Mountain Range Fractals
by Owen Borville
September 22, 2021
Science, Mathematics
Mountain ranges features multiple peaks and jagged edges that result from the uplift of the Earth's crust from forces underneath the surface.
These peaks and jagged edges can be magnified large and small toward infinity, therefore mountain range patterns can classify as fractals as they feature repeating patterns at multiple scales toward infinity.
Thermal forces created by intense heat and pressure cause the overlying layers of the Earth's crust to be pushed upward, causing uplift of the land surface and the formation of mountains.
Erosion from water, ice, and wind causes these elevated crustal outer layers to modify their shape as the rounded shape is eroded away and sharp peaks and jagged edges are carved by erosional processes.
by Owen Borville
September 22, 2021
Science, Mathematics
Mountain ranges features multiple peaks and jagged edges that result from the uplift of the Earth's crust from forces underneath the surface.
These peaks and jagged edges can be magnified large and small toward infinity, therefore mountain range patterns can classify as fractals as they feature repeating patterns at multiple scales toward infinity.
Thermal forces created by intense heat and pressure cause the overlying layers of the Earth's crust to be pushed upward, causing uplift of the land surface and the formation of mountains.
Erosion from water, ice, and wind causes these elevated crustal outer layers to modify their shape as the rounded shape is eroded away and sharp peaks and jagged edges are carved by erosional processes.
Mount Everest
