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Adirondack Geology: A close look at the High Peak Region
[object Object],[object Object],[object Object],[object Object],Hannah and Aaron explore exposed anorthosite on Baker Mountain in Saranac Lake.
[object Object],[object Object]
Landscapes change over time. The Adirondack Mountains formed from a  combination of uplift  (caused by plates converging) and  erosion  (Jaffe, 5). This picture shows some of the High Peaks, it was taken from the top of Baker Mountain in Saranac Lake. Photo by Jaime Armstrong.
Landscapes change over time. Water is a major force in changing the landscape over time. Hurricane Irene caused the landscape to change dramatically in  the Adirondacks. The picture below shows the washed-out road in Keene. The Ausable River rerouted itself, causing havoc, as a result of the hurricane. Photo by Phil Brown, used with permission.
Landscapes change over time. Duck Hole  was a favorite spot for many Adirondack campers. Flood waters from Hurricane Irene caused a breach in the Duck Hole Dam. What was once “one of the most scenic water bodies  in the High Peaks Wilderness”, according to the Adirondack Mountain Club, is now a mudflat. Hundreds of years from now, geologists will be able to tell that this area was once covered in water due to the fossils left behind. Photos used with permission, by Phil Brown. (DEC won’t rebuild Duckhole Dam)
Angular Unconformity. ,[object Object]
Intrusion ,[object Object],[object Object],[object Object]
Pitchoff Mountain Trail The view from “Balance Rock” on Pitchoff Mountain. Photo by Jaime Armstrong.
Pitchoff Trail: Van Hoevenberg Gneiss ,[object Object],Photo taken on the trail to balance rocks.
Pitchoff Trail: Van Hoevenberg Gneiss ,[object Object],[object Object],This picture was taken where the guidebook described Van Hoevenberg gneiss would be. However, from the description I think that the photo on the previous slide (found further up the trail) is correct.
Pitchoff Mountain ,[object Object],[object Object]
[object Object]

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Final geology lab project part 1

  • 1. Adirondack Geology: A close look at the High Peak Region
  • 2.
  • 3.
  • 4. Landscapes change over time. The Adirondack Mountains formed from a combination of uplift (caused by plates converging) and erosion (Jaffe, 5). This picture shows some of the High Peaks, it was taken from the top of Baker Mountain in Saranac Lake. Photo by Jaime Armstrong.
  • 5. Landscapes change over time. Water is a major force in changing the landscape over time. Hurricane Irene caused the landscape to change dramatically in the Adirondacks. The picture below shows the washed-out road in Keene. The Ausable River rerouted itself, causing havoc, as a result of the hurricane. Photo by Phil Brown, used with permission.
  • 6. Landscapes change over time. Duck Hole was a favorite spot for many Adirondack campers. Flood waters from Hurricane Irene caused a breach in the Duck Hole Dam. What was once “one of the most scenic water bodies in the High Peaks Wilderness”, according to the Adirondack Mountain Club, is now a mudflat. Hundreds of years from now, geologists will be able to tell that this area was once covered in water due to the fossils left behind. Photos used with permission, by Phil Brown. (DEC won’t rebuild Duckhole Dam)
  • 7.
  • 8.
  • 9. Pitchoff Mountain Trail The view from “Balance Rock” on Pitchoff Mountain. Photo by Jaime Armstrong.
  • 10.
  • 11.
  • 12.
  • 13.