Rock List
Site 14: Marble

Age: Neoproterozoic (~600 Ma)
Geological Unit(s): Chrisholm Brook Formation
Description: This rock is the result of metamorphism of a limestone protolith/parent rock. Like a limestone, this rock is rich in carbonate minerals (mainly calcite) and will fizz in acid. Whereas in the sedimentary protolith sediment grains are held together with cement like bricks and mortar, during metamorphism carbonate clasts (allochems) recrystallize and lock together much like jig-saw pieces in a puzzle. This results in a harder rock with no cementation agent around individual grains. This particular marble is contaminated by muds (silicate minerals) evidenced by the brownish layers within the rock. Marble makes an excellent building and sculpting stone, especially when pure and white. For instance, Michelangelo’s ‘David’.
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Department of Geology
902-496-8268
Mailing address:
Saint Mary's University
923 Robie Street
Halifax, Nova Scotia
B3H 3C3