Answer:
d. It also includes , breathing, digestion, swallowing
Answer:
Newer layers of earth form <u>on</u><u> </u><u>top</u> of older layers, so as we dig, we can see further back in time. Comparing the fossils between the layers can offer evidence of change.
<u>Phyletic</u><u> </u><u>gradualism</u> - slow, but constant gradual change; supported by transitional species in the fossil record
<u>Punctuated</u><u> </u><u>equilibrium</u>- long periods of no change followed by short periods of rapid change. Can also be supported by the fossil record when no transitional species are found.
A Rock Hyrax or Rock Rabbit are closely related to elephants As will as Dugong which a species of manatees
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Answer:</h2>
Settlement can be directly turned into <u>sedimentary rocks</u>.
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Explanation:</h2>
Sedimentary rocks are kinds of rocks that are framed by the collection or statement of little particles and ensuing cementation of mineral or natural particles on the sea floor or other places on the earth's crust. Sedimentation is the aggregate name for procedures that reason these particles to settle set up.
The particles that structure a sedimentary shake are called residue and might be made out of geographical or natural debris.