Preview

Volcanoes and Earthquakes Study Guide

Good Essays
Open Document
Open Document
492 Words
Grammar
Grammar
Plagiarism
Plagiarism
Writing
Writing
Score
Score
Volcanoes and Earthquakes Study Guide
Volcanoes and Earthquakes test Bew c.

1. Where do earthquakes occur?
Earthquakes occur at breaks in the earth’s crust called the fault lines. 2. What causes Earthquakes? Tectonic plates pushing, pulling, slipping past each other increasing the stress and causes elastic rebound to happen. During elastic rebound, energy is released and some travel as seismic waves, which cause an earthquake.

3. How do earthquake waves travel and what are the various types of waves?

Body waves travel through the earth’s body or inside.
P waves: * through liquids solids and gases * moves rocks back and forth * fastest
S waves: * shear rock side to side * cant travel through liquids * second fastest
Surface waves: * move along earth’s surfaces * slow and more destructive

4. How would a seismologist locate and earthquake?
They use a seismograph to record seismic waves and use the S-P time method to figure out the epicenter.

5. What is the basic structure of a volcano?
Vents, lava, magma chamber, and ash

6. What is the difference between an explosive and a non-explosive eruption?

Nonexplosive Eruptions * Most common type * Laval flows from them calmly. (can be huge amount)

Explosive Eruptions * Rarer than nonexplosive eruptions * Are very destructive as pyroclastic materials are flung into the air.

7. What materials erupt from a volcano?

Pyroclastic materials and lava.

Types of lava: Aa * Lava pours out quickly from a volcano and forms a hard crust
Pahoehoe
* Lava pours out very slowly and forms a glassy surface.
Pillow lava * Lava that erupts underwater. * Lava forms rounded lumps shaped like pillows.
Blocky Lava * Lava does not travel far from the erupting vent. * The lava forms jumbled heaps and rocks.

Types of pyroclastic materials:
Volcanic Bombs * Large blobs of magma that harden in the air.
Lapilli
* Pebble like

You May Also Find These Documents Helpful

  • Satisfactory Essays

    Questions 5 through 11 are based on Lab Exercise #2: Locating the Epicenter of an Earthquake. Use the seismogram attached to the Week 3 Announcement, do NOT use Figure 4.11 on page 91.…

    • 1340 Words
    • 6 Pages
    Satisfactory Essays
  • Better Essays

    eosc 114 full notes

    • 6069 Words
    • 25 Pages

    At least 3 earthquake recording stations are required to find the location of the earthquake epicenter. A single recording station can only calculate distance, but not direction; to cover all possibilities, a complete circle is drawn around that station. If only two earthquake recording stations are used, the circles will overlap at two points. Data from a third recording station will eliminate one of these points.…

    • 6069 Words
    • 25 Pages
    Better Essays
  • Good Essays

    Plate tectonic theory is a widely excepted theory that the Earth’s lithosphere is made up of plates, both oceanic and continental, which slowly move due to convection currents in the mantle and the asthenosphere. However, it is very hard to be certain as we can’t see the structure of the Earth, so some people do not agree with it. This theory saw the introduction of what we know today to be tectonic plates. Tectonic plates occur where there is radioactive decay in the core and temperatures are extremely high. This decay can occur anywhere in the earth’s core. This results in a plume of magma rising through the mantle creating a thermal current. When this current reaches the surface it spreads through the asthenosphere, before cooling and sinking. These are the convection currents which move tectonic plates. Convection currents will only occur in liquid form and in warm conditions. Tectonic plate theory has evidence to prove that these currents do take place. We know that the mantle is liquid and has high temperatures as magma that originates in the mantle is molten. This means that convection currents can occur. This part of plate tectonic theory is supported by global seismic activity because if convection current did not exist and plates were not able to move, earthquakes would not occur at any plate boundaries, but particularly at collision plate boundaries as there would be no plate movement.…

    • 942 Words
    • 4 Pages
    Good Essays
  • Good Essays

    Judging from the seismogram in Figure 9.4 of the lab book, which wave appears to be the most damaging?…

    • 716 Words
    • 3 Pages
    Good Essays
  • Good Essays

    Chapter Two Geology

    • 1338 Words
    • 6 Pages

    Movement of Earth’s Plates:The plates move due to the mantles CONVECTION CELLS: warm material rises toward surface, cools&descends back into the interior. Creating volcanoes, earthquakes, MTNS.…

