Preview

How Peak Oil Affects Agriculture

Good Essays
Open Document
Open Document
408 Words
Grammar
Grammar
Plagiarism
Plagiarism
Writing
Writing
Score
Score
How Peak Oil Affects Agriculture
Geological Hazards
Plate Tectonics- Theory
Alfred Wegener

Crust- Solid
Mantle- Liquid
Outer Core- Liquid
Inner Core- Solid (Too much pressure for it to be liquid. Doesn’t have the space to expand.)

Convections cells- Due to the pressure in the earth’s core, when it heats up the pressure causes the heat to push against the earth’s mantle, triggering it to move, caused by convection currents.
Convection Currents- it’s a concept of what causes the plate tectonics to move. http://www.scotese.com/pangeanim.htm Plate Boundaries Map

Types of Crust:
Oceanic- young, thin, under oceans, very dense.
Continental- old, thick, makes up land, less dense.
Crusts move towards each other, continental crust is less dense, therefore moves on top of the oceanic crust. The oceanic crust-being closer to the mantle (heat)- burns up through the continental crust, causing volcanoes. A- Diverging plate boundaries- moving apart, it can happen between continental or oceanic crust. The crust moves apart, which forms new oceanic crust, therefore making it young. Volcanoes are formed, but there is no grinding against plates, thus no earthquakes. B- Converging plate margins- earthquakes and volcanoes. The plates coming together. Crusts move towards each other, continental crust is less dense, therefore moves on top of the oceanic crust. The oceanic crust-being closer to the mantle (heat)- burns up through the continental crust, causing volcanoes. East side of south America- trenches. C- Transform Fault Boundaries- Grinding of crust, meaning earthquakes. The longer between earthquakes, the bigger they will be. The San Andreas Fault Line on the Carrizo Plain in Cali.

Subducts- go down.

Are earthquakes and volcanoes located equally and randomly over the earth’s surface? * No, volcanoes and earthquakes are not randomly spread over the earth’s surface as they are linked to plate boundaries. Also, they are mainly around the areas of the coastal regions, as

You May Also Find These Documents Helpful

  • Satisfactory Essays

    This type of plate collapse is a convergent boundary. When the plates crashes, it creates a hot spot in the center, which is the cause of the creation of mountains that come out of the oceans, which we call volcanoes.…

    • 281 Words
    • 2 Pages
    Satisfactory Essays
  • Better Essays

    When the plates move apart, molten material from under the crust moves up to replace the separating crust, resulting in sea floor spreading.…

    • 2390 Words
    • 11 Pages
    Better Essays
  • Better Essays

    Script For Mt St Helens

    • 1103 Words
    • 5 Pages

    There are three plate boundaries, they are the divergent plate boundaries, transform plate boundaries and the convergent plate boundaries. Divergent plates move away from each other and are found in the middle of major oceans. These boundaries help to form underwater volcanoes and create new oceanic crust. Transform plates are plates that slide past each other and this is what causes earthquakes. If…

    • 1103 Words
    • 5 Pages
    Better Essays
  • Powerful Essays

    GEO FINAL STUDY GUIDE

    • 6690 Words
    • 27 Pages

    Convergent- Plates move toward each other and collide, or the more dense plate subducts below the less dense plate. (Forms volcanoes and trenches)…

    • 6690 Words
    • 27 Pages
    Powerful Essays
  • Better Essays

    Anth 368

    • 1944 Words
    • 8 Pages

    The earth’s crust is made out of plate tectonics. Each plate has a defined boundary and direction it moves. The plates in Earth’s crust perform two actions; they submerge under each other or they spread out. The Pacific Plate is the largest plate and it borders around many plates. The Pacific Plate moves northwest. New crust is formed from magma outpours, which are a result of the zones spreading. The tectonic plates created the islands. When the tectonic plates move, it creates the change in geography. Active volcanoes together shape the way islands are build. The magma from the volcano and the deposits from the plate are needed to create the pacific islands structure. The buildup of deposits eventually pushes pass sea level to create the island. The islands that are part of the same volcanic chain will all take over a millions years to rise.…

