The force of gravity on a certain object is calculated through the equation,
F = Gm1m2 / r²
where F is the force, G is a constant, m1 and m2 are masses of the object and Earth, respectively and r is the distance. Substituting the known values for this item,
F = (6.67 x 10⁻¹¹ N.m²/kg²)(1 kg)(5.98 x 10²⁴ kg)/ (6.4 x 10⁶ m)²
F = 9.37 N
Answer: 9.37 N
The answer to this question is letter C) Each student read
the meter stick from different angles.
The students might have been reading the meter stick facing
each other. So when one reads the meter stick as 18, the other student will
read the reverse image of the measurement. 18 and 82 can be easily mistaken
when reversed.
<h2>Correct answer:</h2>
![\boxed{v_{out}=2,85V}](https://tex.z-dn.net/?f=%5Cboxed%7Bv_%7Bout%7D%3D2%2C85V%7D)
<h2>Explanation:</h2>
We can use voltage divider to solve this problem that is defined as the passive linear circuit producing an output voltage
that is a fraction of its input voltage
. So we can use the formula:
![v_{out}=\frac{R_{2}}{R_{1}+R_{2}}v_{in}, \ where \ v_{in}=v_{s}=4V \\ \\ \therefore v_{out}=\frac{35}{14+35}(4) \\ \\ \therefore v_{out}=2,85V](https://tex.z-dn.net/?f=v_%7Bout%7D%3D%5Cfrac%7BR_%7B2%7D%7D%7BR_%7B1%7D%2BR_%7B2%7D%7Dv_%7Bin%7D%2C%20%5C%20where%20%5C%20v_%7Bin%7D%3Dv_%7Bs%7D%3D4V%20%5C%5C%20%5C%5C%20%5Ctherefore%20v_%7Bout%7D%3D%5Cfrac%7B35%7D%7B14%2B35%7D%284%29%20%5C%5C%20%5C%5C%20%5Ctherefore%20v_%7Bout%7D%3D2%2C85V)
Most white dwarfs are hotter than most giant starts and the reason why is because they are very dense, and because they are so dense that's why they are so hot.
Answer:
Convection cell
Explanation:
The convection current refers to the upward rising of the hot molten and less dense magma in the mantle. These currents are formed due to the heat supplied from the core of the earth. This upward movement of magma results in the movement of the lithospheric plates over the less dense viscous layer of the asthenosphere.
As the magma at the greater depth gets heated up, due to the increasing heat and pressure, it gets heated up and rises upward in the form of convection cells. As it rises upward, it cools and slowly moves laterally and eventually sinks after its density increases. This cycle repeats and forms the main mechanism for the plate tectonic movement.