The pull of Earth's gravity during the moon's formation caused the crust on the far side of the moon to become thicker than the crust on the near side. On the near side, the lunar crust is about 60 km thick. On the far side, the lunar crust is up to 100 km thick.
The Moon's crust is thicker on the far side compared to the near side because of a phenomenon called tidal locking. This means the Moon rotates on its axis in the same amount of time it takes to orbit Earth, causing one side to always face us. The gravitational interactions with Earth's gravity have led to differences in the thickness of the crust between the two sides.
Right now scientists do not know why the Earth-facing side of the moon has thicker crust. One proposal is that Earth may have once had two moons that collided at relatively low speeds. The geologically different regions on the moon would then have originated from two separate moons.
The Moon's crust on the near side is thinner and smoother with large plains called maria, formed from ancient lava flows. The far side has a thicker crust with more craters and mountains, as it has been shielded from volcanic activity due to tidal locking.
Thicker. The side of the moon facing Earth has a thicker crust compared to the side facing away, known as the lunar farside. This difference is due to the asymmetry in the thickness of the Moon's crust caused by the cooling of the lunar magma ocean.
The Moon's near side has more Maria (dark, smooth plains) than the far side because the lunar crust is thinner on the near side, allowing for more volcanic activity in the past. This resulted in more volcanic eruptions and lava flows creating the Maria that we see today. The far side of the Moon has a thicker crust, which limited the amount of volcanic activity.
The crust of the Moon is thinner on the side facing the Earth because the Moon is tidally locked with the Earth. This means that the Moon rotates at exactly the same rate it revolves around the Earth, so only one side of the Moon ever faces the Earth. Since the gravity of Earth acts on the Moon, the crust has been pulled slightly towards Earth on the side of the Moon facing Earth. Because of this, the crust of the Moon is thinner on one side than the other.
The moon's crust averages between 31 and 37 miles in thickness. The crust on the far side is a bit thicker than the near side.
that the moon has a thinner crust on the side facing earth
The Moon's crust is thicker on the far side compared to the near side because of a phenomenon called tidal locking. This means the Moon rotates on its axis in the same amount of time it takes to orbit Earth, causing one side to always face us. The gravitational interactions with Earth's gravity have led to differences in the thickness of the crust between the two sides.
Right now scientists do not know why the Earth-facing side of the moon has thicker crust. One proposal is that Earth may have once had two moons that collided at relatively low speeds. The geologically different regions on the moon would then have originated from two separate moons.
The Moon's crust on the near side is thinner and smoother with large plains called maria, formed from ancient lava flows. The far side has a thicker crust with more craters and mountains, as it has been shielded from volcanic activity due to tidal locking.
because of its size and gravitational pull it gathers many moons over years and years of rotation.there is no telling what happens on the other side of the sun when we are on this side.
Thicker. The side of the moon facing Earth has a thicker crust compared to the side facing away, known as the lunar farside. This difference is due to the asymmetry in the thickness of the Moon's crust caused by the cooling of the lunar magma ocean.
The Moon's near side has more Maria (dark, smooth plains) than the far side because the lunar crust is thinner on the near side, allowing for more volcanic activity in the past. This resulted in more volcanic eruptions and lava flows creating the Maria that we see today. The far side of the Moon has a thicker crust, which limited the amount of volcanic activity.
Faults are made up of fractures in the earths crust. One side of the fault moves opposite of the other side.
I dont know go ask someone else
These uneven planchets are not very rare and have little or no added value.