Add to ORKGA subtle break in slope (marked with red arrow) was likely created by late-glacial sea wave action. Similar features are present elsewhere in the quadrangle, all at about 340 ft (103.6 m), and may represent the local elevation limit of late-glacial marine inundation or a pause during ocean regression. Project Name: STATEMAP Unity Pond Surficialhttps://digitalmaine.com/mgs_geologic_field_photos/20424/thumbnail.jp
Miles and miles of rock walls in the Unity quadrangle, such as this remnant in the Sebasticook Land ...
View of Kanokolus Bog along the western quadrangle edge. Wetlands are common in the Unity quadrangle...
This granite boulder was rounded during transport in glacial ice and is an “erratic” because it diff...
A subtle break in slope (marked with red arrow) was likely created by late-glacial sea wave action. ...
Illustration of possible late-glacial sea extent in the Unity Pond quadrangle. The location of Beech...
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 ...
Illustrations of possible proglacial lake and late-glacial sea extents in the Unity quadrangle as ic...
Low relief, generally shallow depth to bedrock, and fine-grained Presumpscot Formation deposits resu...
A sample of silty Presumpscot Formation and fossil shells (circled in red) that were deposited on th...
The swale between fields (photo center) once served as a glacial meltwater path, but this feature wa...
An exposure of sandy and stony glacial till in the Carlton Pond Wildlife Management Area. Project Na...
This granite boulder was rounded during transport in glacial ice and is an “erratic” because it diff...
Maine Geological Survey, Open-File Map 22-4.https://digitalmaine.com/mgs_maps/3149/thumbnail.jp
Well-preserved glacial striations are rare in the Unity quadrangle due to the fissile local metasedi...
Miles and miles of rock walls in the Unity quadrangle, such as this remnant in the Sebasticook Land ...
View of Kanokolus Bog along the western quadrangle edge. Wetlands are common in the Unity quadrangle...
This granite boulder was rounded during transport in glacial ice and is an “erratic” because it diff...
A subtle break in slope (marked with red arrow) was likely created by late-glacial sea wave action. ...
Illustration of possible late-glacial sea extent in the Unity Pond quadrangle. The location of Beech...
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 ...
Illustrations of possible proglacial lake and late-glacial sea extents in the Unity quadrangle as ic...
Low relief, generally shallow depth to bedrock, and fine-grained Presumpscot Formation deposits resu...
A sample of silty Presumpscot Formation and fossil shells (circled in red) that were deposited on th...
The swale between fields (photo center) once served as a glacial meltwater path, but this feature wa...
An exposure of sandy and stony glacial till in the Carlton Pond Wildlife Management Area. Project Na...
This granite boulder was rounded during transport in glacial ice and is an “erratic” because it diff...
Maine Geological Survey, Open-File Map 22-4.https://digitalmaine.com/mgs_maps/3149/thumbnail.jp
Well-preserved glacial striations are rare in the Unity quadrangle due to the fissile local metasedi...
Miles and miles of rock walls in the Unity quadrangle, such as this remnant in the Sebasticook Land ...
View of Kanokolus Bog along the western quadrangle edge. Wetlands are common in the Unity quadrangle...
This granite boulder was rounded during transport in glacial ice and is an “erratic” because it diff...