Add to ORKGIllustrations of possible proglacial lake and late-glacial sea extents in the Unity quadrangle as ice retreated to the northwest. Meltwater paths/spillways marked with blue arrows. Unity and Freedom village locations marked with U and F for reference. A: Extents of Glacial Lake Freedom and Glacial Lake Halfmoon (highest stage). B: Extent of Glacial Lake Halfmoon (lowest stage). C: Extent of late-glacial sea, which entered from low area in northwest portion of the quadrangle. Project Name: STATEMAP Unity Surficialhttps://digitalmaine.com/mgs_geologic_field_photos/20438/thumbnail.jp
Glacial geologic history in the area of the Greenwood Lake, Isabella and Cramer quadrangles. Text an...
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...
Western view from the Hills to Sea Trail, which traverses southern portions of the quadrangle. This ...
Illustration of possible late-glacial sea extent in the Unity Pond quadrangle. The location of Beech...
A subtle break in slope (marked with red arrow) was likely created by late-glacial sea wave action. ...
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...
The swale between fields (photo center) once served as a glacial meltwater path, but this feature wa...
A sample of silty Presumpscot Formation and fossil shells (circled in red) that were deposited on th...
Low relief, generally shallow depth to bedrock, and fine-grained Presumpscot Formation deposits resu...
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...
View of Kanokolus Bog along the western quadrangle edge. Wetlands are common in the Unity quadrangle...
Glacial geologic history in the area of the Greenwood Lake, Isabella and Cramer quadrangles. Text an...
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...
Western view from the Hills to Sea Trail, which traverses southern portions of the quadrangle. This ...
Illustration of possible late-glacial sea extent in the Unity Pond quadrangle. The location of Beech...
A subtle break in slope (marked with red arrow) was likely created by late-glacial sea wave action. ...
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...
The swale between fields (photo center) once served as a glacial meltwater path, but this feature wa...
A sample of silty Presumpscot Formation and fossil shells (circled in red) that were deposited on th...
Low relief, generally shallow depth to bedrock, and fine-grained Presumpscot Formation deposits resu...
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...
View of Kanokolus Bog along the western quadrangle edge. Wetlands are common in the Unity quadrangle...
Glacial geologic history in the area of the Greenwood Lake, Isabella and Cramer quadrangles. Text an...
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 ...
