Coasts-The essential revision
... slightly acidic, can slowly dissolve certain rocks. BIOLOGICAL – This involves the actions of animals (fauna) and plants (flora). Plant roots are very effective at growing and expanding in rock cracks. Animals such as rabbits and sea birds will burrow in weak rocks ...
... slightly acidic, can slowly dissolve certain rocks. BIOLOGICAL – This involves the actions of animals (fauna) and plants (flora). Plant roots are very effective at growing and expanding in rock cracks. Animals such as rabbits and sea birds will burrow in weak rocks ...
earthquakes
... • The 2004 Indian Ocean earthquake, was an undersea earthquake that occurred at 00:58:53 UTC (07:58:53 local time) December 26, 2004, with an epicentre off the west coast of Sumatra, Indonesia. The earthquake triggered a series of devastating tsunamis along the coasts of most landmasses bordering t ...
... • The 2004 Indian Ocean earthquake, was an undersea earthquake that occurred at 00:58:53 UTC (07:58:53 local time) December 26, 2004, with an epicentre off the west coast of Sumatra, Indonesia. The earthquake triggered a series of devastating tsunamis along the coasts of most landmasses bordering t ...
Momentum Transport
... Control volume and station nomenclature for applying conservation principles across a gas dynamic discontinuity separating two regions of flow in which diffusion processes can be neglected ...
... Control volume and station nomenclature for applying conservation principles across a gas dynamic discontinuity separating two regions of flow in which diffusion processes can be neglected ...
Chapter 4: Igneous Rocks: Product of Earth`s Internal Fire
... Surface waves travel more slowly than P waves and S waves, but are often the largest vibrational signals in a seismogram. Love waves consist entirely of shear wave vibrations in the horizontal plane, analogous to an S wave that travels horizontally. Rayleigh waves combine shear and compressional vib ...
... Surface waves travel more slowly than P waves and S waves, but are often the largest vibrational signals in a seismogram. Love waves consist entirely of shear wave vibrations in the horizontal plane, analogous to an S wave that travels horizontally. Rayleigh waves combine shear and compressional vib ...
File
... When they break large amounts of energy is released in the form of waves. This release of energy from the stress built up in the crust is what we call Earthquakes. Earthquakes are caused by the release of stress that builds up as the plates move around the Earth. Earthquakes ...
... When they break large amounts of energy is released in the form of waves. This release of energy from the stress built up in the crust is what we call Earthquakes. Earthquakes are caused by the release of stress that builds up as the plates move around the Earth. Earthquakes ...
Earthquakes and Damages Name
... ____ 35. Which type of seismic wave causes rock particles to move together and apart in the same direction as the wave is moving? A. L wave B. S wave C. P wave D. surface wave ____ 36. What is the minimum number of seismograph stations a scientist must have data from in order to locate the epicenter ...
... ____ 35. Which type of seismic wave causes rock particles to move together and apart in the same direction as the wave is moving? A. L wave B. S wave C. P wave D. surface wave ____ 36. What is the minimum number of seismograph stations a scientist must have data from in order to locate the epicenter ...
Earth Science – Quiz 2
... B) reversed magnetizations along the rift valleys and normal magnetizations along the ridge C) normal and reversed magnetized strips roughly parallel to the ridge D) normal and reversed magnetized strips roughly perpendicular to the ridge axis 16. A typical rate of seafloor spreading in the Atlantic ...
... B) reversed magnetizations along the rift valleys and normal magnetizations along the ridge C) normal and reversed magnetized strips roughly parallel to the ridge D) normal and reversed magnetized strips roughly perpendicular to the ridge axis 16. A typical rate of seafloor spreading in the Atlantic ...
Fact Sheet - SharpSchool
... from seismometers. Seismometers should be attached to bedrock (the solid rock that lies beneath the soil and looser rocks) in order to feel the vibrations that result from an earthquake. Seismologist use a method of measurement called richer scale to describe the magnitude (strength) of an earthquak ...
