4-6-minoura - Extras Springer
... pumice (Gouves) conform to the published data (Table 1). Glass shards with a similar refractive index are found only in the Pleistocene V-1 tephra from Aegean Sea deep-sea cores [12]. We conclude that the felsic layers found in the coastal sequences correspond to the Thera tephra. The major and mino ...
... pumice (Gouves) conform to the published data (Table 1). Glass shards with a similar refractive index are found only in the Pleistocene V-1 tephra from Aegean Sea deep-sea cores [12]. We conclude that the felsic layers found in the coastal sequences correspond to the Thera tephra. The major and mino ...
full C.V. in format here.
... Data analysis for an experiment in the Baltic Sea to study atmospheric flux profile relations under different sea conditions. ...
... Data analysis for an experiment in the Baltic Sea to study atmospheric flux profile relations under different sea conditions. ...
FOURTH GRADE EARTHQUAKES
... As discussed in the Pre Lab, the damage caused by earthquakes is dependent on the intensity of the earthquake and the type of ground a structure is built on. A third factor is the materials used in a building’s construction. In earthquake country, unreinforced building materials like brick are not s ...
... As discussed in the Pre Lab, the damage caused by earthquakes is dependent on the intensity of the earthquake and the type of ground a structure is built on. A third factor is the materials used in a building’s construction. In earthquake country, unreinforced building materials like brick are not s ...
Homework Set 2
... 5. Examine the attached map showing the rupture extent of the December 2004 Sumatra-Andaman earthquake (M9.0). Then answer the following ...
... 5. Examine the attached map showing the rupture extent of the December 2004 Sumatra-Andaman earthquake (M9.0). Then answer the following ...
Earthquakes: Do we ever cause them?
... Have you ever felt an earthquake? They happen when there is a sudden release of energy in the Earth’s crust. They have lots of natural causes, but scientists are just discovering that some of the things people do can set them off, too. That might sound a little hard to believe. We’ve all felt the gr ...
... Have you ever felt an earthquake? They happen when there is a sudden release of energy in the Earth’s crust. They have lots of natural causes, but scientists are just discovering that some of the things people do can set them off, too. That might sound a little hard to believe. We’ve all felt the gr ...
Opportunity to Lead the Earthquake Monitoring Project at the U.S.
... hiring a Supervisory Geophysicist to lead our Earthquake Monitoring Project. This important and influential permanent position is at the GS-14 or GS-15 level (salary range $115,613 to $157,100). The mission of the ESC is to reduce seismic hazard by conducting basic and applied research on earthquake ...
... hiring a Supervisory Geophysicist to lead our Earthquake Monitoring Project. This important and influential permanent position is at the GS-14 or GS-15 level (salary range $115,613 to $157,100). The mission of the ESC is to reduce seismic hazard by conducting basic and applied research on earthquake ...
wave - UniMAP Portal
... an object and is not related to refraction. Diffraction occurs when a wave passes through an opening that is comparable in size to the wavelength; the waves will “bend” around the edges of the opening. ...
... an object and is not related to refraction. Diffraction occurs when a wave passes through an opening that is comparable in size to the wavelength; the waves will “bend” around the edges of the opening. ...
Packet #9
... o the seismic station above, how manyy additional onnes scientist need to predict an earthquake? ...
... o the seismic station above, how manyy additional onnes scientist need to predict an earthquake? ...
Waves are moving energy
... When ocean waves encounter land • Deep water waves change to shallow water waves as they approach the shore • Once the wave passes over water whose depth is less than one half its wavelength, the wave “feels” the bottom • When this happens, the circular motion of the water molecules in the wave is ...
... When ocean waves encounter land • Deep water waves change to shallow water waves as they approach the shore • Once the wave passes over water whose depth is less than one half its wavelength, the wave “feels” the bottom • When this happens, the circular motion of the water molecules in the wave is ...
Properties of Waves
... distance / thousands of km An earthquake station is 6000 km from an earthquake. The P-wave reaches the earthquake station before the S-wave. Use the graph to find the difference in the arrival time of the S-wave and P-wave. ...
... distance / thousands of km An earthquake station is 6000 km from an earthquake. The P-wave reaches the earthquake station before the S-wave. Use the graph to find the difference in the arrival time of the S-wave and P-wave. ...
Slide 1 - Cloudfront.net
... Large waves are more able to remove large chunks of rock from a shoreline than average-sized waves are because large waves transfer more energy than average-sized waves do. ...
