Venus - Sherry
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ihslVenus is the second planet from the Sun and is similar in size to Earth. It has a dense atmosphere composed primarily of carbon dioxide and rotates slowly in the opposite direction of Earth, with its day longer than its year. Venus was observed by ancient civilizations and remains the brightest object in the night sky, though its surface is obscured by thick, acidic clouds and it has mountains higher than those on Earth.
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Plate boundaries are the borders between sections of the Earth's crust called tectonic plates. These boundaries can separate plates, causing land masses to break apart into smaller pieces over time. There are currently seven major tectonic plates that make up the Earth's land.
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The document discusses plate tectonics and describes how the Earth's lithosphere is broken into tectonic plates that move over time. It explains that there are two main types of plates - oceanic plates composed mostly of basalt beneath the oceans, and continental plates composed mostly of granite located on land. There are about 16 major tectonic plates that are in constant slow motion, generating geological events like mountain building and volcanism at their boundaries. Alfred Wegener originally proposed the theory of continental drift that recognized plates moved over time.
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The document summarizes the theory of continental drift, which was proposed by Alfred Wegener in 1912. It explains that the continents move across the ocean bed due to shifting tectonic plates at a rate of 1 to 10 cm per year. This movement of plates causes volcanic and seismic activity at plate boundaries. The document also discusses Pangaea, a supercontinent that existed 300 million years ago before breaking apart over 100 million years.
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Photographic evidence - Plate Tectonics
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Subduction zone - Elshaima
Subduction zones occur at convergent plate boundaries where one tectonic plate slides under another plate. There are two types of lithosphere - oceanic and continental - and subduction can happen between oceanic-oceanic plates, oceanic-continental plates, or continental-continental plates. When two plates converge, one plate will subduct below the other at a boundary called a subduction zone.
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There are three main types of seismic waves: P waves, S waves, and L waves. P waves are the first to arrive and move side to side, while S waves follow and move up and down. L waves, also known as surface waves, are the largest and come last, moving in a circular motion. Seismic waves are caused by the breaking of rock in earth's plates and are recorded by seismographs.
Continental drift - Elshaima
The document discusses the theory of continental drift, which was discovered by Alfred Wagner and proposes that the Earth's continents were once joined together in a supercontinent called Pangaea. The theory is supported by three main clues: geological evidence of matching rock layers across continents, evidence of changing climates in the distant past, and the discovery of the same fossils in different continents.
Mountain building - Elshaima
There are four main types of mountains: dome mountains which form when magma pushes up from below the surface; volcanic mountains, which are extinct volcanoes; folded mountains, where pressure from the sides folds and uplifts rock layers; and fault block mountains, where the movement of geological faults causes blocks of land to be uplifted.
Fault - Ping Tian
The document defines three types of faults: normal faults where one land moves down, reverse faults where one land moves up, and strike-slip faults where lands move sideways relative to each other. It also asks and answers three questions: there are three kinds of faults, they are named normal, reverse, and strike-slip faults, and a fault is a break in the ground where land moves.
Earth's interior - Ping Tian
The document describes the different layers that make up the Earth, including the lithosphere, hydrosphere, atmosphere, biosphere, inner core, outer core, mantle, oceanic crust, and continental crust. It states that the layers outside the Earth include the crust, lithosphere, hydrosphere, atmosphere, and biosphere, while the layers inside include the inner core, outer core, and mantle. The document also answers three questions: 1) The inner core has the highest density. 2) The structure from outside to inside is crust, mantle, outer core, inner core. 3) The inner core is the hottest layer.
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- 1. second planet from the Sun *
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- 3. *
- 4. *
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