alpine natural sciences academy mr. bordelon, m.s. the structure of the earth

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Alpine Natural Sciences Academy Mr. Bordelon, M.S. The Structure of the Earth

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W hat The Model Tells Us. The model helps scientists explain many geological events such as earthquakes, volcanoes, the movement of continents, etc.

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Page 1: Alpine Natural Sciences Academy Mr. Bordelon, M.S. The Structure of the Earth

Alpine Natural Sciences AcademyMr. Bordelon, M.S.

The Structureof the Earth

Page 2: Alpine Natural Sciences Academy Mr. Bordelon, M.S. The Structure of the Earth

Current Scientific ModelScientists currently believe that the Earth is

composed of four layers:

Crust Mantle Outer Core Inner Core

Page 3: Alpine Natural Sciences Academy Mr. Bordelon, M.S. The Structure of the Earth

What The Model Tells Us.

The model helps scientists explain many geological events such as earthquakes, volcanoes, the movement of continents, etc.

Page 4: Alpine Natural Sciences Academy Mr. Bordelon, M.S. The Structure of the Earth

CrustThin silicate rock material.

The crust is the outermost layer of rocks making up the solid Earth. It is distinguished from the underlying mantle rocks by its composition, lower density, and the lower velocity at which it conducts seismic energy.

Page 5: Alpine Natural Sciences Academy Mr. Bordelon, M.S. The Structure of the Earth

The crust lays above the mantle and is the earth's hard outer shell, the surface on which we are living. In relation with the other layers the crust is much thinner. It floats upon the softer, denser mantle. The crust is made up of solid material, but is not the same thickness everywhere. There is an Oceanic crust and a Continental crust. The first one is about 4-7 miles (6-11 km) thick and consists of heavy rocks, like basalt. The Continental crust is thicker than the Oceanic crust, about 19 miles(30 km) thick. It is mainly made up of light material, like granite.

Page 6: Alpine Natural Sciences Academy Mr. Bordelon, M.S. The Structure of the Earth

MantleDense and mostly solid silicate rock.

The region just below the crust and extending all the way down to the Earth's core is called the mantle. The mantle is relatively flexible so it flows instead of fracturing.

Page 7: Alpine Natural Sciences Academy Mr. Bordelon, M.S. The Structure of the Earth

The layer above the core is the mantle. It begins about 6 miles(10 km) below the oceanic crust and about 19 miles(30 km) below the continental crust. The mantle is to divide into the inner mantle and the outer mantle. It is about 1,800 miles(2,900 km) thick and makes up nearly 80 percent of the Earth's total volume.

Page 8: Alpine Natural Sciences Academy Mr. Bordelon, M.S. The Structure of the Earth

Outer CoreA liquid molten core of nickel and iron.

Beneath the mantle is the Earth's core. The Earth's core consists of a fluid outer core. Because the outer core contains iron, when it flows it generates a magnetic field. This is the source of the Earth's magnetic field.

Page 9: Alpine Natural Sciences Academy Mr. Bordelon, M.S. The Structure of the Earth

The inner part of the earth is the core. This part of the earth is about 1,800 miles (2,900 km) below the earth's surface. The core is a dense ball of the elements iron and nickel. It is divided into two layers, the inner core and the outer core. The inner core - the center of earth - is solid and about 780 miles (1,250 km) thick. The outer core is so hot that the metal is always molten, but the inner core pressures are so great that it cannot melt, even though temperatures there reach 6700ºF (3700ºC). The outer core is about 1370 miles (2,200 km) thick. Because the earth rotates, the outer core spins around the inner core and that causes the earth's magnetism.

Page 10: Alpine Natural Sciences Academy Mr. Bordelon, M.S. The Structure of the Earth

Inner CoreSolid metal core made up of nickel and iron.

The Earth's little understood inner core is a frozen yet white hot globe of curiously laid out iron crystals, spinning independently of the rest of the planet.

Page 11: Alpine Natural Sciences Academy Mr. Bordelon, M.S. The Structure of the Earth

ATMOSPHEREThe earth is surrounded by all kind of gases. This

layer is called the earth's atmosphere. Without these atmosphere life on earth isn't possible. The atmosphere gives us air, water, warmth and is protecting us against harmful rays of the sun and against meteorites. This layer around the earth is a colorless, odorless, tasteless 'sea' of gases, water and fine dust. The atmosphere is made up of different layers with different qualities. It consists of 78% nitrogen, 21% oxygen, 0,93% argon, 0,03% carbon dioxide and 0,04% of other gases. The Troposphere is the layer where the weather happens, above this layer is the Stratosphere. Within the Stratosphere is the Ozone layer, that absorbs the Sun's harmful ultraviolet rays. Above the Stratosphere is the Mesosphere, the Thermosphere - in which the Ionosphere - and the Exosphere. The atmosphere is about 500 miles (800 km) thick.

Page 12: Alpine Natural Sciences Academy Mr. Bordelon, M.S. The Structure of the Earth

Influence of the Sun and MoonThe sun and the moon both have their

influence on the earth. Sometimes they cooperate and sometimes they counteract each other. Such influences are: the gravity, the warmth of the sun, the sunlight and the chronology. Through the gravitational force of the earth the moon orbits the earth. The moon also gravitates the earth, but less powerful. By the way gravity pulls the Earth and Moon toward each other, tides are caused (high tide and low tide). The sun also has some influence here. The sun brings light and is also responsible for the warming up of the earth.

Page 13: Alpine Natural Sciences Academy Mr. Bordelon, M.S. The Structure of the Earth

Earth: More than meets the eyes!