Add to ORKGMoss-covered cobbles and boulders mark a dry channel that was once the path of a glacial meltwater stream. Evidence of former glacial meltwater channels is plentiful in the Puzzle Mountain quadrangle, with many paths revealed by lidar topographic data. Project Name: STATEMAP Puzzle Mountain Surficialhttps://digitalmaine.com/mgs_geologic_field_photos/17870/thumbnail.jp
An exposure of glacial outwash in the Bear River Valley shows sand with cobbles and small boulders t...
6-D-18. Meltwater channel eroded in till on W side of Red Hill, Rumford. East Andover-EC-89-15, Pr...
A large glacially transported boulder near Long Mountain. Project Name: STATEMAP Puzzle Mountain Sur...
Moss-covered cobbles and boulders mark a dry channel that was once the path of a glacial meltwater s...
The swale between fields (photo center) once served as a glacial meltwater path, but this feature wa...
Glacial striations on Puzzle Mountain (compass for scale). Ice flow was in the same direction as the...
Northwestern view of the Bear River Valley from Puzzle Mountain. These hills and valleys were shaped...
Fluvial processes dominate the modern Puzzle Mountain quadrangle landscape. Waterfalls in the quadra...
An exposure of platy lodgement till (also known as “hardpan”) along a logging road. Glacial ice plas...
The increased availability and reliability of meter and sub-meter resolution LiDAR has provided unpr...
Area where Connector Trail descends into a former glacial meltwater channel. Project Name: STATEMAP ...
Meltwater Channel NNE of Readfield Villagehttps://digitalmaine.com/mgs_geologic_field_photos/1277/th...
This study evaluated and classified landscape geomorphology through the remote analysis of 2014, 1-m...
Glacially sculpted ledge area at end of Mount Blue State Park snowshoe trail; ice flow was roughly r...
An exposure of glacial outwash in the Bear River Valley shows sand with cobbles and small boulders t...
6-D-18. Meltwater channel eroded in till on W side of Red Hill, Rumford. East Andover-EC-89-15, Pr...
A large glacially transported boulder near Long Mountain. Project Name: STATEMAP Puzzle Mountain Sur...
Moss-covered cobbles and boulders mark a dry channel that was once the path of a glacial meltwater s...
The swale between fields (photo center) once served as a glacial meltwater path, but this feature wa...
Glacial striations on Puzzle Mountain (compass for scale). Ice flow was in the same direction as the...
Northwestern view of the Bear River Valley from Puzzle Mountain. These hills and valleys were shaped...
Fluvial processes dominate the modern Puzzle Mountain quadrangle landscape. Waterfalls in the quadra...
An exposure of platy lodgement till (also known as “hardpan”) along a logging road. Glacial ice plas...
The increased availability and reliability of meter and sub-meter resolution LiDAR has provided unpr...
Area where Connector Trail descends into a former glacial meltwater channel. Project Name: STATEMAP ...
Meltwater Channel NNE of Readfield Villagehttps://digitalmaine.com/mgs_geologic_field_photos/1277/th...
This study evaluated and classified landscape geomorphology through the remote analysis of 2014, 1-m...
Glacially sculpted ledge area at end of Mount Blue State Park snowshoe trail; ice flow was roughly r...
An exposure of glacial outwash in the Bear River Valley shows sand with cobbles and small boulders t...
6-D-18. Meltwater channel eroded in till on W side of Red Hill, Rumford. East Andover-EC-89-15, Pr...
A large glacially transported boulder near Long Mountain. Project Name: STATEMAP Puzzle Mountain Sur...