The isostasy of a mountain will make it ultimately be eroded to near sea level. This is considered science earth.
isostasy
Common isostasy problems in geology include crustal rebound, subsidence, and isostatic adjustment. These issues can impact the Earth's crust by causing changes in elevation, leading to geological hazards such as earthquakes, volcanic activity, and landslides. Isostasy problems can also affect the stability of the Earth's surface and contribute to the formation of mountain ranges and ocean basins.
Three principal models of isostasy are:The Airy-HeiskanenModel- where different topographic heights are accommodated by changes in crustal thickness, in which the crust has a constant density The Pratt-HayfordModel- where different topographic heights are accommodated by lateral changes in rock density. The Vening Meinesz, or Flexural Model- where the lithosphere acts as an elastic plate and its inherent rigidity distributes local topographic loads over a broad region by bending.
Isostasy theory was developed by the American geologist Clarence Edward Dutton in the late 19th century. He proposed that the Earth's crust is in equilibrium, with less dense crust floating on top of the denser mantle.
The concept you are referring to is called isostasy. Isostasy explains how the Earth's lithosphere (crust and upper mantle) floats on the denser underlying asthenosphere in gravitational equilibrium, with thicker crust floating higher and thinner crust floating lower to maintain balance. This concept helps explain variations in topography and subsurface structure of the Earth's surface.
because isostasy, defored and thickened crust will undergo regional uplift both during mountain building for a long period afterward
the root to decrease in size
The root to decrease in size
strength and weaknesses of isostasy
Isostasy can cause continental uplift or subsidence depending on changes in crustal thickness and density. When weight is added to the crust, such as by mountain building or erosion, the crust can adjust by uplifting or sinking to maintain gravitational equilibrium. This vertical movement of the crust due to isostasy is known as isostatic rebound or isostatic subsidence.
isostasy
An isostatic is something that pertains to or is characterized by isostasy. Isostasy is the equilibrium of the Earths crust.
Common isostasy problems in geology include crustal rebound, subsidence, and isostatic adjustment. These issues can impact the Earth's crust by causing changes in elevation, leading to geological hazards such as earthquakes, volcanic activity, and landslides. Isostasy problems can also affect the stability of the Earth's surface and contribute to the formation of mountain ranges and ocean basins.
Three principal models of isostasy are:The Airy-HeiskanenModel- where different topographic heights are accommodated by changes in crustal thickness, in which the crust has a constant density The Pratt-HayfordModel- where different topographic heights are accommodated by lateral changes in rock density. The Vening Meinesz, or Flexural Model- where the lithosphere acts as an elastic plate and its inherent rigidity distributes local topographic loads over a broad region by bending.
Isostasy is most likely found in regions where the Earth's lithosphere is in gravitational equilibrium with the underlying asthenosphere. This phenomenon occurs when there are variations in crustal thickness or density, such as in mountain ranges or oceanic trenches. Isostatic adjustments occur as the crust responds to changes in load, such as erosion, sediment deposition, or glacial melting. Thus, isostasy is prevalent in tectonically active areas and regions experiencing significant geological changes.
The balance between gravity and buoyancy is called equilibrium.
Monkey