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We tend to think about the environment and sea as liquids in consistent movement, and of the Earth as a strong. However, investigations of the earth have demonstrated the structure of our planet is in truth anything besides static. It is a continually moving framework. Rocks move, erosion happens constantly, and plates that shape the planet's covering shift, all bringing on seismic tsunamis and earthquakes. The mantle of the Earth sags under the weight of the highest mountains, and recovers as those mountains erode. Solid rock melts, it’s lighter elements rise and heavier ones sink. The fluid material of lava moves in currents deep under the Earth.
Some of the planet’s incredibly intense heat is left over from its original formation. Radioactive material in the heart of the planet also creates extremely hot temperatures. In Hawaii, heat comes from mantle rock that has melted, forming magma--molten rock that is still underground. Once magma erupts to the surface, it is called lava. When lava hardens, or magma hardens underground, it is called igneous rock. Our planet has a solid inner core, believed to be made up of high percentages of iron and nickel. The inner core, about 1,500 miles in diameter, is surrounded by a fluid outer core. The temperature of the molten outer core registers some 7,000 degrees Fahrenheit. The combined core: inner and outer is hotter than the surface of the sun. And it is under incredible pressure from all the layers of material around it, which are pressing down under the influence of gravity. Molten rock heats up deep in the Earth, but its melting temperature changes with pressure. The higher the pressure, the more heat is required to change rock from a solid to liquid state.
Most volcanoes are found at meeting points of the Earth’s tectonic plates. Imagine the pattern on a soccer ball-that is how the earth is divided. Tectonic plate theory is fairly recent, having been developed in the 1960s. The Hawaiian Island chain played a major role in the formation of the theory. Geologists noted that Hawai‘i is a long line of peaks, and originally they believed all the islands appeared at roughly the same time, arising from some kind of geologic rift. But more recent geological work has indicated that the oldest islands are at the far northwest end of the chain, and the youngest are at the southeast, near the Island of Hawai‘i. They also noticed the same pattern on two other island groups on the Pacific plate. All three chains, though hundreds or thousands of miles apart, form lines that run parallel to each other. As the theory goes, each chain was developing over a “hot spot,” where magma melts through the crust to create volcanoes.
The Pacific Plate is just one of several that cover the Earth’s surface. Some geologists count seven large plates and at least two dozen smaller ones. Among the major ones is the North American Plate, which includes all of North America and about half of the North Atlantic Ocean. The South American Plate has most of South America and approximately half the South Atlantic. A single plate accounts for most of Asia and Europe, there is one for Africa, and one that forms Antarctica. Australia lies on the last major plate, which includes parts of the Indian Ocean and the western South Pacific.
Earth's structural plates are isolated by splits in the planet's covering, and they advance toward or far from each other. The focus where the plates meet are the absolute most topographically dynamic places on Earth. The periphery of the Pacific Plate is some of the time called the Ring of Fire, for the quantity of dynamic volcanoes that exist along the limit. Structural plates slide along the side in a few zones, as at the San Andreas Fault in California. In different zones they spread separated, leaving the mediating space to load with the lava that ascends from the Earth's mantle. There is additionally zones where two plates are pushed into each other, one sliding up over another while the lower plate is driven once more into the mantle. The Hawaiian problem areas contains these type of zones