    • 1944 Words
    • 8 Pages
    Better Essays
  • Good Essays

    Chapter Two Geology

    • 1338 Words
    • 6 Pages

    PLATE TECHTONIC THEORY:The lithosphere that is broken into plates move on earth’s surface relative to one another. Zones of volcanic, E.quake mark most plate boundaries.…

    • 1338 Words
    • 6 Pages
    Good Essays
  • Good Essays

    Plate Tectonic Assignment

    • 568 Words
    • 3 Pages

    17. What, if any correlation is there between the distribution of earthquakes, volcanoes and plate boundaries?…

    • 568 Words
    • 3 Pages
    Good Essays
  • Better Essays

    Pompeii Research Paper

    • 1091 Words
    • 5 Pages

    Volcanoes are formed on land near coastal areas when a continental plate and an oceanic plate converge. The oceanic plate submerges, due to its higher density, and is pushed deeper and deeper beneath the surface. The high temperature and pressures below melt the rock which creates hot, buoyant magma. Ultimately this magma rises towards the surface and accumulates in a reservoir, known as the magma chamber. The eruption occurs when the pressure within in the chamber surpasses the pressure of the upper rock, magma forces its way through the cracks in Earth’s crust. Magma that is low in gas and silicon dioxide produces thin quickly spreading lava which has a low viscosity, while a magma that is heavily composed of gas and silicon dioxide will yield a thick, viscose magma. The thicker magma builds up and because of this pressure, will cause a large…

    • 1091 Words
    • 5 Pages
    Better Essays
  • Good Essays

    The global seismic and volcanic activity is concentrated along the margins of the earth’s plates, which are broken pieces of the crust and are moved by convection currents that are caused by heat rising and falling inside the mantle generated by radioactive decay in the core. This movement of the plates and the Earth’s inner activity is called plate tectonics and can cause seismic and volcanic activity. However, earthquakes and volcanoes also occur within the plates rather than their edges, an example of which is the Hawaiian volcanoes that occur above a stationary hot spot beneath the Pacific plate. In the late 1960s the theory of plate tectonics was developed by Alfred Wegener and provides an explanation for the Earths tectonic behaviour, particularly the global distribution of mountain building, earthquake activity, and volcanism in a series of linear belts. However, before the theory was developed people had noticed that the continents either side of the Atlantic Ocean seemed to nearly fit together. In 1912 Alfred Wegner published the theory of continental drift suggesting that the continents used to be joined together in an ancient supercontinent which he named Pangaea. He then proposed that it later split in to two continents- Laurasia in the north and Gondwanaland in the south, which further split forming our current continents and at some point these land masses had drifted apart to their current positions on the globe.…

    • 1090 Words
    • 3 Pages
    Good Essays
  • Good Essays

    Plate Tectonics Theory

    • 470 Words
    • 2 Pages

    Plate tectonics theory, which is the modern theory of the motions of Earth’s layer, explains how geological features, such as mountain ranges, continents, and bodies of water move and form. An important aspect of plate tectonics theory is that the outer layer of the earth is divided into plates which move across the earth’s surface. “These plates move relative to each other, typically at rates of 2-4 inches per year. As the plates move, they interact along their boundaries” (Plate Tectonics). In other words, the formation of geological features occur at the plate boundaries which is where plates slide and interact. There are four types of plate boundaries: divergent boundaries, convergent boundaries, transform…

    • 470 Words
    • 2 Pages
    Good Essays
  • Powerful Essays

    A volcanic or seismic hazard can have an effect on all people from differing economic backgrounds and the extent of the disaster if often directly linked to the magnitude of the earthquake or the areal extent of the volcanic eruption. This is therefore a result of the occurrence of type of plate boundary. A volcanic eruption produced at a destructive plate boundaries is likely to be much more devastating than at a constructive. This occurs because the volcano is usually composite and therefore expresses rhyolitic lava with low silica content and therefore erupts unpredictably and with great force. At this plate boundary, a denser plate (e.g. oceanic or and older plate) subducts a less dense plate (continental or newer) and this plate descends into the asthenosphere. The plate melts at the Benioff zone due to increased temperatures and pressures and stress is…

