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Ostrovityanka [42]
3 years ago
5

The boundary between the crust and mantle is marked by a seismic-velocity discontinuity called

Physics
2 answers:
Minchanka [31]3 years ago
7 0

The boundary between the crust and mantle is marked by a seismic-velocity discontinuity is called Mohorovicic discontinuity.

Mohorovicic discontinuity was discovered by Andrija Mohorovicic in 1909 who was a Croatian seismologist. He realized that the velocity of a seismic wave is related to the material's density where it is moving through. He decoded that the acceleration of the seismic waves that are observed within outer shell of the earth is a compositional change. Thus, the acceleration should be caused by a material of higher density.

oksano4ka [1.4K]3 years ago
3 0

Mohorovicic discontinuity is your answer

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If a bus travel 200 km in 45 minutes calculate the speed in kilometre per minute​
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An airplane flies with a velocity of 750. kilometers
viktelen [127]

Answer:

650 km/hr

Explanation:

Draw a right triangle from (0.0) (Point A) down 30 degrees and to the right for a length of 750 (Point B).  Then draw a line from B up to the x axis to make a right angle (Point C).  Use the cosine function to find line AC, the vector portion of AB that lies of the x (East) axis.  Cosine(30)= Adjacent/Hypotenuse.

Cos(30) = AC/750

750*(cos(30)) = AC

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5 0
2 years ago
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Design an experiment to test the rate at which temperature changes for two different masses (amounts) of water.
mrs_skeptik [129]

Answer:Experimental Question:  How does the amount of a substance affect the rate at which temperature changes?

It depends on the conductivity of the material. If the shift is extreme, the temperature near the heating / cooling source will be similar to the temperature of the heating / cooling source and it will take time for the remainder of the material to rise to temperature. It will depend on the conductivity of the material.

Hypothes is:  

Materials  List:

• digital stopwatch

• 250ml beaker

• rubber bung

• thermometer

• bunsen burner

• tripod

• gauze

• retort stand and clamp

• goggles

Safety Procedures *:

1. Adult supervision is required.  

2. Wear safety goggles, apron, and closed-toe shoes.  

3. Do not wear baggy sleeves or dangling jewelry. Tie long hair back.  

4. Use hot pads or oven mitts to handle hot objects.  

5. Do not reach over a hot burner.  

6. Do not leave the experiment unattended.  

7. Clean up spills immediately.  

8. Report any injuries to your Learning Coach or adult supervisor immediately

Experimental Procedures :

• Fill an empty beaker with exactly 150ml of water (check side-scale of beaker)

• Set up apparatus as shown above. Ensure the thermometer is about 2cm above the bottom of the beaker.

• Light the bunsen burner and put on a blue flame. Heat up the water.

• When the temperature on the thermometer has reached 90°C, immediately switch off the burner.

• Start the stopwatch and time for 5.0 minutes.

• Read the thermometer value at the 5.0 minute mark.

• Before repeating the experiment, check the level of water is still 150ml

Data Table:  

Start Temperature of Water (°C) Temperature after 5min (°C) Drop in Temperature

(°C) Average Rate of Cooling x 1000 (°C/s)

80 70 10 17

75 66 9 15

70 62 8 13

65 59 6 10

60 55 5 8

Analysis:  

Conclusions : There is a strong correlation between the average rate of cooling and the start temperature: the greater the start temperature, the  faster the average rate of cooling.

Explanation:

use quillbot or this will be considered plagerism

3 0
2 years ago
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