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Geology, Ecology, andGeology, Ecology, and
Resources of IowaResources of Iowa
By Danielle JannuschBy Danielle Jannusch
Welcome to theWelcome to the
Hawkeye StateHawkeye State
• Iowa was a tremendous geologic and
ecologic history. This presentation will
discuss:
– Geologic Feature: Devonian Fossil Gorge
– Ecologic Feature: Iowa Prairie
– Renewable and nonrenewable resources of
Iowa
Iowa GeologyIowa Geology
http://www.igsb.uiowa.edu/browse/geoiowa/geoiowa.htm
http://www.igsb.uiowa.edu/service/geology.htm
Iowa Geologic historyIowa Geologic history
• The oldest rocks in Iowa are buried deep underground.
• Most of Iowa’s geologic history is written in sedimentary rocks, such as sandstone,
limestone, dolomite and shale, which are over 3,000 feet thick in places. (DNR, 2010)
• Iowa sedimentary rocks originated as layers of loose sediment accumulating in
shallow seas and along coastal and floodplain environments between 74 million years
ago (Cretaceous) and 530 million years ago (Cambrian).
• Over time, this sediment was lithified into rock containing fossil remains of past
animal and plant life.
• Fossiliferous sedimentary rocks are found among the abundant outcrops of
northeastern, eastern, and central Iowa
• Most sedimentary rock exposures in Iowa are found along river valleys, at roadcuts,
and in quarries.
• Since most of our geologic history is buried, most of our knowledge comes from rock
samples brought up to the land surface during the drilling of wells.
• The oldest known formation in Iowa the Otter Creek Mafic Complex (about 2.95 billion
years old), the youngest is the Wisconsinan glacial drift (about 10,000 years old).
(DNR, 2010)
• Additionally, river sediments that are still being deposited today.
Iowa StratigraphicIowa Stratigraphic
Column:Column:
This column shows allThis column shows all
the different rock typesthe different rock types
found on the surfacefound on the surface
and in the subsurfaceand in the subsurface
of Iowa terrain Column.of Iowa terrain Column.
This column has beenThis column has been
used to correlate Iowaused to correlate Iowa
rocks with sedimentaryrocks with sedimentary
strata throughout thestrata throughout the
Midwest and theMidwest and the
countrycountry
Source:
http://publicatio
ns.iowa.gov/48
62/1/EM-40.pdf
Geologic Feature:Geologic Feature:
Devonian FossilDevonian Fossil
GorgeGorge
• Discovered during the Flood of 1993
when floodwaters from Coralville Lake
came over the spillway eroded away
15 feet of glacial-age sediments to
expose 375-million-year old
fossiliferous bedrock.
• The rocks of the gorge: The
dominant rock type at Devonian fossils
gorge is fossiliferous limestone.
The limestone is rich in crinoids,
corals, stromatoporoids and several
species of brachiopod fossils.
• Limestone is comprised of calcite.
• History of the sediments: These
sediments were deposited during the
Devonian Period about 375 million
years ago, when eastern Iowa was
covered with a shallow sea. The
fossils suggest that this was a reefal
normal marine environment with a
moderate undercurrent (Prior, 1998)
A recreation
of the
Devonian of
Iowa
1993- The
fossil sea is
discovered
after the flood
of 1993
Newly designed
entrance to the
Gorge
http://www.igsb.uiowa.edu/browse/spillway/spillway.htm
How has plate tectonics affectedHow has plate tectonics affected
the Gorge?the Gorge?
• Current earthquake activity: Only 13
earthquakes with epicenters in Iowa are
known in historic times. The first known
occurrence was in 1867 near Sidney in
southwest Iowa; the most recent occurrence
was in 2004 near Shenandoah in SW Iowa.
The largest Iowa earthquake (Mercalli
magnitude VI) occurred near Davenport in
southeast Iowa in 1934. (DNR, 2010)
• Activity around the Gorge is rare, but some
of the strata are inclined.
• Looking north toward the Coralville Lake
Spillway some of the limestone strata are
inclined and domed. (DNR, 2010)
• It has been suggested that this inclination
may be the result of irregular settling of the
sedimentary layers when they were still soft,
or the result of much later, broad-scale
warping of rock units across the Midwest.
• Small geologic faults are also exposed here,
with vertically displaced strata and tiny
gouges along the rock faces indicating
movement in the geologic past (about 310
million years ago) (Prior, 1998)
•http://www.igsb.uiowa.edu/Browse/earthqua/iowa_quakes.htm
Glacial and Surficial Processes andGlacial and Surficial Processes and
their impact on Iowatheir impact on Iowa
• Glacial processes are responsible for
many of the geologic features
throughout the state.
