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Tom [10]
4 years ago
15

What would happen if earth suddenly lost its magnetic field

Geography
2 answers:
Fiesta28 [93]4 years ago
6 0

Answer:

From what I know, compasses and other magnetic things would not work.

Explanation:

Marrrta [24]4 years ago
4 0

Answer:

The world would collapse I think?

Explanation:

Just my opinion what would happen I may not be right tho.

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is when it contributes towards the contamination and destruction of natural habitats and the wildlife that live in those habitats by exposing them to harmful chemicals that would otherwise not be present over the natural course of things

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Asteroid A has a mass of 7.80×1020 kilograms (kg), and asteroid B has a mass of 3.70×1018 kg. Assuming that the same force was a
PtichkaEL [24]

Answer:

The ratio of asteroid-A’s acceleration to asteroid-B’s acceleration is 37:7800.

Explanation:

Mass of asteroid-A = m =7.80\times 10^{20} kg

Mass of asteroid-B = m' = 3.70\times 10^{18} kg

As we know , Force = mass × Acceleration

1) Force on an asteroid-A

F = m\times a

where , a is the acceleration due to force applied on asteroid-A

2) Force on an  asteroid-B

F' = m'\times a'

where , a' is the acceleration due to the force applied on asteroid-B

Same force is exerted on the both the asteroids say F.

F = F'

m\times a=m'\times a'

\frac{a}{a'}=\frac{3.70\times 10^{18} kg}{7.80\times 10^{20} kg}=\frac{37}{7800}

The ratio of asteroid-A’s acceleration to asteroid-B’s acceleration is 37:7800.

5 0
3 years ago
Battles over shipping routes often focus on the control of
NARA [144]

Answer:

the silk road

Explanation:

Wasn't alot of information but i think this i right.

7 0
4 years ago
Read 2 more answers
A sediment core is removed from the floor of an inland sea. The sea has been in existence, off and on, throughout the entire tim
KatRina [158]

Answer:

A. volcanic ash layers were regularly interspersed between the sedimentary strata.

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  • In order to assign the absolute dates to the fossil records of the sedimentary core that have been deposited n the inland areas of the seafloor bottoms.
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