    • 1487 Words
    • 4 Pages
    Powerful Essays
  • Good Essays

    Earthquakes develop in the crust of the earth. The inner parts contains a lot of energy. Some of this energy can escape through cracks which can cause volcanic activity, but most of it is stored within the earth’s inner part, contained in the crust.The earth’s outer crust has rough edges and lines making it look a bit like a jigsaw puzzle.The energy stored here causes the pieces to slide, glide, knock and move around each piece. These pieces are also known as tectonic plates.…

    • 514 Words
    • 3 Pages
    Good Essays
  • Good Essays

    romeo and juliet

    • 563 Words
    • 3 Pages

    Most naturally occurring earthquakes are related to the tectonic nature of the Earth. Such earthquakes are called tectonic earthquakes. The Earth's lithosphere is a patchwork of plates in slow but constant motion caused by the release to space of the heat in the Earth's mantle and core. The heat causes the rock in the Earth to flow on geological timescales, so that the plates move slowly but surely. Plate boundaries lock as the plates move past each other, creating frictional stress. When the frictional stress…

    • 563 Words
    • 3 Pages
    Good Essays
  • Better Essays

    Conservative Plate Margins

    • 2967 Words
    • 9 Pages

    When two plates slide past each other they create a conservative plate margin. The relative movement is horizontal, and classified as either sinistral (moving to the left) or dextral (moving to the right). Along these margins crust (lithosphere) is not being destroyed by subduction, neither is it being created. There is no melting of rock, and, therefore, no volcanic activity or formation of new crust. Despite the absence of volcanic activity, these margins are tectonically extremely active and are associated with powerful, considerable magnitude, earthquakes, being the sites of extensive shallow focus earthquakes. Transfer faults are mainly found on the ocean floor, where they offset mid ocean ridges and enable the ocean floor to spread at different rates. At conservative plate boundaries, there are very few features to be seen, save for the large crack that forms in the ground where two separate plates are moving against each other. Sometimes there is known to be some cliff forming along the fault line.…

    • 2967 Words
    • 9 Pages
    Better Essays
  • Satisfactory Essays

    Vulcanicity

    • 362 Words
    • 2 Pages

    VulcanicityVolcanoes mostly occur at plate margins. They can also occur at hot spots and in rift valleys. The most active volcanic zone is the Pacific Ring of Fire around the Pacific plate. Here plates are colliding or separating. At active points on these plates volcanic mountains are formed, e.g. Nazca Plate and South American Plate, where plates separate, e.g. Pacific and Nazca Plate and in rift valleys, e.g. African Plate, Kenya. The most active area on the globe is the western rim of the Pacific Plate - stretching from Russia to New Zealand.Several findings relating to earthquakes and volcanic activity can be explained by plate tectonics. If you follow news stories of earthquakes, you may begin to wonder why such places as California or Japan have so many earthquakes, whereas the north eastern United States or Western Europe have so few. The fact is that earthquakes occur along belts and the vast majority of these belts lie on the boundaries of the earth’s tectonic plates. The same is true of volcanoes and locations known for earthquakes, such as the Philippines, have many volcanoes.The Hawaiian Islands are located near the centre of the Pacific Plate. These islands of Hawaii experience plate movement, helping to form the volcanoes that created those islands. At the south of the island group, many volcanoes are still active, while those to the north are mainly dormant. The reason for this is that the Pacific Plate is moving north over a stationary lava source (mantle plume) below Hawaii. The south islands remain above it, while the northern islands have moved away.The Oceanic crusts are tend to be youngest at the centre of ocean basins and along mid-ocean ridges, or along submarine ridges where new seafloor is created. There is much volcanic activity here as massive fissure eruptions frequently occur. Crusts of oceanic and continental type differ by their thickness and by composition. Basalt, an igneous rock (from the cooling of magma), makes up the SIMA,…

    • 362 Words
    • 2 Pages
    Satisfactory Essays

Related Topics