Add to ORKGAn exposure of sandy and stony glacial till in the Carlton Pond Wildlife Management Area. Project Name: STATEMAP Unity Pond Surficialhttps://digitalmaine.com/mgs_geologic_field_photos/20426/thumbnail.jp
Gravel pit exposure of esker sand and gravel in the Halfmoon Stream Valley. Project Name: STATEMAP U...
In addition to the Kanokolus Esker, several smaller esker segments can be found in the eastern part ...
This granite boulder was rounded during transport in glacial ice and is an “erratic” because it diff...
An exposure of sandy and stony glacial till in the Carlton Pond Wildlife Management Area. Project Na...
Low relief, generally shallow depth to bedrock, and fine-grained Presumpscot Formation deposits resu...
Well-preserved glacial striations are rare in the Unity Pond quadrangle due to the fissile local met...
Illustration of possible late-glacial sea extent in the Unity Pond quadrangle. The location of Beech...
This granite boulder was rounded during transport in glacial ice and is an “erratic” because it diff...
The swale between fields (photo center) once served as a glacial meltwater path, but this feature wa...
Western view from the Hills to Sea Trail, which traverses southern portions of the quadrangle. This ...
Miles and miles of rock walls in the Unity quadrangle, such as this remnant in the Sebasticook Land ...
Well-preserved glacial striations are rare in the Unity quadrangle due to the fissile local metasedi...
A sample of silty Presumpscot Formation and fossil shells (circled in red) that were deposited on th...
A subtle break in slope (marked with red arrow) was likely created by late-glacial sea wave action. ...
View of Kanokolus Bog along the western quadrangle edge. Wetlands are common in the Unity quadrangle...
Gravel pit exposure of esker sand and gravel in the Halfmoon Stream Valley. Project Name: STATEMAP U...
In addition to the Kanokolus Esker, several smaller esker segments can be found in the eastern part ...
This granite boulder was rounded during transport in glacial ice and is an “erratic” because it diff...
An exposure of sandy and stony glacial till in the Carlton Pond Wildlife Management Area. Project Na...
Low relief, generally shallow depth to bedrock, and fine-grained Presumpscot Formation deposits resu...
Well-preserved glacial striations are rare in the Unity Pond quadrangle due to the fissile local met...
Illustration of possible late-glacial sea extent in the Unity Pond quadrangle. The location of Beech...
This granite boulder was rounded during transport in glacial ice and is an “erratic” because it diff...
The swale between fields (photo center) once served as a glacial meltwater path, but this feature wa...
Western view from the Hills to Sea Trail, which traverses southern portions of the quadrangle. This ...
Miles and miles of rock walls in the Unity quadrangle, such as this remnant in the Sebasticook Land ...
Well-preserved glacial striations are rare in the Unity quadrangle due to the fissile local metasedi...
A sample of silty Presumpscot Formation and fossil shells (circled in red) that were deposited on th...
A subtle break in slope (marked with red arrow) was likely created by late-glacial sea wave action. ...
View of Kanokolus Bog along the western quadrangle edge. Wetlands are common in the Unity quadrangle...
Gravel pit exposure of esker sand and gravel in the Halfmoon Stream Valley. Project Name: STATEMAP U...
In addition to the Kanokolus Esker, several smaller esker segments can be found in the eastern part ...
This granite boulder was rounded during transport in glacial ice and is an “erratic” because it diff...