Answer:4-strikes the plane at same time as the other body
Explanation:
Given
If both bodies is falling on a horizontal plane and second body is given an acceleration in horizontal direction then it does not change the time to reach the Horizontal Plate as there is no change in vertical direction.
Horizontal acceleration will give only horizontal range and horizontal velocity.
Answer:
given,
mass of the skier = 70.1 Kg
angle with horizontal, θ = 8.6°
magnitude of the force,F = ?
a) Applying newton's second law
velocity is constant, a = 0
![F_{rope} = m g sin\theta](https://tex.z-dn.net/?f=F_%7Brope%7D%20%3D%20m%20g%20sin%5Ctheta)
![F_{rope} = 70.1\times 9.8\times sin 8.6^0](https://tex.z-dn.net/?f=F_%7Brope%7D%20%3D%2070.1%5Ctimes%209.8%5Ctimes%20sin%208.6%5E0)
![F_{rope}= 102.73\ N](https://tex.z-dn.net/?f=F_%7Brope%7D%3D%20102.73%5C%20N)
b) now, when acceleration, a = 0.135 m/s²
velocity is constant, a = 0.135 m/s₂
![F_{rope} = m g sin\theta+ma](https://tex.z-dn.net/?f=F_%7Brope%7D%20%3D%20m%20g%20sin%5Ctheta%2Bma)
![F_{rope} = 70.1\times 9.8\times sin 8.6^0+70.1\times 0.135](https://tex.z-dn.net/?f=F_%7Brope%7D%20%3D%2070.1%5Ctimes%209.8%5Ctimes%20sin%208.6%5E0%2B70.1%5Ctimes%200.135)
![F_{rope}= 112.19\ N](https://tex.z-dn.net/?f=F_%7Brope%7D%3D%20112.19%5C%20N)
Answer:
Despite being such prominent feature on our planet, much of the mid-ocean ridge system remains a mystery. While we have mapped about half of the global mid-ocean ridge in high resolution, less than one percent of the mid-ocean ridge has been explored in detail using submersibles or remotely operated vehicles. so therefore we do not have enough information about them to know what will happen
Explanation:
A mid-ocean ridge or mid-oceanic ridge is an underwater mountain range, formed by plate tectonics. This uplifting of the ocean floor occurs when convection currents rise in the mantle beneath the oceanic crust and create magma where two tectonic plates meet at a divergent boundary. Mid-ocean ridges occur along divergent plate boundaries, where new ocean floor is created as the Earth’s tectonic plates spread apart. As the plates separate, molten rock rises to the seafloor, producing enormous volcanic eruptions of basalt. The speed of spreading affects the shape of a ridge slower spreading rates result in steep, irregular topography while faster spreading rates produce much wider profiles and more gentle slopes.