Because there are other wind directions to take it other places
The term "erosion" best describes how soil and rock pieces travel from one location to another.
Erosion in earth science refers to the activity of surface processes, such as wind or water currents, that shift rock, soil, or dissolved material from one area in the Earth's crust to another. The dynamic action of erosive elements including ice, water, snow, plants, wind, animals, and people causes this natural phenomenon.
Earthen materials are worn away during erosion, a geological process in which they are moved by wind or water. Water, ice, acids, salts, plants, animals, and temperature changes are some of the weathering agents. Erosion is the process by which the broken pieces of rock and mineral are carried away after a rock has been fractured.
Learn more about erosion:
brainly.com/question/3852201
#SPJ4
Answer:
The most recent eon is subdivided into three eras and eleven periods.
Explanation:
The geological time scale has been constructed so that it can help in better research and understanding of the past, as well as making it easier to distinguish the past and its characteristics at a certain time. There are larger and smaller divisions in the geologic time scale, with the eon being the largest unit, followed by era, and then period.
The most recent eon is the Paherozoic, starting from 542 million years ago and still going on. It is subdivided into three eras and eleven periods so far. The three eras are:
- Paleozoic
- Mesozoic
- Cenozoic
The eleven periods are:
- Cambrian
- Ordovician
- Silurian
- Devonian
- Carboniferous
- Permian
- Triassic
- Jurassic
- Cretaceous
- Tertiary
- Quaternary
The natural cycle that would have a direct effect of burning of fossil fuels would be the carbon cycle. <span>The </span>carbon cycle<span> is the biogeochemical </span>cycle<span> by which </span>carbon<span> is exchanged among the biosphere, pedosphere, geosphere, hydrosphere, and atmosphere of the Earth. Hope this answers the question.</span>
Isotope is the study and application of stable and radioactive isotopes to geological processes and their time scales.
