# Earthquake time travel graph calculator

**Earthquake**-station distances need to be calculated separately by first picking P and S arrival **times** on seismograms, and then using a P and S wave **travel** **time** **graph** to determine the distance. We are showing the 1000 latest **earthquakes** with a magnitude of at least 5. To plot a different selection of events, visit Interactive **Earthquake** Browser.

The National Seismic Hazards Mapping project provides an online Web tool for determining the probability of a large **earthquake** within 50 kilometers (~31 miles) of a specific location in the United States over a certain **time** period. The calculation is based on the latest available information from seismic hazard data. However, asking if it's safe to **travel** somewhere because of recent. This **time** difference is called the S minus P (S – P) **time** and is like the Walk – Run [or Slow Walk – Walk] **time** of our simulation. Record this difference, in seconds, on Data Table 2. Repeat this step, and record the difference in arrival times. Recover all materials and return to the classroom. **Calculating** the Origin **Time** of the **Earthquake** (10 pts) The first seismic waves felt in Reno, Nevada occurred at 9:31:45 am (hrs:minutes:seconds). Using this **time**, the information gathered in Part A, and the **travel time** curve, to **calculate** the exact **time** (to the nearest second), when the **earthquake** originated. Explain how you arrived at your answer. massive **earthquakes** occurring.

Basic worksheet that leads students through the processes of **calculating** distances to an epicenter, **travel** times for P & S waves and origin times of an **Earthquake**. Leads students through skills such as subtracting **time** and using a **travel time graph**.

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**Earthquake** Live Map. View the latest **earthquakes** on the interactive map above, displaying the magnitude, location, depth and the event **time**. The information is provided by the USGS **Earthquake** Hazards Program. The **earthquake** is a shaking of the Earth's surface, caused by the displacement of a part of the Earth's crust and the sudden release. Basic Math. Math **Calculator**. Step 1: Enter the expression you want to evaluate. The Math **Calculator** will evaluate your problem down to a final solution. You can also add, subtraction, multiply, and divide and complete any arithmetic you need. Step 2: Click the blue arrow to submit and see your result!.

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**Earthquakes** Practice: **Time**-**travel graphs** and Seismographs 1. How long will it take a P wave to **travel** 8000km? _____ 2. A P wave arrives at 3:00pm. If the S waves arrive at the seismograph station at 3:10pm, approximately how far was the **earthquake** from the station? _____ 1. How long does it take for a primary wave to **travel** 2000 km? _____ 2. TESC discusses how to use this **time travel graph**, **calculate** S-P arrival times and epicenter distance from a seismogram. Used to triangulate the **earthquake's**.

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Enter the two magnitudes you want to compare - for our example these are 5.8 and 7.1. We find out that a magnitude 7.1 is 20 **times** bigger (on a seismogram, in terms of amplitudes), and ~89 **times** stronger (in terms of energy release) than a 5.8 magnitude. the amplitude of shaking is 10 **times** larger.

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Plain **Graph** Paper Author: incompetech.com Subject: Plain **Graph** Paper Created Date: 7/6/2010 11:33:15 PM. ASCE 7-10. These gridded text files contain S S, S 1, PGA, C RS, and C R1 parameter values from the 2010 ASCE 7 Standard. Please note that these values will not exactly match those provided by the U.S. Seismic Design Maps. The Maps interpolate the underlying probabilistic and deterministic ground motions, as well as the risk coefficients. A **travel**-**time** curve is a **graph** of the **time** that it takes for seismic waves to **travel** from the epicenter of an **earthquake** (**time** and distance = zero) to seismograph stations varying distances away. The curves are the result of analyzing seismic waves from thousands of **earthquakes**, received by hundreds of seismic stations around the world. **Calculator**: Generate a listing of phase arrival times at YOUR seismic station. Recent **Earthquakes**. Specify **Earthquake**. **Graph** of seismic **travel time** in minutes versus distance in degrees for an **earthquake** at the Earth's surface. Table of P and S minus P times versus distance in degrees. Composite ANSS list of **earthquakes** for the past 14 days.

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This is all the data it takes to enable **time**-slicing. Given the point in **time** t from which we wish to query our **graph** G, we can easily filter to include only the edges which were valid at **time** t. Using the bind parameter @queryTime with value t in the query below, we should get all the valid paths. 1.

