Earthquake Insurance
... tends to be expensive. Your premium amount will depend on your location, along with the age and structural composition of your home. In addition, earthquake policies include a percentage deductible, generally ranging from 2 to 20 percent of total damages, which means you’ll still have significant ou ...
... tends to be expensive. Your premium amount will depend on your location, along with the age and structural composition of your home. In addition, earthquake policies include a percentage deductible, generally ranging from 2 to 20 percent of total damages, which means you’ll still have significant ou ...
preventive and mitigation measures
... If you are in a vehicle, pull over to a clear location, stop and stay there with your seatbelt fastened until the shaking stops. Avoid bridges, flyovers or ramps that might have been damaged by earthquake. If in costal area, move to higher ground and check tsunami warning. If you are in a hill ...
... If you are in a vehicle, pull over to a clear location, stop and stay there with your seatbelt fastened until the shaking stops. Avoid bridges, flyovers or ramps that might have been damaged by earthquake. If in costal area, move to higher ground and check tsunami warning. If you are in a hill ...
The Geography of Science
... ScienceDaily – earthquake proof house Search “Earthquake resistant building” in ‘Google Images.’ Extra: For more able students, the implications of China’s large scale dam construction program in the area may also be considered. See BBC News website mapping the earthquake zone The Asia-Pacific J ...
... ScienceDaily – earthquake proof house Search “Earthquake resistant building” in ‘Google Images.’ Extra: For more able students, the implications of China’s large scale dam construction program in the area may also be considered. See BBC News website mapping the earthquake zone The Asia-Pacific J ...
Click here for the "Dynamic Earth Vocabulary"
... Primary Wave: Known as a “p-wave”, is a type of seismic wave that causes particles in the ground to move in a push-pull motion similar to a coiled spring. Secondary Wave: Known as a “s-wave”, is a type of seismic wave that causes particles to move in an up-down motion. Rolling Wave: Known as a “r-wa ...
... Primary Wave: Known as a “p-wave”, is a type of seismic wave that causes particles in the ground to move in a push-pull motion similar to a coiled spring. Secondary Wave: Known as a “s-wave”, is a type of seismic wave that causes particles to move in an up-down motion. Rolling Wave: Known as a “r-wa ...
Earthquakes
... 3. Which type of earthquake wave moves the fastest? a. P-waves b. S-waves c. Love waves d. Rayleigh waves e. Permanent waves 4. Which type of earthquake wave could travel through a vacuum? a. P-waves b. S-waves c. surface waves d. all of the above e. none of the above 5. Which type of earthquake bod ...
... 3. Which type of earthquake wave moves the fastest? a. P-waves b. S-waves c. Love waves d. Rayleigh waves e. Permanent waves 4. Which type of earthquake wave could travel through a vacuum? a. P-waves b. S-waves c. surface waves d. all of the above e. none of the above 5. Which type of earthquake bod ...
1906 San Francisco Earthquake
... in the process, generating seismic waves that produce shaking. 1906 earthquake essentially turned off earthquakes of magnitude about 6 and larger for the next 73 years. Central California has been experiencing a seismically quiet period caused by stress relaxation after 1906. The region may slowly b ...
... in the process, generating seismic waves that produce shaking. 1906 earthquake essentially turned off earthquakes of magnitude about 6 and larger for the next 73 years. Central California has been experiencing a seismically quiet period caused by stress relaxation after 1906. The region may slowly b ...
Exercise 1
... 7) Explain the situations that cause the formation of arcs, mountains and magnetic anomalies during earthquakes, mentioning the types of movements involved. 8) In which direction and at what velocity is the Indian plate is moving currently? 9) Explain the theory of continental drift and the evidence ...
... 7) Explain the situations that cause the formation of arcs, mountains and magnetic anomalies during earthquakes, mentioning the types of movements involved. 8) In which direction and at what velocity is the Indian plate is moving currently? 9) Explain the theory of continental drift and the evidence ...
Earthquakes * Day 1 - NVHSEarthScienceOlsen
... • To describe the location of earthquakes, we use the terms focus and epicenter • When analyzing how earthquakes travel, we talk about the 3 main types of earthquake waves: s, p, and surface – These waves travel at different speeds and cause differing amounts of destruction – The magnitude of an ear ...
