A. Age of the rock. This doesn't matter, it could be 7 billion years old, but still stable.
Short Answer:
buoyancy
Long answer:
An object submerged in water displaces water according to how much it weighs. In fact, the water will push upward against the object with a force equal to the weight of the water it displaces. For example, a bowling ball and a beach ball that are the same size will have the same volume. The bowling ball, however, is more massive and thus denser than the beach ball. In both cases, the water pushes up against the ball with a force equal to the weight of water it displaced. In the case of the bowling ball, it weighs more than the amount of water it displaced, so it sinks. The beach ball, however, displaces very little water and the air inside it is much lighter than the weight of the water it displaced, so it floats.When lifting something underwater, you have the help of water pushing the object upwards along with your own strength, which is why it's easier to pick up things underwater than on land.
Source:
https://www.wonderopolis.org/wonder/why-is-it-easier-to-lift-someone-in-water-than-on-land
Most divergenr boundaries occur along the mid ocean ridges where sea floor spreading occurs. divergent boundaries also occur on land. When a divergent boundary develops on land, two of earth's plates slide apart. A deep valley called a rift valley form along the divergent boundary.
Answer:
A, B, F, C, D, E.
Explanation:
A fault line is a break or fracture in the ground that occurs due to the discontinuity of the larger rocks mass and thus is due to the significant displacement of the rocks in the geologic crust.
As the youngest layer is found at the surface and the older layer is founded at the bottom the oldest will tose of the igneous rocks and the youngest will be those of the sedimentary rocks. The faults are composed of the mineral contents like the quartz, feldspar, and clay. And have an abundant of illite and the chlorite minerals.
The quantitative assessment of the vertical slip area of the fault gives in the estimation of the fault angles are called as the piercing points. The example of the rocky mountains of the Himalayan orogeny and those of that are formed by the granitic rocks and the genesis.
