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The contact is vertical, with granodiorite the dominant rock below a depth of about 100 feet.
It grades inwards over tens to hundreds of metres into a coarser-grained porphyritic granodiorite .
These stone balls are formed when the material - granodiorite , a metamorphic rock - melts in magma and is of different density than the surrounding fluid.
Granite and granodiorite are examples of silica-rich plutonic rocks.
They were composed of solid granodiorite ; a very hard igneous rock.
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