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Lone Rock Point Lone Rock Point is a promontory north of Burlington, Vermont and on the eastern shore of Lake Champlain.[1] It is publicly accessible via a trail network and sits on land owned by the Episcopal Diocese of Vermont.[2] The site is of geologic significance for its spectacular exposure of a thrust contact between the Cambrian-aged Dunham Dolomite and the Middle-Ordovician Iberville Shale. The thrust fault exposed at this location is regionally called the Champlain Thrust which formed during the Taconic Orogeny.[3] At this site, the stratigraphic throw of the Champlain Thrust measures about 8,850 feet.[4] The site is arguably the most visited structural geology feature in all of New England[5] and is featured in many structural geology text books as a classic example of a thrust fault.[6][7] Dunham DolomiteThe Dunham Dolomite is a Cambrian dolomite that is exposed in the hanging wall of the Champlain Thrust Fault at Lone Rock Point. This unit was initially deposited in a warm, shallow sea environment as a platform carbonate. Well-exposed mullions at the base of the dolomite plunge about 15 degrees southeast, indicating transport direction (headed toward the modern lake).[4] The light colored rocks along the shoreline are blocks of dolomite that have fallen after the shale eroded away.[8] Iberville ShaleThe Ordovician Iberville Shale was likely deposited in a deeper marine environment and consists of fine-grained clastic materials.[1] Slip surfaces within the Iberville Shale seen at Lone Rock Point often contains calcite slickenlines along the planar thrust surface.[4] Overlying pressure has led to a high degree of vertical faulting and calcite dissolution (white banding) throughout the unit.[4] The top-most layer of the shale has been eroded away.[8] References
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