... • To describe the location of earthquakes, we use the terms focus and epicenter • When analyzing how earthquakes travel, we talk about the 3 main types of earthquake waves: s, p, and surface – These waves travel at different speeds and cause differing amounts of destruction – The magnitude of an ear ...
Earthquake Resistant Buildings
... countries to educate and familiarize people on what to do in the event of an earthquake . •Governments of earthquake-prone countries also use posters and signs to warn people about areas that are prone to the effects of earthquakes e.g. coastal areas where tsunamis can occur . ...
... countries to educate and familiarize people on what to do in the event of an earthquake . •Governments of earthquake-prone countries also use posters and signs to warn people about areas that are prone to the effects of earthquakes e.g. coastal areas where tsunamis can occur . ...
Earthquake Lab Walkthrough
... 1. In what order do earthquake waves appear on a seismogram? 2. How many points are needed to determine the epicenter of an earthquake? Why? ...
... 1. In what order do earthquake waves appear on a seismogram? 2. How many points are needed to determine the epicenter of an earthquake? Why? ...
Performance Task (continued)
... Ocotillo, California, leaving virtually no damage. But in 1906, an earthquake with an estimated 8.2 on the same scale devastated the city of San Francisco. Does twice the measurement on the Richter scale mean twice the intensity of the earthquake? In 1935, Charles Richter developed a method to compa ...
... Ocotillo, California, leaving virtually no damage. But in 1906, an earthquake with an estimated 8.2 on the same scale devastated the city of San Francisco. Does twice the measurement on the Richter scale mean twice the intensity of the earthquake? In 1935, Charles Richter developed a method to compa ...
ES Ch 2 NOTES Earthquakes
... location where an earthquake begins. 2) The point directly above the focus on the _________________ is the epicenter. 3) The crust breaks at the focus and the stored ______________ releases and travels outward in all directions as seismic waves. ...
... location where an earthquake begins. 2) The point directly above the focus on the _________________ is the epicenter. 3) The crust breaks at the focus and the stored ______________ releases and travels outward in all directions as seismic waves. ...
Image courtesy of US Geological Survey
... Felt by all; many frightened and run outdoors, walk unsteadily. Windows, dishes, glassware broken; books fall off shelves; some heavy furniture moved or overturned; a few instances of fallen plaster. ...
... Felt by all; many frightened and run outdoors, walk unsteadily. Windows, dishes, glassware broken; books fall off shelves; some heavy furniture moved or overturned; a few instances of fallen plaster. ...
2010 Pichilemu earthquake
The 2010 Pichilemu earthquake (Spanish: Terremoto de Pichilemu de 2010), also known as the Libertador O'Higgins earthquake, was a 6.9 MW intraplate earthquake that struck Chile's O'Higgins Region on 11 March 2010. The earthquake was centred 15 kilometres (9.3 mi) northwest of the city of Pichilemu, according to the University of Chile Seismological Service.The earthquake was caused by increased regional stress arising from an earthquake on 27 February, centered offshore Maule Region, which was felt throughout central Chile. The 11 March earthquake was at first thought to be an aftershock from the 27 February event, but University of Chile Seismologist Jaime Campos identified it as an ""independent earthquake"". The Hawaii-based Pacific Tsunami Warning Center pointed out the possibility of local tsunamis within 100 kilometres (62 mi) of the epicentre, although small, but violent waves were seen in the Pichilemu and Bucalemu area. One person was reported dead. At least eleven aftershocks immediately followed, causing panic throughout coastal towns between the Coquimbo and Los Lagos regions.The earthquake was specially destructive in the epicentre town, Pichilemu, capital of Cardenal Caro Province. The city hosts five National Monuments of Chile, of which two, the Agustín Ross Park and the Agustín Ross Cultural Centre, were seriously damaged by the earthquake. It also damaged the villages of La Aguada and Cardonal de Panilonco. Rancagua, the capital of O'Higgins Region, was also damaged, leading President Sebastián Piñera to declare a catastrophe state in O'Higgins Region.