Distribution of surficial eolian and outwash sand deposits, Bureau County, Illinois

              R 7 E
R 8 E
R 9 E
R 9 E
R 10 E
R 11 E
T 16 N
R 6 E
T 17 N T 18 N
T 15 N T 16 N T 17 N T 18 N
R 6 E R 7 E R 8 E R 9 E R 10 E R 11 E
T 14 N
88
88
92
92
92
89
29
26
26
6
34 6
34
34
6
34
80
180
'
'
'
'
'
'
'
'
' ' '
'
'
'
' '
'
'
'
'
'
' '
New Bedford
Walnut
Manlius
Ohio
Dover
Malden
Hollowayville Seatonville
La Moille
Arlington
Cherry
Ladd
Dalzell
Spring Valley
De Pue
Bureau
Junction
Tiskilwa
Buda
Neponset
Mineral
Sheffield
Wyanet
Princeton
V
V
V
V
V
V
V
V
V
V
V
V
Illinois County Geologic Map
ICGM Bureau County-SS
ICGM Bureau County-SS
Base map compiled by Illinois State Geological Survey from 1:100,000-scale Digital Line Graph
data provided by the United States Geological Survey. North American Datum of 1983 (NAD 83).
Lambert Conformal Conic Projection.
Geology based on field work and data compilation by Xiaodong Miao, 2007.
Digital cartography by Jane E.J. Domier and Steve M. Radil, Illinois State Geological Survey.
The Illinois State Geological Survey and the University of Illinois make no guarantee, expressed
or implied, regarding the correctness of the interpretations presented in this document and ac-cept
no liability for the consequences of decisions made by others on the basis of the information
presented here. The geologic interpretations are based on data that may vary with respect to
accuracy of geographic location, the type and quantity of data available at each location, and the
scientific and technical qualifications of the data sources. This map is not meant to be enlarged.
This map provides a general view of sand distribution. It does not replace the need for detailed
investigations of specific sites.
Recommended citation:
Miao, X., 2009, Distribution of Surfical Eolian and Outwash Sand Deposits, Bureau County, Illi-nois:
Illinois State Geological Survey, Illinois County Geologic Map, ICGM Bureau County-SS,
1:100,000.
DISTRUBUTION OF SURFICIAL EOLIAN AND
OUTWASH SAND DEPOSITS
BUREAU COUNTY, ILLINOIS
Xiaodong Miao
2009
1 / ° 1 2
APPROXIMATE MEAN
DECLINATION, 2009
MAGNETIC NORTH
TRUE NORTH
Interstate Route
U.S. Route
State Route
Other paved roads
Road Classification
ADJACENT
COUNTIES
1 Whiteside
2 Lee
3 Henry
4 La Salle
5 Stark
6 Putnam
7 Marshall
2
3
1
4
5
6
7
For more information contact:
Institute of Natural Resource Sustainability
Illinois State Geological Survey
615 East Peabody Drive
Champaign, Illinois 61820-6964
(217) 244-2414
http://www.isgs.illinois.edu
Institute of Natural Resource Sustainability
William W. Shilts, Executive Director
ILLINOIS STATE GEOLOGICAL SURVEY
E. Donald McKay III, Interim Director
© 2009 University of Illinois Board of Trustees. All rights reserved.
For permission information, contact the Illinois State Geological Survey.
1 0 1 2 3 4 5 6 7 8 9 10 KILOMETERS
SCALE 1:100,000
1 0 1 2 3 4 5 6 7 8 MILES
Sand and gravel deposits are widespread in northwestern Bureau
County along the southern edge of the Green River Lowland and
scattered throughout the rest of the county. These deposits are largely
the direct or indirect result of glacial processes. There are two basic
types of sand and gravel deposits: outwash, which is composed of
poorly sorted sand and gravel from 10 to 50 feet thick and up to 200
feet in some locations, and sand dunes formed by the wind. The dune
deposits range in thickness from 20 to 60 feet and constitute a smaller
aggregate resource than the outwash deposits. Sand dunes are promi-nent
landforms in this county. They were deposited on outwash plains,
moraines, and stream terraces.
