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Glacial ice is classified as a metamorphic rock, yet glaciers are a basic part of the hydrologic cycle. Should glaciers be considered a part of the geosphere or do they belong to the hydrosphere? Explain.

Short Answer

Expert verified
Glaciers belong to both the hydrosphere and the geosphere.

Step by step solution

01

Understand the Classification of Glaciers

Glaciers are large masses of ice formed from accumulated snowfall that compacts into ice over time. These masses are dynamic and capable of movement.
02

Define Geosphere and Hydrosphere

The geosphere refers to the solid earth, including rocks and sediments, while the hydrosphere encompasses all water bodies like oceans, lakes, rivers, and glaciers in any form.
03

Consideration as Part of the Hydrosphere

Since glaciers consist of frozen water, they are a significant part of Earth's water system, contributing to sea level changes and global water distribution. Thus, they are considered part of the hydrosphere due to their water content and dynamic role in the hydrologic cycle.
04

Consideration as Part of the Geosphere

On the other hand, glaciers are also considered part of the geosphere because they are formed from ice, which is a type of rock, specifically a metamorphic rock. Glacial processes influence the landscape by eroding and depositing sediments.
05

Conclude on Dual Classification

Given glaciers are both composed of water and influence earth's structure and sediment, they play roles in both spheres. Therefore, glaciers are part of both the hydrosphere and the geosphere, reflecting their dual nature as water bodies and rock formations.

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Key Concepts

These are the key concepts you need to understand to accurately answer the question.

The Hydrologic Cycle and Glaciers
The hydrologic cycle is a complex system that explains how water moves through the environment. It involves the processes of evaporation, condensation, precipitation, infiltration, and runoff. All these processes help distribute water from one place to another across the planet.

The role of glaciers in the hydrologic cycle is significant because they store vast amounts of fresh water. As glaciers melt, they release water back into the environment, which directly impacts sea levels and water supplies. This shows that glaciers are an integral component of the hydrosphere as they contribute to global water circulation. However, because glaciers are made of ice, they are also considered a metamorphic rock, creating a link to the geosphere.
  • Glaciers act as reservoirs of water influencing global water distribution.
  • Melting glaciers are key contributors to sea level changes.
  • They connect atmospheric processes through their role in precipitation and melting.
The Geosphere and Glaciers
The geosphere encompasses all the solid parts of the Earth, including rocks and soil. It forms a critical layer that supports the foundation for landscapes and habitats.

Glaciers, despite being composed of ice, are considered part of the geosphere due to their geological activity. Over time, glaciers shape landscapes through processes like erosion, transportation, and deposition. These processes can create features such as valleys, fjords, and moraines. This geological activity shows that glaciers are not only water bodies but also dynamic earth-shaping forces.
  • Glaciers are classified as metamorphic rocks because they change state under pressure and time.
  • Their movement and size heavily influence geological formations.
  • Glaciers' erosion capabilities help carve out new terrains over millions of years.
Defining the Hydrosphere
The hydrosphere includes all the water found on, under, and above the Earth's surface. This includes oceans, lakes, rivers, glaciers, and even underground aquifers.

Glaciers are a crucial component of the hydrosphere because they are predominantly made up of frozen water. In understanding how glaciers fit into the hydrosphere, it is vital to consider that they are significant resources of fresh water, influencing both global water systems and climate systems by storing and releasing water gradually.
  • The water content within glaciers plays a critical role in the overall water cycle.
  • They are pivotal in regulating Earth's temperature by reflecting sunlight.
  • The release of glacial meltwater can affect both marine and terrestrial ecosystems.
Understanding Metamorphic Rock
Metamorphic rocks are rocks that have been transformed due to pressure and temperature changes. Unlike igneous or sedimentary rocks, metamorphic rocks don’t melt but instead re-crystallize or change form under intense conditions.

Glacial ice falls into this category because it forms from the compaction and recrystallization of snow over hundreds or thousands of years—making it a unique kind of rock. Understanding glaciers as metamorphic rock highlights their role not only in water storage but also in geological processes, thus bridging the geosphere and hydrosphere concepts.
  • Metamorphic transformation involves changes in the structure and composition of the rock.
  • Glacier ice exhibits properties of metamorphic rock due to immense pressure over time.
  • The cycle of compaction and reformation in glaciers links them to geological processes.

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Most popular questions from this chapter

While taking a break from a hike in the Northern Rockies with a fellow geology enthusiast, you notice that the boulder you are sitting on is part of a large deposit of sediment that consists of a jumbled mixture of many different sediment sizes. Since you are in an area that once had extensive valley glaciers, your colleague suggests that the deposit must be glacial till. Although you know this is certainly a likely possibility, you remind your companion that material deposited by landslides can also consist of an unsorted mix of many sizes. How might you and your friend determine whether this deposit is actually glacial till?

Studies have shown that during the lce Age the margins of some ice sheets advanced southward from the Hudson Bay region at rates ranging from about 50 to 320 meters per year. a. Determine the maximum amount of time required for an ice sheet to move from the southern end of Hudson Bay to the south shore of present day Lake Erie, a distance of 1600 kilometers. b. Calculate the minimum number of years required for an ice sheet to move this distance.

For each of the statements below, identify the type of glacier that is being described. a. A glacier that is often described as continental. b. A glacier that forms when one or more valley glaciers spreads out at the base of a steep mountain. c. Greenland is the only example of this type of glacier in the Northern Hemisphere. d. A glacier that may also be called an alpine glacier. e. This glacier is a stream of ice leading from the margin of an ice sheet through the mountains to the sea.

If Earth were to experience another lce Age, one hemisphere would have substantially more expansive ice sheets than the other. Would it be the Northern Hemisphere or the Southern Hemisphere? What is the reason for the large disparity?

If the budget of a valley glacier were balanced for an extended span, what feature would you expect to find at the terminus of the glacier? Now assume the glacier's budget changes so that ablation exceeds accumulation. How would the terminus of the glacier change? Describe the deposit you would expect to form under these conditions.

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