Arrange the layers and fault line from youngest to oldest

Geography

2 answers:

Harrizon [31]2 years ago

6 0

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.

Mazyrski [523]2 years ago

3 0

Answer:

E-D-C-B-F-A

Explanation:

The top layer is clearly shown as not being cut by the fault line and leveled

You might be interested in

What current brings water to the coasts of Europe

Lena [83]

What is 96 divided by 6

5 0

2 years ago

Read 2 more answers

Would earthquakes occur at a depth of over 700 kilometers? why or why not

neonofarm [45]

Earthquakes can occur at depths of over 700 km.

Explanation:

The earthquakes are a natural hazard which is associated with boundaries of the tectonic plates. The majority of the earthquakes occur at convergent and transforming plate boundaries. The reason as to why the earthquakes occur at these places is because of the pressure between the colliding or sliding plates, where the crust cracks and during the adjustment the force created is manifested with strong vibrations.

In general, the earthquakes occur at depths between 20 and 50 km, which is usually the depth where the plates create the most pressure upon each other. That is not to say that that is the only range where earthquakes occur, as they can occur anywhere from the surface of Earth and down to 800 km in depth. With other words, the earthquakes occur anywhere from the top of the lithosphere to the top of the astenosphere. Earthquake hot-spots are: