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Comparison of the rocky planets
Comparison of the rocky planets

... Venus ~1000x more than Earth Mars ~1/1000 of Earth atmospheric density decreases away from surface ...
Concept Review
Concept Review

... g. the layer of rock between Earth’s crust and core; denser than the crust h. the portion of Earth that is water i. the mostly solid, rocky part of Earth; extends from the center of the core to the surface of the crust j. a set of particles or interacting components considered to be a distinct physi ...
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...  ___The theory that states all continents were once a part of one giant landmass, split apart and slowly moved to there present positions.  ___The theory that Earth’s crust and upper mantle is broken up into sections.  ___The process that explains how continents move and where new crust is made. ...
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... Alfred Wegner hypothesized that continents move. What did he call this? __________________________ 2. The ________________________ is located directly under the lithosphere. This is a layer of hotter and softer rock in the mantle. 3. The switch in the Earth’s magnetic field is called: ______________ ...
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... 1. Apply the concepts learned in the chapter to a model of Earth’s interior. 2. Interpret data to make a model to scale. 3. Design and make a model of Earth’s interior and features of the surface. 4. Communicate the features of the model in a presentation to the class. ...
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... 1. Oceanic crust – under ______________, 4-7 km thick (high density) 2. _____________________ crust – under continents, ___-____ km (lighter in density) ...
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... Earth’s crust consists of major and minor tectonic plates that move relative to each other. A combination of constructive and destructive geologic processes formed Earth’s surface. Evidence of the dynamic changes of Earth’s surface through time is found in the geologic record. ...
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... Chacko, Reimink spent his summers in the field collecting rock samples from the Acasta Gneiss Complex, which was discovered in the 1980s and found to contain some of the Earth's oldest rocks, between 3.6 and four billion years old. Due to their extreme age, the rocks have undergone multiple metamorp ...
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... The soft layer of the mantle on which the lithosphere floats What parts something is made up of The transfer of heat by one substance to another by direct contact of particles of matter The transfer of heat by movements of fluids The layer of rock that forms Earth’s surface The movement of energy fr ...
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Layers of the Earth Vocabulary

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... 4. Ancient northern hemisphere supercontinent.[8] 6. Ancient original supercontinent.[7] 7. Type of volcano that has not erupted for some time but will erupt again.[7] 9. Rock formed from cooled lava.[6] 11. Point on earth's surface directly above the focus of a quake.[9] 12. Large earth break.[5] 1 ...
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History of Earth



The history of Earth concerns the development of the planet Earth from its formation to the present day. Nearly all branches of natural science have contributed to the understanding of the main events of the Earth's past. The age of Earth is approximately one-third of the age of the universe. An immense amount of biological and geological change has occurred in that time span.Earth formed around 4.54 billion years ago by accretion from the solar nebula. Volcanic outgassing probably created the primordial atmosphere, but it contained almost no oxygen and would have been toxic to humans and most modern life. Much of the Earth was molten because of frequent collisions with other bodies which led to extreme volcanism. One very large collision is thought to have been responsible for tilting the Earth at an angle and forming the Moon. Over time, the planet cooled and formed a solid crust, allowing liquid water to exist on the surface.The first life forms appeared between 3.8 and 3.5 billion years ago. The earliest evidences for life on Earth are graphite found to be biogenic in 3.7-billion-year-old metasedimentary rocks discovered in Western Greenland and microbial mat fossils found in 3.48-billion-year-old sandstone discovered in Western Australia. Photosynthetic life appeared around 2 billion years ago, enriching the atmosphere with oxygen. Life remained mostly small and microscopic until about 580 million years ago, when complex multicellular life arose. During the Cambrian period it experienced a rapid diversification into most major phyla. More than 99 percent of all species, amounting to over five billion species, that ever lived on Earth are estimated to be extinct. Estimates on the number of Earth's current species range from 10 million to 14 million, of which about 1.2 million have been documented and over 86 percent have not yet been described.Geological change has been constantly occurring on Earth since the time of its formation and biological change since the first appearance of life. Species continuously evolve, taking on new forms, splitting into daughter species, or going extinct in response to an ever-changing planet. The process of plate tectonics has played a major role in the shaping of Earth's oceans and continents, as well as the life they harbor. The biosphere, in turn, has had a significant effect on the atmosphere and other abiotic conditions on the planet, such as the formation of the ozone layer, the proliferation of oxygen, and the creation of soil.
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