Add to ORKGView of Kanokolus Bog along the western quadrangle edge. Wetlands are common in the Unity quadrangle – even in upland areas – mostly due to shallow depth to bedrock that results in poor drainage. Project Name: STATEMAP Unity Surficialhttps://digitalmaine.com/mgs_geologic_field_photos/20437/thumbnail.jp
A subtle break in slope (marked with red arrow) was likely created by late-glacial sea wave action. ...
The swale between fields (photo center) once served as a glacial meltwater path, but this feature wa...
Maine Geological Survey, Open-File Map 22-4.https://digitalmaine.com/mgs_maps/3149/thumbnail.jp
View of Kanokolus Bog along the western quadrangle edge. Wetlands are common in the Unity quadrangle...
Low relief, generally shallow depth to bedrock, and fine-grained Presumpscot Formation deposits resu...
In addition to the Kanokolus Esker, several smaller esker segments can be found in the eastern part ...
The Kanokolus Esker is a significant glacial landform and aggregate resource in the Unity Pond quadr...
Western view from the Hills to Sea Trail, which traverses southern portions of the quadrangle. This ...
An exposure of sandy and stony glacial till in the Carlton Pond Wildlife Management Area. Project Na...
Well-preserved glacial striations are rare in the Unity Pond quadrangle due to the fissile local met...
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...
Illustration of possible late-glacial sea extent in the Unity Pond quadrangle. The location of Beech...
Illustrations of possible proglacial lake and late-glacial sea extents in the Unity quadrangle as ic...
Gravel pit exposure of esker sand and gravel in the Halfmoon Stream Valley. Project Name: STATEMAP U...
A subtle break in slope (marked with red arrow) was likely created by late-glacial sea wave action. ...
The swale between fields (photo center) once served as a glacial meltwater path, but this feature wa...
Maine Geological Survey, Open-File Map 22-4.https://digitalmaine.com/mgs_maps/3149/thumbnail.jp
View of Kanokolus Bog along the western quadrangle edge. Wetlands are common in the Unity quadrangle...
Low relief, generally shallow depth to bedrock, and fine-grained Presumpscot Formation deposits resu...
In addition to the Kanokolus Esker, several smaller esker segments can be found in the eastern part ...
The Kanokolus Esker is a significant glacial landform and aggregate resource in the Unity Pond quadr...
Western view from the Hills to Sea Trail, which traverses southern portions of the quadrangle. This ...
An exposure of sandy and stony glacial till in the Carlton Pond Wildlife Management Area. Project Na...
Well-preserved glacial striations are rare in the Unity Pond quadrangle due to the fissile local met...
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...
Illustration of possible late-glacial sea extent in the Unity Pond quadrangle. The location of Beech...
Illustrations of possible proglacial lake and late-glacial sea extents in the Unity quadrangle as ic...
Gravel pit exposure of esker sand and gravel in the Halfmoon Stream Valley. Project Name: STATEMAP U...
A subtle break in slope (marked with red arrow) was likely created by late-glacial sea wave action. ...
The swale between fields (photo center) once served as a glacial meltwater path, but this feature wa...
Maine Geological Survey, Open-File Map 22-4.https://digitalmaine.com/mgs_maps/3149/thumbnail.jp