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Earth’s Structure,[object Object]
Crust,[object Object],There are two different crusts on our planet, the continental and the oceanic. ,[object Object],The continental crust is the thicker crust, made of land, which is made up of silicon,aluminum, and oxygen. It is also less dense than oceanic crust.,[object Object],The oceanic crust is the thinner crust made up of water, and is denser than the continental crust.It is also made up of silicon, aluminum, and oxygen.,[object Object]
Oceanic Crust,[object Object]
Continental Crust,[object Object]
Mantle,[object Object],This is the thickest layer of the Earth containing most of its mass.No one has ever been to the mantle because they can’t drill through the crust, and the heat is to hot to bear.,[object Object],Scientists have figured out that magma pushes out from the mantle and has to be at the bottom of the ocean.,[object Object]
Mantle,[object Object]
Asthenosphere,[object Object],This is the soft layer of the mantle on which tectonic plates move.It is made up of solid rock that flows very slowly.,[object Object]
Lithosphere,[object Object],This is the solid outer layer of the Earth that consists of the crust , and the rigid upper part of the mantle.The lithosphere is divided into pieces called tectonic plates.,[object Object]
Lithosphere,[object Object]
Outer Core,[object Object],This is the liquid layer of the Earth’s core. This lies beneath the mantle and surrounds the inner core.,[object Object]
Inner Core,[object Object],This is the solid dense center of our planet that extends from the bottom of the outer core to the center of the Earth which is the hottest on our planet.,[object Object]
Continental Drift,[object Object],This is the hypothesis that states that the continents once formed a single landmass, broke up, and drifted to their present locations.,[object Object],Pangea, a super continent, broke apart from each other to their present locations.Wegener,a scientist could never get it approved.,[object Object],Glossopteris, an ancient plant, has been found on all continents proving Wegener’s hypothesis.,[object Object],He also proved continental drift with sea-floor-spreading and plate tectonics.,[object Object]
Continental Drift,[object Object],Wegener proved continental drift because of geologic, fossil, and climate evidence.,[object Object],Geologic evidence- the evidence of how all the shore lines and mountain ranges are lined up.,[object Object],Fossil evidence- the evidence in where the fossils are found. Example: Glossopteris,[object Object],Climate evidence- the evidence that the climate has changed.,[object Object]
Continental Drift,[object Object]
Geologic Time,[object Object],Geologic time has been classified into three different parts. Cenozoic, Paleozoic, and Mesozoic.,[object Object],Cenozoic is the era we live in. It is sometimes referred to it as the “ Age of the Mammals”.,[object Object],Paleozoic is the first era. It was the age of animals. It is also the longest era.,[object Object],Mesozoic is the middle era. It was when the dinosaurs roamed the Earth.,[object Object]
Earth5jlorenz
Era vs. Epoch vs. Period,[object Object],Eon is the largest division of geologic time.,[object Object],Era, the second largest time period, usually consists of two or more periods.,[object Object],Period, the third largest time period, is a unit of geologic time which eras are divided.,[object Object],Epoch, is the smallest division of geologic time.,[object Object]
Earth5jlorenz
Fossils,[object Object],There are many types of fossils, but the major ones are the trace fossils and index fossils.,[object Object],Trace fossils- the mark that is formed in soft sediment by the movement of an animal.,[object Object],Index fossil- a fossil that is found in the rock layers of one geologic age.,[object Object]
Earth5jlorenz

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