Add to ORKGGlacial striations on Puzzle Mountain (compass for scale). Ice flow was in the same direction as the compass pointer (bottom to top of photo). Project Name: STATEMAP Puzzle Mountain Surficialhttps://digitalmaine.com/mgs_geologic_field_photos/17866/thumbnail.jp
This boulder was moved a short distance to its current location by logging road construction, but it...
View toward the east of glacially scuplted bedrock. Ice flow was from left to right (toward the sout...
Glacial striations along the ski trail to Hedgehog Hill at Mount Blue State Park. Project Name: STAT...
Glacial striations on Puzzle Mountain (compass for scale). Ice flow was in the same direction as the...
Glacial striations in a bedrock exposure on the Record Hill ridgeline. Former glacial ice flow was l...
Glacially sculpted ledge area at end of Mount Blue State Park snowshoe trail; ice flow was roughly r...
Well-preserved glacial striations are rare in the Unity quadrangle due to the fissile local metasedi...
An exposure of platy lodgement till (also known as “hardpan”) along a logging road. Glacial ice plas...
Ledges at Center Hill, glacially sculpted and striated; ice flow was roughly right to left. Project ...
Northwestern view of the Bear River Valley from Puzzle Mountain. These hills and valleys were shaped...
Moss-covered cobbles and boulders mark a dry channel that was once the path of a glacial meltwater s...
Well-preserved glacial striations are rare in the Unity Pond quadrangle due to the fissile local met...
An example of moderately washed and sorted ice-contact sediments in an unnamed stream valley. Projec...
A large glacially transported boulder near Long Mountain. Project Name: STATEMAP Puzzle Mountain Sur...
This granite boulder was rounded during transport in glacial ice and is an “erratic” because it diff...
This boulder was moved a short distance to its current location by logging road construction, but it...
View toward the east of glacially scuplted bedrock. Ice flow was from left to right (toward the sout...
Glacial striations along the ski trail to Hedgehog Hill at Mount Blue State Park. Project Name: STAT...
Glacial striations on Puzzle Mountain (compass for scale). Ice flow was in the same direction as the...
Glacial striations in a bedrock exposure on the Record Hill ridgeline. Former glacial ice flow was l...
Glacially sculpted ledge area at end of Mount Blue State Park snowshoe trail; ice flow was roughly r...
Well-preserved glacial striations are rare in the Unity quadrangle due to the fissile local metasedi...
An exposure of platy lodgement till (also known as “hardpan”) along a logging road. Glacial ice plas...
Ledges at Center Hill, glacially sculpted and striated; ice flow was roughly right to left. Project ...
Northwestern view of the Bear River Valley from Puzzle Mountain. These hills and valleys were shaped...
Moss-covered cobbles and boulders mark a dry channel that was once the path of a glacial meltwater s...
Well-preserved glacial striations are rare in the Unity Pond quadrangle due to the fissile local met...
An example of moderately washed and sorted ice-contact sediments in an unnamed stream valley. Projec...
A large glacially transported boulder near Long Mountain. Project Name: STATEMAP Puzzle Mountain Sur...
This granite boulder was rounded during transport in glacial ice and is an “erratic” because it diff...
This boulder was moved a short distance to its current location by logging road construction, but it...
View toward the east of glacially scuplted bedrock. Ice flow was from left to right (toward the sout...
Glacial striations along the ski trail to Hedgehog Hill at Mount Blue State Park. Project Name: STAT...