answersLogoWhite

0


Best Answer

Isoseismic lines are contour lines that are drawn on a map joining points of equal seismic intensity. They will firm a series of broadly concentric circles centred on the point or area of maximum seismic activity which is commonly the earthquake epicentre.

For more information on this topic and on how seismologists locate the epicentre of an earthquake, please see the related questions.

User Avatar

Wiki User

13y ago
This answer is:
User Avatar

Add your answer:

Earn +20 pts
Q: How do you interpret isoseismic lines to determine damage and location of epicenter?
Write your answer...
Submit
Still have questions?
magnify glass
imp
Related questions

What is minimum number of seismic stations needed to determine the location of an earthquakes epicenter?

The minimum number of seismic stations needed to determine the location of an earthquake's epicenter is THREE.


What is the minimum number of seismic stations needed to determine the location of an earthquake epicenter?

The minimum number of seismic stations needed to determine the location of an earthquake's epicenter is THREE.


What is the minimum number of seismic stations needed to determine the location of an earthquakes epicenter?

The minimum number of seismic stations needed to determine the location of an earthquake's epicenter is THREE.


Why are seismographs stations needed to determine the location of an epicenter?

Three seismograph stations are needed to determine the location of an epicenter because each seismograph can determine distance to the epicenter but not direction. The point where the three circles intersect is the epicenter of the earthquake. +++ Focus - not epicentre, which is the point of maximum movement on the surface above the slip itself.


Why three seismograph stations are needed to determine the location of an epicenter?

Three seismograph stations are needed to determine the location of an epicenter because each seismograph can determine distance to the epicenter but not direction. The point where the three circles intersect is the epicenter of the earthquake. +++ Focus - not epicentre, which is the point of maximum movement on the surface above the slip itself.


What is the minimum number of seismograph station required to determine the location of an earthquake epicenter?

56


What is the minimum number of seismic stations needed to determine the location of an earthquake and epicenter?

you need to have 3 seismic stations to triangulate the location of the earthquake and remember a earthquake can be from the inside of the earth but not necessarily at the epicenter because no epicenter is a straight line down.


What is the minimum number of seismic stations needed to locate the epicenter of an earthquake?

The minimum number of seismic stations needed to determine the location of an earthquake's epicenter is THREE.


How could you find the location of the epicenter?

how do seismologist know how to find the location of a epicenter


How does triangulation determine the epicenter?

To locate the epicenter you use the speed of waves that travel from the epicenter to the seismic sensor locations. With two sensors you are able to narrow the location to two places (when on a surface using intersecting hyperbolas). With a third sensor you have the location on a surface and below ground. This third sensor is why they call it tri - angulation but the angles are hard to find without HS trigonometry and other mathematics.


Why is a seismic record from three locations needed to determine the position of an epicenter?

It is recorded from three differences because you can do two tests and they can meet at one spot but it may not be the actual epicenter. They do the third test to be ssure they have the right spot or epicenter.


how do scientists determine earthquake location and how do they use this information?

Scientists use devices called Seismographs to determine the epicenter of an earthquake. If 3 or more seismographs detect an earthquake, seismic wave activity can be measured and quantified and then cross-referenced with other data (the primary and secondary seismic waves) to determine the earthquake's location.