by sinking
When the weight of part of the Earth's crust changes, it can lead to isostatic adjustments. This means that the crust will slowly adjust by rising or sinking to reach a new equilibrium. These adjustments can affect local sea levels, cause earthquakes, or create volcanic activity due to changes in pressure and magma movement.
Aluminum is the most abundant metallic element on Earth. It makes up more than eight percent of the earth's crust. Though, it is never free in nature. It combines with oxygen, sand, iron and titanium, and its ores are mainly bauxites.
The moon's crust is thinner than Earth's crust. The Moon's crust is estimated to be around 25 to 40 kilometers thick, while Earth's crust varies between 5 to 70 kilometers thick.
Earth's crust is composed of multiple tectonic plates that float on the semi-fluid mantle below, while the moon's crust is one solid, unbroken layer, with no tectonic activity. Earth's crust is richer in elements like silicon and oxygen, while the moon's crust is mostly made up of different types of rock, such as basalt and anorthosite.
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 crust will respond by adjusting its position to accommodate the additional weight. This may cause the crust to sag or deform if the weight is significant. Over time, the crust may undergo internal deformation processes to regain equilibrium.
Because the Oceans spread their weight out evenly over the Earth, and the Crust is supported evenly from below by Earth's Mantle, the crust cannot "go" anywhere. True, it will compress somewhat from the weight of the oceans, but the oceans could be of any given depth (even a thousand miles) and the crust would do nothing but stay right where it is. Rock is heavier than water, so the continents outweigh the oceans by a considerable amount, even though they take up far less area. If the oceans were a couple of miles deeper, they would flood over the continents, but this would have little impact on their position.
New crust sometimes rides over existing crust, burying it, and sometimes it folds up, creating mountains.
earthquakes happen when these sections of earths crust move
No. The crust is rigid; it does not allow convection.
After the ice from the ice age melted, the weight of the ice was removed from the continental crust. This caused the crust to gradually rebound or rise up due to the release of the pressure, a process known as post-glacial rebound or isostatic rebound. This uplift can continue for thousands of years after the ice has melted.
When mass is added to Earth's crust, it causes the crust to subside and sink due to the increased weight. Conversely, when mass is removed from the crust, it can rebound and rise due to the decreased load. This process is known as isostatic adjustment and can result in changes in the Earth's topography.
When weight is removed from or added to the crust, the Earth's gravitational field adjusts to reach a new state of equilibrium. This process involves redistributing mass within the Earth to balance the gravitational forces. The adjustment may involve movement of material within the Earth's interior or changes in the shape of the Earth’s surface.
Oxygen comprises about 47% by weight of Earth's crust
They weld together into new continental crust.
A pie breather is a small weight (mine's a chicken! LOL) that u place in the middle of a raw pie crust when pre-cooking it. It keeps the pie crust from bubbling by releasing the air. (my chicken whistles - added bonus)
New crust is being added to the other edge of the boundary