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A **travel** **time** curve is a **graph** of the **time** that it takes for seismic waves to **travel** from the epicenter of an **earthquake** to seismograph stations at varying distances away. The velocity of seismic waves through different materials yield information about Earth's deep interior. IRIS' **travel** **times** graphic for the 1994 Northridge, CA **earthquake**. **Earthquake Travel Time** Information and **Calculator Calculator** : Generate a listing of phase arrival times at YOUR seismic station Recent **Earthquakes** Specify **Earthquake Graph** of seismic **travel time** in minutes versus distance in degrees for an **earthquake** at the Earth's surface Table of P and S minus P <b>times</b> versus distance in degrees.

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**Earthquake** **Travel** **Time** Information and **Calculator** **Calculator**: Generate a listing of phase arrival **times** at YOUR seismic station Recent **Earthquakes** Specify **Earthquake** **Graph** of seismic **travel** **time** in minutes versus distance in degrees for an **earthquake** at the Earth's surface Table of P and S minus P **times** versus distance in degrees. This mileage **calculator** estimates the number of driving miles between two locations in the United States. home ... Use the following mileage **calculator** to determine the **travel** distance, in terms of miles, and **time** taken by car to **travel** between two locations in the United States, disregarding traffic conditions. From: To: Related Gas Mileage.

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TESC discusses how to use this **time travel graph**, **calculate** S-P arrival times and epicenter distance from a seismogram. Used to triangulate the **earthquake's**.

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Job Summary: Engineering. 2. **Calculate** the difference between the arrival **time** of the P - wave and the S- wave . **Time** Difference = 6.0 − 1.0 = 5.0 min 3. Refer to the **Earthquake Time Travel Graph**. Determine the location on the **graph** where the two curves have a **time** difference equal to the **time** difference you previously calculated.

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**Earthquake Travel Time** Information and **Calculator Calculator** : Generate a listing of phase arrival times at YOUR seismic station Recent **Earthquakes** Specify **Earthquake Graph** of seismic **travel time** in minutes versus distance in degrees for an **earthquake** at the Earth's surface Table of P and S minus P <b>times</b> versus distance in degrees. How to Use an **Earthquake Travel Time Graph** An **Earthquake Travel Time Graph** can be used to find several different variables. Let’s start with: **TRAVEL TIME** or DISTANCE from EPICENTER (Given one, find the other) Sample Problem: A seismic station is 3000 kilometers from the epicenter of an **earthquake**. This simple relation says that the **travel time** curve is a straight line which has a slope of \(1/v_2\) and an intercept of \(t_i\).This intercept **time** is the **time** where the refraction line extends to intercept the \(y\)-axis –above the source position–.This is not a real “**time**” -.

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read over to the **Travel Time** axis. For example, a P-wave **traveling** 7200 km would take a **travel time** of 10:40 (10 min. 40 sec.) to go this distance. The slower S-wave would take 19:20 (19 min. 20 sec.) to go the same distance. Given the **travel time** of a seismic wave, the distance from the epicenter can be determined. Have your students read a simple **time**-distance **graph** that shows the relationship between the arrival times of P and S **earthquake** waves and the distance the **earthquake** is away. This is a fundamental data skill and will help them understand other **earthquake** epicenter location activities. Job Summary: Engineering. 2. **Calculate** the difference between the arrival **time** of the P - wave and the S- wave . **Time** Difference = 6.0 − 1.0 = 5.0 min 3. Refer to the **Earthquake Time Travel Graph**. Determine the location on the **graph** where the two curves have a **time** difference equal to the **time** difference you previously calculated.

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**Travel**-**time** curves are **graphs** that indicate how long it takes each type of seismic wave to **travel** a distance measured on Earth's surface. The difference between the S-wave arrival **time** and the P-wave arrival **time** corresponds to the distance of the seismograph station from the **earthquake** focus. This **time** difference can be converted.

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Be sure to review both the textbook and the example before attempting this lab. A. Locating the **Earthquake** Epicenter (50 pts) 1. Estimate to the nearest half-second the S-P interval from the three seismograms shown in Figures 1, 2 and 3. After, use the S-P **travel time** curve (Fig. 4) to determine the distance between the epicenter and the city.

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How to Use the **Earthquake Travel Time Graph** (Page 11 of the Earth Science Reference Tables). The **graph** on page 11 can be used to find several different variables. ... Saki, then down the road to her other friend Kam. The **graph** shows her journey. **Calculate** each of the following. (a) Her total distance travelled. (b) Her final displacement. (c.

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Determining the **Earthquake** Distance. You can now determine the distance from each seismic recording station to the **earthquake**’s epicenter using the known times of **travel** of the S and P waves.Examine the **graph** to the right, a **graph** of seismic wave **travel** times. There are three curves on the **graph**: The upper curve shows S wave **travel**-**time**.

