Geography High School

examine the images of the grand canyon below. notice that most of the canyon consists of layers of sedimentary rocks, but if you were to hike down into the inner gorge you would encounter the vishnu schist, a metamorphic rock. which of the following processes were involved as the vishnu schist metamorphosed? photograph a shows the grand canyon the inner gorge of the grand canyon, a steep gorge in the deepest part of the canyon with a river at its bottom. photograph b shows the vishnu schist, a dark colored rock outcrop jutting out from one side of the inner gorge. view available hint(s)for part a examine the images of the grand canyon below. notice that most of the canyon consists of layers of sedimentary rocks, but if you were to hike down into the inner gorge you would encounter the vishnu schist, a metamorphic rock. which of the following processes were involved as the vishnu schist metamorphosed? photograph a shows the grand canyon the inner gorge of the grand canyon, a steep gorge in the deepest part of the canyon with a river at its bottom. photograph b shows the vishnu schist, a dark colored rock outcrop jutting out from one side of the inner gorge. eruption and cooling of a lava flow. intense pressure due to regional metamorphism. deposition, burial, compaction, and cementation of sediment. cooling of magma.

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Answer 1

The following processes were involved as the vishnu schist metamorphosed photograph b shows the vishnu schist, a dark colored rock outcrop jutting out from one side of the inner gorge eruption and cooling of a lava flow.

The Vishnu Schist found in the inner gorge of the Grand Canyon was formed through intense pressure due to regional metamorphism. This is different from the sedimentary rocks found in the rest of the canyon, which are formed through deposition, burial, compaction, and cementation of sediment. Eruption and cooling of a lava flow and cooling of magma are not processes that were involved in the metamorphosis of the Vishnu Schist.

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Related Questions

What are gases that accumulate in the atmosphere and contribute to global warming?

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The gases that accumulate in the atmosphere and contribute to global warming are known as greenhouse gases. They trap heat from the sun and cause the Earth's temperature to increase.

What is global warming?

Global warming refers to the phenomenon of Earth's average surface temperature increasing due to human activities that increase the concentration of greenhouse gases in the atmosphere. Greenhouse gases such as carbon dioxide, methane, and water vapor trap heat in the Earth's atmosphere, causing global temperatures to rise. This is referred to as the greenhouse effect.

What is the greenhouse effect?

The greenhouse effect is a natural process that occurs when certain gases in the Earth's atmosphere, referred to as greenhouse gases, trap heat from the sun, preventing it from escaping into space. As a result, the Earth's temperature is kept within a range that is conducive to life as we know it.

However, human activities such as burning fossil fuels, deforestation, and industrial processes have led to an increase in the concentration of greenhouse gases in the atmosphere, intensifying the greenhouse effect and causing global warming. This is a significant concern, as global warming can have a range of negative impacts on the environment and human societies.

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what volcanic eruption was the loudest in modern history?

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Answer:

Explanation:

The loudest volcanic eruption in modern history was the 1883 eruption of the Krakatoa volcano, which is located between the islands of Java and Sumatra in Indonesia. The explosion was so powerful that it was heard over 3,000 miles away, and it produced a sound that is estimated to have reached 172 decibels at a distance of 100 miles from the source. The eruption caused widespread damage and loss of life, with tsunamis and other effects felt across the region.

The Aleutian and Hawaiian Islands form from completely different processes related to Plate Tectonics. Using Plate Tectonic theory and correct technical terms, explain how they form.

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The Aleutian and Hawaiian Islands form from two different processes related to Plate Tectonics. The Aleutian Islands are formed by the subduction of the Pacific plate beneath the North American plate at the Aleutian Trench. This process is also known as a convergent plate boundary.

During subduction, the oceanic lithosphere is consumed and in the process magma is produced and rises to the surface. This magma then cools and hardens to form the Aleutian Islands.

The Hawaiian Islands are formed by a process known as hotspot volcanism. Hotspots are stationary mantle plumes that rise from the mantle and melt the lithosphere.

This process is also known as a divergent plate boundary. The Hawaiian hotspot is located beneath the Pacific plate and has created the Hawaiian Ridge of islands, as the Pacific plate has moved over it.

The molten material erupts to the surface to create new volcanoes and as the older volcanoes move away from the hotspot, they become inactive and form islands.

Both processes create volcanic islands, but the way in which the volcanoes form differs between the Aleutian and Hawaiian Islands. The Aleutian Islands are formed through subduction while the Hawaiian Islands are formed through hotspot volcanism.

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