Till plain

A till plain is an extensive flat plain of glacial till that forms when a sheet of ice becomes detached from the main body of a glacier and melts in place, depositing the sediments it carried. Ground moraines are formed when the till melts out of the glacier in irregular heaps, forming rolling hills.

Contents

• Glaciated till plains
• Till plains tour kickoff show loudhouse 7 23 2009
• References

Till plains created by the Wisconsin glaciation cover much of northern Ohio (see Glacial till plains (Ohio)).