... Large waves are more able to remove large chunks of rock from a shoreline than average-sized waves are because large waves transfer more energy than average-sized waves do. ...
Entry Task
... smaller than tectonic plates • A small percentage of earthquakes occur along faults within plates – Stress along a plate boundary can cause the rocks to break and move along weak areas in the middle of the plate. ...
... smaller than tectonic plates • A small percentage of earthquakes occur along faults within plates – Stress along a plate boundary can cause the rocks to break and move along weak areas in the middle of the plate. ...
Earthquakes, Volcanoes and Igneous Activity
... A special condition associated with strong earthquakes on the ocean floor is the production of seismic sea waves. Tsunami-the Japanese word for "wave in the harbor"-is a large wavelength ocean wave pnoduced by disruption of the ocean floor. This disruptibn can be caused by the fau-lting associated w ...
... A special condition associated with strong earthquakes on the ocean floor is the production of seismic sea waves. Tsunami-the Japanese word for "wave in the harbor"-is a large wavelength ocean wave pnoduced by disruption of the ocean floor. This disruptibn can be caused by the fau-lting associated w ...
3. Earthquakes 3.1. Elastic rebound theory
... Most earthquakes are distributed along active plate boundaries. The depth at which they occur (focal depth) varies according to the tectonic setting (Figs. 30 & 31). Earthquakes occurring along divergent margins are shallow and associated with tensional forces (Fig. 31A). Shallow earthquakes also oc ...
... Most earthquakes are distributed along active plate boundaries. The depth at which they occur (focal depth) varies according to the tectonic setting (Figs. 30 & 31). Earthquakes occurring along divergent margins are shallow and associated with tensional forces (Fig. 31A). Shallow earthquakes also oc ...
worksheet a MS Word file ()
... Slide 25 – What are some of the aspects of an earthquake that scientists want to determine and ...
... Slide 25 – What are some of the aspects of an earthquake that scientists want to determine and ...
Exam 3 PRACTICE – Winter 2016 KEY
... 15. A loop of connected surface currents is called a a. Gyre b. Coriolis structure c. Thermocline d. Pycnocline 16. What is the direct cause of the ocean’s surface currents? a. Salinity variations b. Density variations c. Vertical circulation d. Wind 17. In terms of heat energy, what do surface curr ...
... 15. A loop of connected surface currents is called a a. Gyre b. Coriolis structure c. Thermocline d. Pycnocline 16. What is the direct cause of the ocean’s surface currents? a. Salinity variations b. Density variations c. Vertical circulation d. Wind 17. In terms of heat energy, what do surface curr ...
File
... If the end was fixed • If the string fixed to the pole instead how would it change things? • When the pulse hits the pole it wants to move up, but the pole exerts a downward force. • This force creates a wave that is in the opposite displacement of the original wave. ...
... If the end was fixed • If the string fixed to the pole instead how would it change things? • When the pulse hits the pole it wants to move up, but the pole exerts a downward force. • This force creates a wave that is in the opposite displacement of the original wave. ...
6 W A V E REPORTING PROCEDURES TSUNAMI
... Pacific are coordinated through the IOC's International Tsunami Information Centre (ITIC), located in Honolulu; and also through the IOC's International Co-ordination Group for the Tsunami Warning System in the Pacific (ICG-ITSU) which is open to all Member States of IOC. The Pacific Tsunami Warning ...
... Pacific are coordinated through the IOC's International Tsunami Information Centre (ITIC), located in Honolulu; and also through the IOC's International Co-ordination Group for the Tsunami Warning System in the Pacific (ICG-ITSU) which is open to all Member States of IOC. The Pacific Tsunami Warning ...
Types of Earthquake Waves
... The fastest of all three types of waves P waves travel between 5 and 13 km/second Represented by the compression waves of the slinky on the previous slide. Can pass through liquids, solids and gasses Expand and compress materials in their path Move buildings back and forth The compression causes a s ...
... The fastest of all three types of waves P waves travel between 5 and 13 km/second Represented by the compression waves of the slinky on the previous slide. Can pass through liquids, solids and gasses Expand and compress materials in their path Move buildings back and forth The compression causes a s ...
towers earthquake powerpoint
... The fastest of all three types of waves P waves travel between 5 and 13 km/second Represented by the compression waves of the slinky on the previous slide. Can pass through liquids, solids and gasses Expand and compress materials in their path Move buildings back and forth The compression causes a s ...