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The table shows the distance a seismic wave can **travel** based on its distance from an earthquakeÕs epicenter. Draw a scatter plot and a curve of best fit that relates distance to **travel** **time**. Then determine approximately how far from the epicenter the wave will be felt 8.5 minutes after the **earthquake** occurs. **Travel** **Time** (min) 1 2 5 7 10 12 13.

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What is meant by **travel time** in terms of locating an **earthquake**? You can observe the P- and S-wave arrivals on a seismogram to **calculate** how far away an **earthquake** was from your station. A traveltime curve is a **graph** of arrival times, commonly P or S waves, recorded at different points as a function of distance from the seismic source. **Calculator**: Generate a listing of phase arrival times at YOUR seismic station. Recent **Earthquakes**. Specify **Earthquake**. **Graph** of seismic **travel time** in minutes versus distance in degrees for an **earthquake** at the Earth's surface. Table of P and S minus P times versus distance in degrees. Composite ANSS list of **earthquakes** for the past 14 days. .

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Select Page. tsunami **travel time calculator**. by | Mar 3, 2021 | Uncategorized | 0 comments | Mar 3, 2021 | Uncategorized | 0 comments.

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How to Use the **Earthquake Travel Time Graph** (Page 11 of the Earth Science Reference Tables). The **graph** on page 11 can be used to find several different variables. ... Saki, then down the road to her other friend Kam. The **graph** shows her journey. **Calculate** each of the following. (a) Her total distance travelled. (b) Her final displacement. (c. Once you’ve calculated the S-P Interval **Time**/Lag **Time** for this Seismic Station, determine how far away this station was from the Epicenter of the **earthquake**. From the S-P interval a seismologists can determine the to an **earthquake**. Given three differently located seismic stations, the **time**-**travel graph** can be used to determine the position of. This simple relation says that the **travel time** curve is a straight line which has a slope of \(1/v_2\) and an intercept of \(t_i\).This intercept **time** is the **time** where the refraction line extends to intercept the \(y\)-axis –above the source position–.This is not a real “**time**” -. **Calculator**: Generate a listing of phase arrival times at YOUR seismic station. Recent **Earthquakes**. Specify **Earthquake**. **Graph** of seismic **travel time** in minutes versus distance in degrees for an **earthquake** at the Earth's surface. Table of P and S minus P times versus distance in degrees. Composite ANSS list of **earthquakes** for the past 14 days. The information is then used to determine **earthquake** locations, the subsurface structures and etc. ... o Arrival times can be represented on a **travel**-**time graph** or T-X plot, that is P-wave arrival times ... o From the **travel**-**time** curve we can **calculate**: o velocities of P-wave propagation through layers 1 and 2 (V 1 and V 2).

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Seismologists have just registered an **earthquake** in Seward, Alaska, that is big enough to produce a tsunami. The ocean depth is 4,000 meters. Use the wave speed formula to approximate the tsunami's speed. Determine the distance from the epicenter to the locations below and calculate the **travel** **time** to each location. Please insert your.

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Annual **Earthquakes**. In a single year, on average, more than 900,000 **earthquakes** are recorded and 150,000 of them are strong enough to be felt. Each year about 18 **earthquakes** are major with a Richter magnitude of 7.0 to 7.9, and on average one **earthquake** has a magnitude of 8 to 8.9. Magnitude 9 **earthquakes** are rare.

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A **travel time** curve is a **graph** of the **time** that it takes for seismic waves to **travel** from the epicenter of an **earthquake** to seismograph stations at varying distances away. The velocity of seismic waves through different materials yield information about Earth's deep interior. IRIS' **travel** times graphic for the 1994 Northridge, CA **earthquake**. By looking at the **time** between the arrivals of the P- and S-waves, one can determine the distance to the **earthquake** from that station, with longer **time** intervals indicating longer distance. These distances are determined using a **travel**-**time** curve, which is a **graph** of Pand S-wave arrival **times** (see Figure 13. 11).

**Calculator**. How much bigger is a magnitude 8.7 **earthquake** than a magnitude 5.8 **earthquake**? An explanation of the magnitude of an **earthquake** versus the strength, or energy release, of an **earthquake**... with a little bit of math. How much bigger is a.

Make sure you subtract any rests or stops you made from the total trip duration. If the total distance travelled was 500 miles and the **time** it took you was 5 hours, then your average speed was 500 / 5 = 100 miles per hour (mph). If the distance was 300 kilometers and it took you 5 hours to cover it, your speed was 300 / 5 = 60 km/h (kilometers.

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