... from seismometers. Seismometers should be attached to bedrock (the solid rock that lies beneath the soil and looser rocks) in order to feel the vibrations that result from an earthquake. Seismologist use a method of measurement called richer scale to describe the magnitude (strength) of an earthquak ...
Multi-station Seismograph Network
... Asperity—literally “roughness. It is an area on a fault that is stuck or locked. A type of surface roughness appearing along the interface of 2 faults. Physics the elastically compressed region of contact between two surfaces caused by the normal force. Asthenosphere—the ductile part of the earth ju ...
... Asperity—literally “roughness. It is an area on a fault that is stuck or locked. A type of surface roughness appearing along the interface of 2 faults. Physics the elastically compressed region of contact between two surfaces caused by the normal force. Asthenosphere—the ductile part of the earth ju ...
Trivial Pursuit File
... Sheer force of the water hitting the river bed and banks Increasing incomes so more money for holidays, holiday leave time from work has increased, good pensions ...
... Sheer force of the water hitting the river bed and banks Increasing incomes so more money for holidays, holiday leave time from work has increased, good pensions ...
Section 19.1 Forces within Earth
... movements can occur 3. Fault Scarps, people can fall into large openings 4. Tsunami, large waves of water can drown people ...
... movements can occur 3. Fault Scarps, people can fall into large openings 4. Tsunami, large waves of water can drown people ...
tsunamis - MrDanielASBSukMSSci
... (750 mi) of fault line slipped 20 m (60 ft) along the subduction zone where the India Plate dives under the Burma Plate. The seabed of the Burma plate is estimated to have risen several metres vertically up over the India plate, creating shock waves in the Indian Ocean that travelled at up to 800 km ...
... (750 mi) of fault line slipped 20 m (60 ft) along the subduction zone where the India Plate dives under the Burma Plate. The seabed of the Burma plate is estimated to have risen several metres vertically up over the India plate, creating shock waves in the Indian Ocean that travelled at up to 800 km ...
EXAM 3
... E. none of the above 38. Which of the following is not an earthquake hazard? A. fire B. ground fissures C. tsunami waves D. lahars E. landslides 39. The bending of waves through different rock layers is called (1) ___________ whereas the bouncing of waves off of layer boundaries is called (2) ______ ...
... E. none of the above 38. Which of the following is not an earthquake hazard? A. fire B. ground fissures C. tsunami waves D. lahars E. landslides 39. The bending of waves through different rock layers is called (1) ___________ whereas the bouncing of waves off of layer boundaries is called (2) ______ ...
Word format
... E. none of the above 4. The horns of a (1) _______ dune point towards the direction the wind blows from, whereas in a (2) _________ dune they point in the direction the wind is blowing towards. A. (1) transverse; (2) longitudinal B. (1) barchan; (2) barchanoid C. (1) transverse; (2) parabolic D. (1) ...
... E. none of the above 4. The horns of a (1) _______ dune point towards the direction the wind blows from, whereas in a (2) _________ dune they point in the direction the wind is blowing towards. A. (1) transverse; (2) longitudinal B. (1) barchan; (2) barchanoid C. (1) transverse; (2) parabolic D. (1) ...
Earthquakes - Leon County Schools
... http://elearning.niu.edu/simulations/images/S_portfolio/Mercalli/Mercalli_Scale.swf ...
... http://elearning.niu.edu/simulations/images/S_portfolio/Mercalli/Mercalli_Scale.swf ...
Chapter 15
... Types of faults • NORMAL - one side of a fault slips down relative to another • REVERSE (& Thrust) - one side of a fault is driven up and over the other • STRIKE-SLIP – occur where plates meet evenly and slip past each other horizontally. (The angle at which a fault cuts through the earth is refer ...
... Types of faults • NORMAL - one side of a fault slips down relative to another • REVERSE (& Thrust) - one side of a fault is driven up and over the other • STRIKE-SLIP – occur where plates meet evenly and slip past each other horizontally. (The angle at which a fault cuts through the earth is refer ...
