Answer:
17,190 years
Explanation:
Each isotope has a characteristic half-life, which is the time required for half of that isotope to decay. After one half-life has elapsed, 50% of the isotope has decayed and 50% remains. After two half-lives, 75% has decayed and 25% remains. After three half-lives, 87.5% has decayed and 12.5% remains. For carbon-14, which has a half-life of 5,730 years, three half-lives corresponds to 17,190 years.
soft clay and wet and sandy soil as they are more likely to collapse or corrode over time especially the wet and sandy soil which will erode with rain or water
Answer:
Eastern Coast of the US, Western coast of Europe and upwards to the polar region
Explanation:
The two images explain clearly that the currents help contribute to warm water, and shown in the second infographic, it says that it brings that water towards the areas listed above. Even without that second picture, we can conclude that it at least goes around north Eastern coast of the US and West Europe as seen by the Gulf Stream current's projection based on arrows.
Answer:
there's a few processes I've learned of that creates landforms.
Events such as landslides, floods, and other natural changes in nature can cause land to change shape.
Physical weathering and erosion also can cause land formation. The rocks that break down changes the shape of land.
Explanation:
Answer:
Transform Boundaries — Grinding Plates
This kind of boundary results in a fault — a crack or fracture in the earth's crust that is associated with this movement.
Explanation:
