# What Three Factors Do Geologists Use To Determine Earthquake Risk

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## How do geologists determine earthquake risk?

Geologists measure changes in the amount of pressure or stress on faults to see if pressure is building up. … Geologists can determine earthquake risk by locating where faults are active and where past earthquakes have occured.

## What is the main factor in determining the risk that a location might have an earthquake quizlet?

The main factor in determining the risk that a location might have on an earthquake is plate boundaries.

## What two factors are used to determine the probability of earthquake?

Scientists estimate earthquake probabilities in two ways: by studying the history of large earthquakes in a specific area and the rate at which strain accumulates in the rock. Scientists study the past frequency of large earthquakes in order to determine the future likelihood of similar large shocks.

## What are four indicators that seismologists use to determine earthquake risk?

What are four indicators that Seismologists use to determine Earthquake Risk?

Measures the total amount of energy released by an earthquake energy released depends on:
• The size of the fault
• The motion that occurs
• The strength of the rocks.

## What 2 factors do geologists consider when determining earthquake risk for a region?

What two factors do geologists consider when determining earthquake risk for a region? Geologists can determine earthquake risk by locating where faults are active and where past earthquakes have occurred.

## What are the 3 fault types?

There are three main types of fault which can cause earthquakes: normal reverse (thrust) and strike-slip.

## What do a data geologist use to see where earthquakes are most common?

What data do geologists use to see where earthquakes are most common? They look for fault lines and plate boundaries.

## What are four instruments that are used to detect movement along faults?

Four instruments that are used to monitor faults are creep meters laser-ranging devices tiltmeters and satellites. A creep meter uses a wire stretched across a fault to measure sideways movement of the ground. A laser-ranging device uses a laser beam bounced off a reflector to detect even slight fault movements.

## What are four ways that earthquakes cause damage?

The damage caused by earthquakes is from ground shaking ground rupture landslides tsunamis and liquefaction.

## Can geologists determine the statistical probability of when a major earthquake will take place?

Neither the USGS nor any other scientists have ever predicted a major earthquake. … USGS scientists can only calculate the probability that a significant earthquake will occur in a specific area within a certain number of years.

## What is the risk of earthquakes?

Earthquake risk is the probable building damage and number of people that are expected to be hurt or killed if a likely earthquake on a particular fault occurs. Earthquake risk and earthquake hazard are occasionally incorrectly used interchangeably.

## Are there clues and considerations in identifying earthquake hazards?

Because nearly all earthquakes occur on faults determining seismic risks on a finer scale largely consists of identifying mapping and studying active faults in each state or region.

## How do scientist monitor and predict earthquakes?

Seismic monitoring utilizes sensitive seismographs to record the ground motion from seismic waves created by earthquakes or other sources. Seismograms from seismic monitoring stations can be used to determine the location origin time and magnitude (as well as other characteristics) of earthquakes.

## What are some methods for predicting earthquakes?

However there are still some ways of monitoring the chances of an earthquake:
• Laser beams can be used to detect plate movement.
• A seismometer is used to pick up the vibrations in the Earth’s crust. An increase in vibrations may indicate a possible earthquake.
• Radon gas escapes from cracks in the Earth’s crust.

## How is radon used to predict earthquakes?

In the last decade several studies have concluded that elevated concentrations of radon gas in soil or groundwater could be the sign of an imminent earthquake. It is believed that the radon is released from cavities and cracks as the Earth’s crust is strained prior to the sudden slip of an earthquake.

## What are the factors that affect the disaster risks of earthquake?

Ground shaking is the primary cause of earthquake damage to man-made structures. Many factors influence the strength of earthquake shaking at a site including the earthquake’s magnitude the site’s proximity to the fault the local geology and the soil type.

## How does a Regions geology affect earthquake risk?

Two important local geologic factors that affect the level of shaking experienced in earthquakes are (1) the softness of the surface rocks and (2) the thickness of surface sediments. … Areas of intense shaking due to proximity to probable earthquakes were mapped in the SCEC Phase II Report.

## Why is there a need for us to identify areas which are prone to earthquake and other tectonic related disaster?

Identification of prone to earthquakes areas helps to take the preparation for that upcoming possibility of the earthquake. If any area is identified as earthquake-prone the buildings bridges and etc are made earthquake resistant. Extra care is taken in case of transportation and livelihood of people.

## What are the three main types of earthquake waves?

There are three major kinds of seismic waves: P S and surface waves. P and S waves together are sometimes called body waves because they can travel through the body of the earth and are not trapped near the surface.

## What are the 3 types of stress in geology?

There are three types of stress: compression tension and shear.

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## What causes earthquakes?

Earthquakes are the result of sudden movement along faults within the Earth. The movement releases stored-up ‘elastic strain’ energy in the form of seismic waves which propagate through the Earth and cause the ground surface to shake.

## How Geologists use data from seismographs to learn about earthquakes?

Seismographs detect seismic waves and use this data to study the length and depth of the waves. In this way geologists can determine the location of the fault and mark it as an earthquake risk area.

## Which strategy do geologists use to locate the center of an earthquake?

Geologists use seismic waves to locate the center of an earthquake.

## What are three ways in which geologists use seismographic data?

What are three ways in which geologists use seismographic data? Geologists use seismographic data to map faults monitor changes along faults and to try to predict earthquakes.

## What does the data from seismographs tell geologists when making maps of faults?

How do geologists use seismographic data to make maps of faults? Seismographs detect the reflected seismic waves and geologists use this data to map the length and depth of the fault. Why do geologists collect data on friction along the sides of faults? So they can try to predict the probability of a large earthquake.

## How do geologists calculate movement along a fault?

htm. The rate of movement along a plate boundary can be determined by measuring the displacement of rocks or other features along the boundary. … The San Andreas Fault has cut through this rock unit dividing it into two parts which are now widely separated on opposite sides of the fault.

## What are three effects of earthquakes?

The effects from earthquakes include ground shaking surface faulting ground failure and less commonly tsunamis.

## Did you know facts about earthquakes?

• There are several million earthquakes annually. …
• An earthquake can affect the length of a day. …
• San Francisco is moving towards L.A. …
• Standing water smells before an earthquake. …
• Internal waves post-quake are called “seiches”

## What are the 5 effects of earthquakes?

The primary effects of earthquakes are ground shaking ground rupture landslides tsunamis and liquefaction. Fires are probably the single most important secondary effect of earthquakes.

## How do you determine the magnitude of an earthquake?

Magnitude is expressed in whole numbers and decimal fractions. For example a magnitude 5.3 is a moderate earthquake and a 6.3 is a strong earthquake. Because of the logarithmic basis of the scale each whole number increase in magnitude represents a tenfold increase in measured amplitude as measured on a seismogram.

## How can you determine the epicenter of an earthquake using data from seismic stations worldwide?

Scientists use triangulation to find the epicenter of an earthquake. When seismic data is collected from at least three different locations it can be used to determine the epicenter by where it intersects. Every earthquake is recorded on numerous seismographs located in different directions.

## What do you think is the importance of determining the epicenter of an earthquake?

The main importance in determining the epicentre is so that the fault that ruptured causing the earthquake can be identified. … If the fault is previously unknown (such as the 2010 Canterbury earthquake) then it is important because it means that the hazard models for the area need improvement.

## What are the factors that pose a high risk to landslide?

These factors include both natural events such as geological weathering and erosion and human-related activities such as deforestation and changes made to the flow of groundwater. Destruction of vegetation by droughts fires and logging has been associated with increased risk for landslides.

## How can you determine whether or not you live in an area where an earthquake is likely to occur?

You should consider the following factors when deciding whether or not to get earthquake insurance: proximity to active earthquake faults seismic history of the region (frequency of earthquakes) time since last earthquake building construction (type of building and foundation) architectural layout materials used …

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