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The low relief and gentle slopes of the region also make it unlikely that the erratic boulders have rolled over, except at the time of initial emplacement as ice melted beneath them.
The quartzite that composes the erratics is extremely tough and resistant with little evidence of spalling along bedding planes.
The latter is considered to be minor—measured in hundreds of years.
Note: Further down I show an easy way to measure the strength of your bleach/liquid chlorine.The rate of chlorine-36 production by cosmic rays (thermal and fast neutrons) depends on the concentrations of potassium (K), Calcium (Ca) and chlorine (Cl), the elevation of the rock, surface orientation, and geomagnetic latitude.The rate of accumulation of chlorine-36 depends on the balance between the production rate of chlorine-36 and on the rate of erosion of the rock surface.Six of the ages clearly fall within the age range of the Late Wisconsinan Glaciation (ca. The range in ages likely reflect events during the history of each rock that could affect its exposure to cosmic radiation such as rotation of the rock due to settlement which could have changed its orientation with the sky.