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Chapter 10 Earthquakes
Chapter 10 Earthquakes

...  90% of Earthquakes occur within depths less than 100 km  Majority of Catastrophic Earthquakes occur within Depths less than 60-km Deep – 1964 Alaska EQ ---- 33 km from surface – 1995 Kobe, Japan--- 20 km from surface Magnitude vs Depth: a) Shallow: Up to 9.5 RM (Moment-Magnitude Scale) b) Interme ...
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... Seismograph- an instrument that detects and records seismic waves Seismogram- chart made by a seismograph in response to a earthquake Earthquakes produce three types of waves. Each waves travels at a different speed and causes the Earth’s crust to move in different ways: 1) P waves (primary waves) ...
Earthquakes - teamafrica
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... A seismometer is an instrument that senses the earth's motion; a seismograph combines a seismometer with recording equipment to obtain a permanent record of the motion. From this record scientists can calculate how much energy was released in an earthquake, which is one way to decide its magnitude. ...
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... New Zealand plate boundary models: In this activity, students make and/or observe two 3D moving models of the different tectonic plate boundaries under the North and South Islands representing the North Island subduction zone and the South Island Alpine Fault. Earthquake location: Students are intro ...
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Summing-up - Zanichelli
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... reference for measuring the magnitude M of an earthquake. All earthquakes are compared to a zero-level earthquake whose seismographic reading measures 0.001 millimeter at a distance of 100 kilometers from the epicenter. An earthquake whose seismographic reading measures x millimeters has a magnitude ...
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... The mud volcano and sulfur caldron areas, north of Yellowstone Lake, comprise the most acidic section of Yellowstone National Park. Mud pots are high-temperature geothermal hot springs or fumaroles of bubbling mud. The temperature of these areas, such as the Black Dragon Cauldron, can exceed 192 d ...
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... Time and again, wood-frame buildings such as suburban houses in California have been pronounced among the safest structures one could be in during an earthquake. Indeed, these buildings are constructed of light wood elements--wood studs for walls, wood beams and joists for floors, and wood beams and ...
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... knowledge acquired over the past events is used to forecast future events – Statistical Analysis  So, even the most elaborate models is inadequate because it is not based on information that might become available in real time about a specific earthquake that looms ahead ...
Earthquakes (Study Notes!)
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... Tsunami – large wave produced by an earthquake on the ocean floor. Aftershock – Earthquake that occurs AFTER a larger earthquake in the same area. Liquefaction – Occurs when an earthquake’s violent shaking suddenly turns loose, soft soil into liquid mud. Seismograph - instrument used to measure seis ...
Restless Earth Part 2: What are the effects and management issues
Restless Earth Part 2: What are the effects and management issues

... I know how we can predict and protect from volcanic eruptions. ...
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1880 Luzon earthquakes



The earthquakes of July 1880 in Luzon, the largest island of the Philippines, was one of the most destructive tremors on record in the history of the country. The shocks continued, with greater or less interruption, from the 14th to the 25th of the month, highlighted by three violent shaking events, which destroyed churches and other buildings, producing loss of life. Coinciding with the tectonic activity was an increased in volcanic activity in Taal Volcano in southwestern Luzon.The Luzon provinces of Manila, Cavite, Bulacan, Laguna, Pampanga, and Nueva Ecija, were the chief victims from the terrible convulsions with Manila and Laguna receiving the most damages. In many places, buildings were converted into shapeless heaps of ruins, and the materials of their prosperity buried beneath the rubbish.
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