Category 1
... goes with each fault. What is…….strike-slip and shearing, normal and tension, reverse and compression ...
... goes with each fault. What is…….strike-slip and shearing, normal and tension, reverse and compression ...
Multi-station Seismograph Network
... Asperity—literally “roughness. It is an area on a fault that is stuck or locked. A type of surface roughness appearing along the interface of 2 faults. Physics the elastically compressed region of contact between two surfaces caused by the normal force. Asthenosphere—the ductile part of the earth ju ...
... Asperity—literally “roughness. It is an area on a fault that is stuck or locked. A type of surface roughness appearing along the interface of 2 faults. Physics the elastically compressed region of contact between two surfaces caused by the normal force. Asthenosphere—the ductile part of the earth ju ...
PacIOOS Wave Buoy Poster
... When these waves enter shallower water, many physical changes occur to the wave. As the first wave “feels” the ocean floor, it slows down, while the second wave catches up to the slowed down wave in its original speed. Similar to ...
... When these waves enter shallower water, many physical changes occur to the wave. As the first wave “feels” the ocean floor, it slows down, while the second wave catches up to the slowed down wave in its original speed. Similar to ...
Earthquakes
... determinations result in two possible locations (two overlapping circles have two points in common). Three or more determinations can only have one location in common. This location is called the epicenter. ...
... determinations result in two possible locations (two overlapping circles have two points in common). Three or more determinations can only have one location in common. This location is called the epicenter. ...
Earthquakes - Lindbergh Schools
... splitting stopped before new plates could form. The faults in the New Madrid Zone are remnants of this old event. Earthquakes occur because the North American Plate is still "settling down". The faults in the New Madrid Zone do not reach the Earth’s surface. They are buried beneath thousands of feet ...
... splitting stopped before new plates could form. The faults in the New Madrid Zone are remnants of this old event. Earthquakes occur because the North American Plate is still "settling down". The faults in the New Madrid Zone do not reach the Earth’s surface. They are buried beneath thousands of feet ...
Notes on Earthquakes and Earth`s interior - earth
... Name ___________________ Topic 6.4-6.5: Notes ...
... Name ___________________ Topic 6.4-6.5: Notes ...
Earthquakes
... which gave the observer an impression of a rolling feeling rather than abrupt hard jolts. After about 1 minute the amplitude or strength of the shock waves increased in intensity and failures in buildings as well as the frozen ground surface began to occur ... After about 3 1/2 minutes the severe sh ...
... which gave the observer an impression of a rolling feeling rather than abrupt hard jolts. After about 1 minute the amplitude or strength of the shock waves increased in intensity and failures in buildings as well as the frozen ground surface began to occur ... After about 3 1/2 minutes the severe sh ...
Rogue wave
Rogue waves (also known as freak waves, monster waves, killer waves, extreme waves, and abnormal waves) are relatively large and spontaneous surface waves that occur far out in open water, and are a threat even to large ships and ocean liners.They present two kinds of danger: although rare, they are unpredictable, and may appear suddenly or without warning, and they can impact with tremendous force (a 12 meter wave in the usual ""linear"" model would have a breaking force of 6 million tons per square metre (MT/m2); modern ships are designed to tolerate a breaking wave of 15 MT/m2), but a rogue wave can dwarf both of these figures with a breaking force of 100 MT/m2.In oceanography, rogue waves are more precisely defined as waves whose height is more than twice the significant wave height (Hs or SWH), which is itself defined as the mean of the largest third of waves in a wave record. Therefore, rogue waves are not necessarily the biggest waves found on the water; they are, rather, unusually large waves for a given sea state. Rogue waves seem not to have a single distinct cause, but occur where physical factors such as high winds and strong currents cause waves to merge to create a single exceptionally large wave.Rogue waves can occur in other media than water. In particular, optical rogue waves allow study of the phenomenon in the laboratory. A 2015 paper studied the wave behavior around a rogue wave, including optical, and the Draupner wave, and concluded that ""rogue events do not necessarily appear without a warning, but are often preceded by a short phase of relative order"".