Surficial eolian sand, previously classified as the Parkland Sand (Wil-liam
and Frye 1970, Lineback 1979), consists of geomorphologically
distinct dune sand and relatively flat-lying sand sheets in inter-dune
areas. Eolian sand is very well sorted, medium to fine grained, and con-tains
no gravel. Most dunes have parabolic, compound parabolic, trans-verse,
or dome forms and are stabilized by vegetation cover under the
current climate regime (Miao et al. 2009). Trees and grass live mostly
on the uplands. The most distinct parabolic dune, with a height of 50
feet and a length of over one-half mile, is located 3 miles west of New
Bedford, in the northwestern part of Bureau County. Dune orientation
and internal cross-bedding structure consistently indicate that winds
from the northwest and west were responsible for dune construction,
similar to the current prevailing wind direction in this region. Some
dunes preserve one or two buried soils, indicating long-term landscape
stability. Seven optically stimulated luminescence ages (OSL or optical
ages) indicate that major dune construction in the Green River Low-land
occurred around 17,000 to 18,000 years ago (Miao et al. 2009).
Eight optical and four radiocarbon ages indicate that the dunes were
reactivated episodically during the Holocene, implying a high poten-tial
for future sand activation, regardless of human-induced climate
changes and associated global warming (Miao et al. 2009).
Most of the outwash sand and gravel in Bureau County is of Wiscon-sinan
age. Sand and gravel of Illinoian age, and possibly older, crops
out along some of the deeper valleys but is overlain by thick overbur-den
under the uplands. The absolute age of the Wisconsinan outwash is
not clearly known, and application of OSL on the outwash is important
for future mapping and research. Thick Wisconsinan glaciofluvial out-wash
(sand and gravel), classified as the Batavia Member of the Henry
Formation (Willman and Frye 1970, Lineback 1979), was deposited
adjacent to the Bloomington Morainic System in Bureau County.
Therefore, outwash sand may not be well sorted and commonly coex-ists
with gravel. Outwash deposits provide an abundant source of sand
and gravel for the aggregate industry.
Eolian and outwash sands are not mutually exclusive because eolian
sand is deposited on glaciofluvial outwash in many places in the Green
River Lowland. Eolian and glaciofluvial sediments were differentiated
based on topography and parent materials interpreted from the Bureau
County Soil Survey (United States Department of Agriculture 1992),
water and related well records, and grain size data. For example,
lobe-like sand deposited on the Bloomington Morainic System is also
classified as eolian, because only wind can blow the sand uphill onto
the topographically high moraine.
Although outwash sand is an important aggregate resource in Bureau
County, dune sand also is highly valued by industry, mostly for use in
foundries for making high-quality metal castings. The modal particle
size of the dune sand of the Green River Lowland is around 250 μm
(sieve 60), which is the perfect size for application as foundry sand.
In addition, dune sand is also very well sorted, making it ideal for ap-plication
in the foundry industry.
Acknowledgments
This work is based on an ongoing project on sand and gravel research
in the Green River Lowland. The research on the Bureau County sand
deposit has benefited from helpful discussions with colleagues Leon
Follmer, Zakaria Lasemi, and Hong Wang.
References
Lineback, J.A., 1979, Quaternary deposits of Illinois: Illinois State
Geological Survey, 1:500,000.
Miao, X.D., P.R. Hanson, H. Wang, and A.R. Young, 2009, Timing
and implications for sand dune development in the Green River
Lowland of Illinois, upper Midwestern United States: Geological
Society of America Abstracts with Programs, North-Central Sec-tion,
v. 41, no. 4, p. 64.
United States Department of Agriculture, Soil Conservation Service,
1992, Soil Survey of Bureau County, Illinois.
Willman, H.B., and J.C.Frye, 1970, Pleistocene stratigraphy of Illinois:
Illinois State Geological Survey, Bulletin 94, 204 p.
Eolian sand on
outwash or moraine
Outwash deposits
Non-sand
V Active sand and gravel pit