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Sample GeoRef Record
Database
GeoRef
Title
The
relationship between glacial geologic processes
and peatland distribution in Indiana
Purdue
University, Department of Forestry and Natural Resources, West
Lafayette, IN, United States (USA)
Source
Proceedings of the Indiana Academy of Science, vol.111, no.1,
pp.21-31, 2002
ISSN
0073-6767
CODEN
PIACAP
Descriptors
bogs
Cenozoic
clastic
sediments
depositional
environment
drift
glacial
environment
Histosols
Holocene
Indiana
lacustrine
environment
Laurentide
ice sheet
mires
moraines
Noble
County Indiana
peat
Pleistocene
Quaternary
Saginaw
Lobe
sediments
soils
spatial
distribution
United
States
upper
Pleistocene
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Abstract
Peat-filled depressions are not randomly distributed in
Indiana. The higher frequency of kettles and peatlands
in northern Indiana is attributed to the dynamic
processes of glacial retreat rather than potential
influences of pre-glacial topography. Ninety
percent of Indiana's peatlands occur in the
northern moraine and lake region of the state. Within this
region, peatlands were significantly more frequent inside the
former boundaries of the Saginaw Lobe than peatlands occurring
outside of this area. An analysis of peatland distribution and
specific glacial drift types in Noble County
showed that peatlands were significantly more frequent in mixed
till and stratified drift in lineated form associated with
collapse of sub-ice tunnels and open ice-walled channels. Four
other drift types contained significantly fewer peatlands than
expected.
GeoRef,
Copyright 2004, American Geological Institute.
Update
200306
Accession Number
2003-018102
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