Add to ORKGWell-preserved glacial striations are rare in the Unity quadrangle due to the fissile local metasedimentary bedrock, but this nice set along Sandy Stream shows that ice flow was to the southeast (same orientation as marker, right to left in photo). Project Name: STATEMAP Unity Surficialhttps://digitalmaine.com/mgs_geologic_field_photos/20432/thumbnail.jp
A subtle break in slope (marked with red arrow) was likely created by late-glacial sea wave action. ...
Low relief, generally shallow depth to bedrock, and fine-grained Presumpscot Formation deposits resu...
View of Kanokolus Bog along the western quadrangle edge. Wetlands are common in the Unity quadrangle...
Well-preserved glacial striations are rare in the Unity quadrangle due to the fissile local metasedi...
Well-preserved glacial striations are rare in the Unity Pond quadrangle due to the fissile local met...
Western view from the Hills to Sea Trail, which traverses southern portions of the quadrangle. This ...
This granite boulder was rounded during transport in glacial ice and is an “erratic” because it diff...
This granite boulder was rounded during transport in glacial ice and is an “erratic” because it diff...
Miles and miles of rock walls in the Unity quadrangle, such as this remnant in the Sebasticook Land ...
Illustrations of possible proglacial lake and late-glacial sea extents in the Unity quadrangle as ic...
An exposure of sandy and stony glacial till in the Carlton Pond Wildlife Management Area. Project Na...
Glacial striations on Puzzle Mountain (compass for scale). Ice flow was in the same direction as the...
A sample of silty Presumpscot Formation and fossil shells (circled in red) that were deposited on th...
Glacial striations in a bedrock exposure on the Record Hill ridgeline. Former glacial ice flow was l...
The swale between fields (photo center) once served as a glacial meltwater path, but this feature wa...
A subtle break in slope (marked with red arrow) was likely created by late-glacial sea wave action. ...
Low relief, generally shallow depth to bedrock, and fine-grained Presumpscot Formation deposits resu...
View of Kanokolus Bog along the western quadrangle edge. Wetlands are common in the Unity quadrangle...
Well-preserved glacial striations are rare in the Unity quadrangle due to the fissile local metasedi...
Well-preserved glacial striations are rare in the Unity Pond quadrangle due to the fissile local met...
Western view from the Hills to Sea Trail, which traverses southern portions of the quadrangle. This ...
This granite boulder was rounded during transport in glacial ice and is an “erratic” because it diff...
This granite boulder was rounded during transport in glacial ice and is an “erratic” because it diff...
Miles and miles of rock walls in the Unity quadrangle, such as this remnant in the Sebasticook Land ...
Illustrations of possible proglacial lake and late-glacial sea extents in the Unity quadrangle as ic...
An exposure of sandy and stony glacial till in the Carlton Pond Wildlife Management Area. Project Na...
Glacial striations on Puzzle Mountain (compass for scale). Ice flow was in the same direction as the...
A sample of silty Presumpscot Formation and fossil shells (circled in red) that were deposited on th...
Glacial striations in a bedrock exposure on the Record Hill ridgeline. Former glacial ice flow was l...
The swale between fields (photo center) once served as a glacial meltwater path, but this feature wa...
A subtle break in slope (marked with red arrow) was likely created by late-glacial sea wave action. ...
Low relief, generally shallow depth to bedrock, and fine-grained Presumpscot Formation deposits resu...
View of Kanokolus Bog along the western quadrangle edge. Wetlands are common in the Unity quadrangle...