The 'Sierra Nevada Batholith' is a large
batholith in the
Sierra Nevada mountain range,
USA, and is a continuous
granitic formation that forms much of the
Sierra Nevada mountain range of
California.
The batholith is composed of many individual masses of rock called ''
plutons'', which formed deep underground during separate episodes of
magma intrusion. The extremely hot, more
buoyant plutons, also called ''plutonic
diapirs'', intruded through denser, native
country rock, ultimately to make landforms such as
Yosemite National Park.
External links
★
US National Park site
★
Yosemite site