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... Intelligent Design Intelligent Design used by both the Media & Young Earth Advocates Since a “Young” Earth required discarding all Scientific evidence, it cannot be either intelligent or by Design. Dbeau 2008 “If young earth is true, it is the most cruel joke that a so-called benevolent Creator coul ...
Changing Earth - Ms. Stinson's Science Class
Changing Earth - Ms. Stinson's Science Class

... one another. When the plates interact, the result of their movement is seen at the plate boundaries , as in the figure above. Movement along any plate boundary means that changes must happen at other boundaries. What is happening to the Atlantic Ocean floor between the North American and African Pla ...
Plate Tectonics
Plate Tectonics

... Chapter 3: Key Concepts Some seismic waves–energy associated with earthquakes–can pass through Earth. Analysis of how these waves are changed, and the time required for their passage, has told researchers much about conditions inside Earth. Earth is composed of concentric spherical layers, with the ...
The Structure of the Earth and Plate Tectonics
The Structure of the Earth and Plate Tectonics

... mostly focused at plate ...
Chapter 8 The Moon and Mercury
Chapter 8 The Moon and Mercury

... 8.8 The Origin of the Moon Current theory of Moon’s origin: Glancing impact of Mars-sized body on the still-liquid Earth caused enough material, mostly from the mantle, to be ejected to form the Moon Computer model ...
Name
Name

... The Earth’s lithosphere is made of a number of solid pieces , called ____________ which move in relation to each other. These plates are “riding” on a more “plastic molten” layer below. This layer is called the ASTHENOSPHERE. The evidence shows that approximately _______ million years ago, the major ...
A new Paradigm… Plate Tectonics
A new Paradigm… Plate Tectonics

... ridge dividing the North Atlantic. This was a controversial assertion during the decadeslong debate over continental drift. ...
science - Amazon Web Services
science - Amazon Web Services

... The three main categories of rock in the earth’s crust are igneous, sedimentary, and metamorphic. Igneous rocks were originally molten; then they were crystallized by cooling. Sedimentary rocks were laid in place by moving water, ice, or wind. Metamorphic rocks are rocks that were under enough press ...
Evidence after wegener: seafloor spreading and
Evidence after wegener: seafloor spreading and

... • this proved that oceanic crust is created at different times, supporting seafloor spreading ...
Powerpoint Presentation Physical Geology, 10th ed.
Powerpoint Presentation Physical Geology, 10th ed.

... The best estimate for Earth's age is ~4.6 billion years (same as age of our Solar System, as indicated by meteorites). Historically, there has been much debate over "how fast" geology happens with two different camps of thought: CatastrophismUniformitarianism- ...
First stop – the CRUST
First stop – the CRUST

... of iron and nickel. The silicates are much less dense than the metals. This separation occurred in the very early stages of the Earth’s formation, as heavier elements were pulled by gravity towards the center, and the lighter elements rose to the surface. ...
Organized Opposition to Plate Tectonics: The New Concepts in
Organized Opposition to Plate Tectonics: The New Concepts in

... on subjective, qualitative correlations, and has not been ground-truthed by radiometric dating, and that the stripe pattern is better explained by fault-related bands of rocks of different magnetic properties. They stress the need to drill all the way through the ocean crust and into the mantle befo ...
HERE
HERE

... plates apart and adding new material at their edges. • Most spreading zones are found in oceans; for example, the North American and Eurasian plates are spreading apart along the mid-Atlantic ridge. • Spreading zones usually have earthquakes at shallow depths (within 30 kilometers of the surface). • ...
ES Chapter 3 PPT
ES Chapter 3 PPT

... • Deep currents are streamlike movements of water that flow very slowly along the ocean floor. • Deep currents form when the cold, dense water from the poles inks below warmer, less dense ocean water and flows toward the equator. • The densest and coldest ocean water is located off the coast of Anta ...
which is integral in the stabilization of new continental crust, or by
which is integral in the stabilization of new continental crust, or by

... Crust formation must therefore occur in at least two stages,first, melting of the mantle to produce basaltic magma,and second,either fractional crystallization or re-melting of the basalt ultimately to produce the more evolved rocks of which continental crust is dominantly composed. The products of ...
Untitled
Untitled

... C) Aniakchak D) Stromboli 14. Most of the young mountains have their origin due to ______ activities. A) Folding B) Faulting C) Depositional D) Erositional 15. Binary star hypothesis of the earth’s origin was postulated by ________. A) Kant B) Laplace C) Russel D) Jeams 16. The lower limit of the c ...
Warm-Up - mssarnelli
Warm-Up - mssarnelli

... We will be doing a mini-lab with Milky Way bars to further demonstrate your understanding of plate tectonics and the features formed by plate movement. You must complete the lab guide and you must follow my instructions at all times! ...
RHV_Margins_Mini_Lesson.v8
RHV_Margins_Mini_Lesson.v8

... Answer: Not very far! We have only drilled into the Earth’s crust, and no more than 0.2% of the depth to the Earth’s center. No drill hole on continental or oceanic crust has reached the Earth’s mantle. Question: What, then, can we learn from scientific drilling? ...
Curriculum Map - Grade 09-12
Curriculum Map - Grade 09-12

... A. The Rock Record A1. State the principle of uniformitarianism A2. Explain how the law of superposition can be used to determine the relative age of rocks A3. Compare three types of unconformity A4. Apply the law of crosscutting relationships to determine the relative age of rocks A5. Summarize the ...
Dynamic Earth Curriculum Final
Dynamic Earth Curriculum Final

... composition. The outermost layer is the crust. It is the thinnest layer making up only about 1  percent of the Earth. The majority of the crust is comprised of elements like silicon (Si),  aluminum (Al), potassium (K), calcium (Ca), oxygen (O), sodium (Na) and minerals made of these  elements. The c ...
continent, continental drift, seafloor, ocean floor, tectonic
continent, continental drift, seafloor, ocean floor, tectonic

... 2. Earthquakes are formed when the boundaries of the lithospheric plates move against each other, building up pressure, then cause a sudden and often violent shift. This movement causes an earthquake. 3. Volcanoes are formed when plates move apart or collide. 4. When two plates collide, one plate is ...
Slide 1
Slide 1

... The subduction process: 1-new oceanic crust is hot, but as it moves away from the mid-ocean ridge it cools down and becomes more ...
Name Plate Tectonics Introduction Go to the following site: http
Name Plate Tectonics Introduction Go to the following site: http

... 12. Complete the Plates & Boundaries Challenge. Write down your score on the line below (I will totally believe your score and not count it against your grade! Promise) SECTION: Slip, Slide & Collide (click “see what happens at different plate boundaries”) ...
continental-drift-and-the-theory-of-plate-tectonics-fran-et-al
continental-drift-and-the-theory-of-plate-tectonics-fran-et-al

... The size of the earth was much smaller than it is today and so all continents were together as a single huge land mass (called Pangea) then and as earth continued grow in size all these continents looked like as if they are moving apart whereas they actually have just reached their current positions ...
Section 1: The Geosphere
Section 1: The Geosphere

... scoured by running water, which moves rocks around and changes their appearance. • Erosion is the process in which the materials of the Earth’s surface are loosened, dissolved, or worn away and transported form one place to another by a natural agent, such as wind, water, ice or gravity. • Erosion w ...
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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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