The buckboard is stopped on the road between Southwest Harbor and Somesville, now Route 102. The view is looking west across Echo Lake to Beach Cliffs.
Description: The buckboard is stopped on the road between Southwest Harbor and Somesville, now Route 102. The view is looking west across Echo Lake to Beach Cliffs.
Notice the elaborate hat worn by the lady in the front seat! The buckboard is stopped on the road between Southwest Harbor and Somesville, now Route 102. The view is looking west across Echo Lake to Beach Cliffs.
Description: Notice the elaborate hat worn by the lady in the front seat! The buckboard is stopped on the road between Southwest Harbor and Somesville, now Route 102. The view is looking west across Echo Lake to Beach Cliffs.
Description: An illustration of Rusticators on the top of Newport Mountain, later known as Champlain Mountain. From Harper's Weekly, Volume 22, No. 1654
This magic lantern slide, “Maine Coast at Bar Harbor,” is an example of slides used as education tools by universities, The University of the State of New York in this case. Photograph was taken from the top of Cadillac Mountain.
Description: This magic lantern slide, “Maine Coast at Bar Harbor,” is an example of slides used as education tools by universities, The University of the State of New York in this case. Photograph was taken from the top of Cadillac Mountain.
"Mount Desert Island was host to the Laurentide Ice Sheet as it extended and receded during the Pleistocene epoch. The glacier left a number of visible marks upon the landscape, such as Bubble Rock, a glacial erratic carried 19 miles by the ice sheet from a Lucerne granite outcrop and deposited precariously on the side of South Bubble Mountain in Acadia National Park. Other such examples are the moraines deposited at the southern ends of many of the glacier-carved valleys on the Island such as the Jordan Pond valley, indicating the extent of the glacier; and the beach sediments located in a regressional sequence beneath and around Jordan Pond, indicating the rebound of the continent after the glacier's recession approximately 25,000 years ago." - Gilman, R.A., Chapman, C.A., Lowell, T.V., and Borns, H.W., 1988, "Shaping of the Landscape by Glacial Erosion, in The geology of Mount Desert Island: Augusta, Maine Geological Survey Bulletin 38."
Description: "Mount Desert Island was host to the Laurentide Ice Sheet as it extended and receded during the Pleistocene epoch. The glacier left a number of visible marks upon the landscape, such as Bubble Rock, a glacial erratic carried 19 miles by the ice sheet from a Lucerne granite outcrop and deposited precariously on the side of South Bubble Mountain in Acadia National Park. Other such examples are the moraines deposited at the southern ends of many of the glacier-carved valleys on the Island such as the Jordan Pond valley, indicating the extent of the glacier; and the beach sediments located in a regressional sequence beneath and around Jordan Pond, indicating the rebound of the continent after the glacier's recession approximately 25,000 years ago." - Gilman, R.A., Chapman, C.A., Lowell, T.V., and Borns, H.W., 1988, "Shaping of the Landscape by Glacial Erosion, in The geology of Mount Desert Island: Augusta, Maine Geological Survey Bulletin 38." [show more]