Central Idea and Supporting Details - Mt. Everest-

What is the central idea of the text?

• Mount Everest is formed only by volcanic activity.

• Mount Everest’s geology helps scientists study Earth’s tectonic history.

• The highest peak of Mount Everest is the most important feature.

• The collision of the Indian and Eurasian plates is the only important geological event.

How was the Himalayan mountain range, including Mount Everest, formed?

• By volcanic eruptions.

• Through the collision of the Indian Plate with the Eurasian Plate.

• By erosion caused by glaciers.

• Through ancient sea deposits.

Which type of rocks make up most of Mount Everest’s geology?

• Sedimentary rocks like limestone.

• Metamorphic rocks like gneiss and schist.

• Igneous rocks like basalt.

• Volcanic rocks like pumice.

How were the metamorphic rocks on Mount Everest formed?

• By cooling from lava.

• Through intense heat and pressure deep within the Earth’s crust.

• By erosion and weathering of older rocks.

• By chemical reactions in the air.

What role does the collision of tectonic plates play in the formation of Mount Everest?

• It causes volcanic eruptions.

• It pushes rocks from the Earth’s crust to the surface, creating the mountain.

• It causes the mountain to sink.

• It melts the rocks deep beneath the surface.

What type of sedimentary rock can be found on Mount Everest?

• Gneiss

• Slate

• Limestone

• Schist

Why is Mount Everest considered an important site for studying plate tectonics?

• It is a place where scientists can study active volcanoes.

• Its diverse geology provides insight into Earth’s tectonic activity and history.

• It is the only mountain in the world made of metamorphic rocks.

• It has the largest collection of fossils on Earth.

Which of the following is true about the geology of Mount Everest?

• It is made only of igneous rocks.

• It has no sedimentary rocks.

• It provides valuable information about tectonic forces and Earth’s history.

• It was formed entirely by the erosion of older mountains.