    • 1338 Words
    • 6 Pages
    Good Essays
  • Powerful Essays

    Earthquakes are an example of seismic activity caused by the build-up of tension at the three types of plate boundaries: destructive, constructive and conservative. The pressure is suddenly released as the plates jerk past each other, sending out seismic waves from the focus that travel through different parts of the earth. The movement of convection currents within the Earth’s mantle causing the crust to become mobile which creates the different types plate margins, makes the cause due to physical factors. However human activity is suggested to be the cause of some minor earthquakes, for instance the building of large reservoirs where the water stresses the surface rocks or the subsidence of deep mine workings.…

    • 2230 Words
    • 9 Pages
    Powerful Essays
  • Good Essays

    Over time plate movement or subduction causes increasing strain on "sticking points" within the crust. Similar to if you rub two pieces of sand paper together, they will initially resist sliding until enough strain is built up. At that point, the "sticking point" is weakened and releases the built up strain. Before this theory was developed, scientists were unsure whether earthquakes caused faulting (plate movement) of faulting caused earthquakes.…

    • 657 Words
    • 3 Pages
    Good Essays
  • Satisfactory Essays

    The first thing earthquakes effects is earth. When two continental plates meet, earthquakes are happening, volcano eruptions and mountain formation caused by continental plates. Earthquakes cause the ground to shake and creates cracks and holes in the ground. They can also make trees and other objects in the wild or nature, fall and crash into the ground. Soil in the ground can change or liquefy because of earthquakes.…

    • 306 Words
    • 2 Pages
    Satisfactory Essays
  • Better Essays

    In class I have learned how the National Hurricane centre detects earthquakes using many different methods from aeroplanes to balloons that fly into the atmosphere and record the weather.…

    • 1318 Words
    • 6 Pages
    Better 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
  • Good Essays

    ANSWERS: Friction between the rough edges of slowly moving segments or plates of the earth’s lithosphere result in a series of jerky starts and stops which is the direct cause of most earthquakes.…

    • 335 Words
    • 2 Pages
    Good 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
  • Better Essays

    Earthquakes

    • 2019 Words
    • 9 Pages

    An earthquake is a shaking or trembling of the crust of the earth caused by underground volcanic action or by the breaking and shifting of rock beneath the surface. The volcanic action and shifting rocks create strain which continues to build to a sudden release of pressure resulting in a shock wave. The vibrations produced in the crust can vary from barely noticeable to enormously destructive. Shock waves can be classified into two broad categories. Waves that send particles oscillating back and forth in the same direction as the waves are traveling are called primary. Primary waves, sometimes called compressional waves, travel through the earth beneath the crust. Secondary waves cause vibrations which move perpendicular to the wave. These waves travel on the surface of the earth and move much slower than primary waves. Thus, when an earthquake occurs, seismic centers throughout the world record primary waves before the secondary waves arrive.…

    • 2019 Words
    • 9 Pages
    Better Essays
  • Powerful Essays

    Earthquake Notes

    • 4604 Words
    • 19 Pages

    An earthquake is the vibration of the earth produced by the quick release of energy. Most often, earthquakes are caused by movement along large fractures in the earth’s crust. Such fractures are called faults. The energy that is released radiates in all directions from its origin in the form of waves. These waves are similar to the waves that occur when you drop a stone into water. Just as the stone sets the water in motion, the energy released in an earthquake produces seismic waves that move through the earth. Frequency range of seismic waves is large, from as high as the audible range (greater than 20 hertz) to as low as the frequencies of the free oscillations of the whole Earth (2 and 7 millihertz). Attenuation of the waves in rock imposes high-frequency limits, and in small to moderate earthquakes the dominant frequencies extend in surface waves from about 1 to 0.1 hertz. The amplitude range of seismic waves is also great in most earthquakes. In the greatest earthquakes the ground amplitude of the predominant P waves may be several centimeters at periods of two to five seconds. Very close to the seismic sources of great earthquakes, investigators have measured large wave amplitudes with accelerations of the ground exceeding that of gravity (9.8 meters, or 32.2 feet, per second squared) at high frequencies and ground displacements of 1 meter at low frequencies.…

    • 4604 Words
    • 19 Pages
    Powerful Essays
  • Good Essays

    Causes of Earthquake

    • 372 Words
    • 2 Pages

    The short answer is that earthquakes are caused by faulting, a sudden lateral or vertical movement of rock along a rupture (break) surface.…

    • 372 Words
    • 2 Pages
    Good Essays