a peanut butter sandwich is the task demands.
It should be noted that the stimulus colors, orientations or the stimulus contrast levels isn't the appropriate answer.