... The fastest of all three types of waves P waves travel between 5 and 13 km/second Represented by the compression waves of the slinky on the previous slide. Can pass through liquids, solids and gasses Expand and compress materials in their path Move buildings back and forth The compression causes a s ...
Earth Hazards - Teacher Friendly Guides
... the San Andreas fault zone are considered at risk for a major earthquake at any time, and either one could generate an earthquake that would wreak havoc on the lives of the 23 million inhabitants of Southern California. Earthquake preparedness drills based on this scenario have been taking place in ...
... the San Andreas fault zone are considered at risk for a major earthquake at any time, and either one could generate an earthquake that would wreak havoc on the lives of the 23 million inhabitants of Southern California. Earthquake preparedness drills based on this scenario have been taking place in ...
Ch. 6 Earthquakes
... – Regions within 20 to 50 kilometers of the epicenter will experience about the same intensity of ground shaking – However, destruction varies considerably mainly due to the nature of the ground on which the structures are built ...
... – Regions within 20 to 50 kilometers of the epicenter will experience about the same intensity of ground shaking – However, destruction varies considerably mainly due to the nature of the ground on which the structures are built ...
Tsunami Detection and Warnings for the United States
... occurred along the face of the North American continental shelf.5 Also, they noted that strong earthquakes have occurred on the ocean floor off the coast of Puerto Rico, and that some of them generated tsunamis that caused major loss of life and property damages in both the Atlantic and Caribbean Ba ...
... occurred along the face of the North American continental shelf.5 Also, they noted that strong earthquakes have occurred on the ocean floor off the coast of Puerto Rico, and that some of them generated tsunamis that caused major loss of life and property damages in both the Atlantic and Caribbean Ba ...
Chapter 7: Earthquakes
... damage Slowest type of seismic wave As depth increases, motion of the particles ...
... damage Slowest type of seismic wave As depth increases, motion of the particles ...
Sample Lesson 57 - Nancy Larson® Science
... “The epicenter is where most of the damage from an earthquake usually occurs.” “In the third sentence, highlight the words ‘place on the surface of Earth that is directly above the focus’ and ‘epicenter.’ ” “Let’s find out what happens when earthquakes occur below the ocean.” “Follow along as I read ...
... “The epicenter is where most of the damage from an earthquake usually occurs.” “In the third sentence, highlight the words ‘place on the surface of Earth that is directly above the focus’ and ‘epicenter.’ ” “Let’s find out what happens when earthquakes occur below the ocean.” “Follow along as I read ...
Tsunami
A tsunami (plural: tsunamis or tsunami; from Japanese: 津波, lit. ""harbor wave"";English pronunciation: /tsuːˈnɑːmi/), also known as a seismic sea wave, is a series of waves in a water body caused by the displacement of a large volume of water, generally in an ocean or a large lake. Earthquakes, volcanic eruptions and other underwater explosions (including detonations of underwater nuclear devices), landslides, glacier calvings, meteorite impacts and other disturbances above or below water all have the potential to generate a tsunami. In being generated by the displacement of water, a tsunami contrasts both with a normal ocean wave generated by wind and with tides, which are generated by the gravitational pull of the Moon and the Sun on bodies of water.Tsunami waves do not resemble normal sea waves, because their wavelength is far longer. Rather than appearing as a breaking wave, a tsunami may instead initially resemble a rapidly rising tide, and for this reason they are often referred to as tidal waves, although this usage is not favored by the scientific community because tsunamis are not tidal in nature. Tsunamis generally consist of a series of waves with periods ranging from minutes to hours, arriving in a so-called ""wave train"". Wave heights of tens of meters can be generated by large events. Although the impact of tsunamis is limited to coastal areas, their destructive power can be enormous and they can affect entire ocean basins; the 2004 Indian Ocean tsunami was among the deadliest natural disasters in human history with at least 230,000 people killed or missing in 14 countries bordering the Indian Ocean.The Greek historian Thucydides suggested in his late-5th century BC History of the Peloponnesian War, that tsunamis were related to submarine earthquakes, but the understanding of a tsunami's nature remained slim until the 20th century and much remains unknown. Major areas of current research include trying to determine why some large earthquakes do not generate tsunamis while other smaller ones do; trying to accurately forecast the passage of tsunamis across the oceans; and also to forecast how tsunami waves would interact with specific shorelines.