Answer:
See below
Explanation:
The lithosphere is largely made up of soil, minerals, and rocks—essentially the earth’s crust. One of the most important processes that takes place in the lithosphere is the rock cycle. In the rock cycle, the three major types of rocks—igneous, sedimentary, and metamorphic—are created and destroyed through various earth activities. Igneous rocks are formed through the cooling and crystallizing of molten rock. Metamorphic rocks form when heat and pressure are added to other rocks. Weathering, erosion, and deposition are the activities that create sedimentary rock, such as coal which is created over thousands of years. Alternately, an earthquake changes the lithosphere instantaneously. A sister to the lithosphere, the hydrosphere contains the liquid parts of the earth. All of Earth’s oceans and smaller bodies of water are a part of this system. The hydrologic cycle—often referred to as the water cycle—continuously moves water on, above, and below the earth’s surface. This movement of water can create an interaction between the hydrosphere and the lithosphere. As water moves through the cycle, rocks and soil are moved as well, often being deposited. These deposited materials may form sedimentary rocks, thus showing how one earth system can have an impact on another. The cryosphere is an even closer relative to the hydrosphere than the lithosphere. The cryosphere consists of all frozen water on the earth. Frozen water makes up about 75 percent of the earth’s fresh water. This makes it clear that the activities of the hydrosphere and cryosphere are closely related with water being frozen in the cryosphere, then thawed into the hydrosphere. Glaciers are the largest feature of the cryosphere, with some spanning hundreds of miles. For the atmosphere, the system changes from water to air. The atmosphere is the thin layer of gasses surrounding the planet. The atmosphere is responsible for the many climates of the earth. The weather, which can change suddenly from no rain to rain, is also a product of the atmosphere; however, the interaction among the spheres is again evident, since the hydrosphere provides the water that enters the atmosphere as water vapor before eventually falling as rain. The biosphere includes all living organisms, from the bottoms of the oceans to the upper reaches of the atmosphere. Though it is identified separately from the other systems, the biosphere is perhaps the most interactive of all the systems. The organisms of the biosphere live in each of the other spheres. For example, breathing impacts the atmosphere with the introduction of carbon dioxide.
