As the glacier advanced, it froze around grains of sand, pebbles, rocks, and even large boulders and carried them along. Both drumlins and eskers are composed of this debris.
A drumlin is an elongated, whale shaped hill that forms at the bed of a glacier. They form when there are numerous hard and soft spots on the glacier bed. The ice deposited material around a small obstacle on the ground. Individual surges of the glacier added more material creating layers and then reshaped the deposits by further ice movements. Drumlins generally occur in groups called swarms. The steep end of a drumlin faces into the ice flow, while the back of the slope became lower as the ice passed.
An esker is formed in warm glaciers where flowing water melts upward into the ice instead of downward into the bed. The flowing stream fills the tunnel with sand and gravel. Most eskers generally parallel the direction of the ice flow. They form near the edge of glaciers where the ice is relatively thin and is not moving fast. When the surrounding ice melts away, it leaves a ridge. Melt water was confined by surrounding ice which caused the deposits of sediment to be left above the surrounding terrain.
Subglacial tunnel filling with sand and gravel.
Modified from National Park Service; drafted by Mary Diman.
(© 2011 by the Regents of the University of Wisconsin System.
Reprinted by permission of The University of Wisconsin Press)
Eskers range from a few feet to over 150 feet high, from hundreds of feet to many miles long, and up to as much as a half mile wide with steep sides. The ridge crests of eskers are usually not level for very long; they are generally knobby. They are more abundant in areas where the glacier was slow moving or stagnant with a supply of debris at or near the glacier base. The slower the stream, the greater the chance for deposits. Many eskers are not continuous because sediment was deposited only in places where the meltwater slowed down
IATCC is the cache designation to highlight a series of EarthCaches along the Ice Age National Scenic Trail grouped into a special category called "ColdCache."
The Ice Age Trail is one of eleven National Scenic Trails designated by the National Park Service. This unique trail is entirely within the state of Wisconsin and follows along the terminal moraine of the most recent glacier which retreated about 10,000 years ago.
This project is supported by the Ice Age Trail Alliance (IATA). The goal is to bring more visitors to the trail and promote public awareness, appreciation, and understanding of Wisconsin’s glacial landscape. The IATA has created an awards program to encourage visits to the trail and ColdCache sites. This awards program is separate from, and in addition to, any other Geo- or EarthCache awards program.
A current list of approved ColdCache sites can be found on the “IATCC Bookmark List”
More information on the Ice Age Trail Atlas, the Companion Guide, the ColdCache Project and Awards Program can be found on the “ColdCache Webpage”
The Geocache Notification Form has been submitted to
GeoCache GC1X75Z – Eskers: Ancient Glacial Riverbeds
Geology of the Ice Age National Scenic Trail; by David M. Mickelson, Louis J. Maher Jr., and Susan L. Simpson Wikipedia
The Geocache Notification Form has been submitted to Adam Backus of Manitowoc County.
1. Estimate how high and wide the feature is at the highpoint.
Notice the relative width of the feature from the bench to the post at the south end.
Does it change much in width?
Based on this information; is the feature a drumlin or an esker?