Isostasy is the balance between the weight of the Earth's crust and the underlying mantle. When crustal material is added, it depresses the underlying mantle, creating an upward force that pushes the crust back up. Similarly, when material is removed, the mantle rebounds and pushes the crust down. This force-balance maintains the equilibrium of the Earth's crust.
why can you only only photograph a lunar eclipse somtimes
outline the negative impact of drought on the farmers of South Africa
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Explanation:
is The loss of natural habitat for animals and insects cost or benefit
The loss of natural habitat for animals and insects is cost because it is like a danger to the ecosystem .
What is the effect of habitat loss?Habitat loss, can be described as the removal of plants as well as the trees that helps in the process of the stabilizatio of the soil, which bring about the increase in the erosion, as well as fading away the nutrient levels in terrestrial ecosystems.
It should be noted that this can bring about the decrease agricultural productivity. and can bring about the biodiversity as well as negatively impact the ecosystem
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Look at the description of the Sherburne. How was the distance to/ from the shore of the sea changing in the area as the Sherburne was being deposited?
Why are there no fossil ferns or primitive pine trees
Answer from your tutor:
The Sherburne formation is starting to become sandier the closer you get to the top because the shore is starting to transition to sandstone.
How did the distance to/from the shore change as Sherburne was deposited?The Sherburne formation refers to sequence of sedimentary rocks that was deposited in the Late Cretaceous period in what is now Montana and Wyoming which is thought to have been deposited in a shallow marine environment with the shoreline fluctuating over time.
As the Sherburne was being deposited, the distance to/from the shore of the sea was changing in the area. At the bottom of the formation, the sediment is composed of finer-grained rocks such as shale and mudstone which indicate a more offshore environment.
But as you move up the formation, the sediment becomes coarser with the sandstone and conglomerate becoming more prevalent which suggests that the shoreline was moving closer and the area was becoming shallower.
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