• The “lake district” area of northern
Iowa is dominated by natural lakes
and bogs, among irregularly shaped
hills, and in the boulders- all evidence
of glacial activity (Anderson and
Prior, 2010)
• This region is called the "Des Moines
Lobe," Its name refers to the location
of Iowa's capital city at the
southernmost limit of this former ice
mass. (Harr et al, 2010)
• The geologically fresh deposits of the
Des Moines Lobe still display the
special landscape shapes that result
from direct contact with melting and
disintegrating glacial ice. (Anderson
and Prior, 2010)
• The Flood of 1993 was the defining
erosional process that uncovered
Devonian Fossil Gorge. Moderate
wind and water erosion is responsible
for the current weathering of the
Gorge. Acid rain leads to chemical
weathering of the Gorge’s limestone.
http://www.igsb.uiowa.edu/Bro
wse/glatrail/glatrail.htm
Iowa EcologyIowa Ecology
http://www.igsb.uiowa.edu/portrait/3change/Change.htm
Ecological feature: Iowa PrairieEcological feature: Iowa Prairie
• Iowa had the largest percentage of its area covered by
tallgrass prairie - 30 million acres before European
settlement (IAN, 1998)
• Now, only 0.01% of the original prairie is left
• Iowa prairie originated nine to ten thousand years ago,
following the retreat of Iowa’s most recent glaciers.
(IAN,1998)
– Prairies formed in much of north and central Iowa due to warm,
dry climatic conditions
• Once established, prairie plants held their ground. The
dense roots of prairie plants did not allow invading trees
and shrubs to grow. (IAN, 1998)
Plants and Animals in the IowaPlants and Animals in the Iowa
Prairie (IAN, 1998)Prairie (IAN, 1998)
• Plants (Autotrophs):
– Big bluestem
– Grasses: Indian grass, Code
grass, Switch grass
– Wildflowers: Compass plant,
black-eyed Susan, lead plants,
prairie coneflower
• Wildlife (Heterotrophs):
– Bison, elk, antelope, wolves,
prairie dogs, red fox, coyote,
moles, shrew
– Birds: meadowlark, red-tailed
hawk
– Insects: spittelbugs, ants,
grasshoppers
– Reptiles and amphibians:
ornate box turtle, western
hognoose snakehttp://www.nps.gov/archive/wica/images/Big_Blue_Stem.jpg
http://www.nps.gov/wica/naturescience/images/Prairie-Coneflower.jpg
Food webFood web
in an Iowain an Iowa
PrairiePrairie
(arrows in the(arrows in the
direction of energydirection of energy
flow)flow)
http://www.nps.g
ov/archive/wica/i
mages/Big_Blue
_Stem.jpg
http://www.natur
ehills.com/image
s/productImages
/black_eyed_sus
an_goldstrum_1.
jpg
http://www.nps.g
ov/wica/naturesc
ience/images/Pr
airie-
Coneflower.jpg
Endangered/Exploited species inEndangered/Exploited species in
IowaIowa
• In Iowa, Chapter 481B of
the Code of Iowa protects
endangered species
• Violations of the
provisions of Chapter
481B for threatened or
endangered species are
misdemeanors
punishable by a fine of up
to $100.
• Complete list:
http://www.iowadnr.gov/w
ildlife/files/wildinfo.html
http://www.iowadnr.gov/other/threatened.html
Iowa
Pleistocene
land snail
Higgins eye
pearly mussel
Osprey
Western
prairie fringed
orchid
Local biodiversityLocal biodiversity
• Iowa’s landscape and biodiversity have changed
drastically over the past 150 years and the
prairie has been destroyed (IAN, 1998)
• Alteration and redirection of many Iowa streams
has caused a decrease in the marshland and
marshland communities throughout the state
• Pollution and land clearing are the major forces
that have changed Iowa’s biodiversity (IAN,
1998)
Renewable andRenewable and
Nonrenewable resources ofNonrenewable resources of
IowaIowa
Mineral/ Rock ResourcesMineral/ Rock Resources
• Most of the mineral
resources in Iowa are
used for construction and
building materials
Examples are:
– Clay and shale
– Crushed limestone
– Gypsum
– Cement
– Sand and gravel
• These minerals and rocks
are extracted from
quarries throughout the
state
http://www.igsb.uiowa.edu/Browse/gypsum/gypsum.htm
NonrenewableNonrenewable
resources found inresources found in
Iowa: CoalIowa: Coal
• Small quantities of coal were first mined in
the 1840's near Fort Des Moines and along
the lower Des Moines River (Coal, 2002)
• In 1854 the Rock Island Railroad reached
the Mississippi River, and by 1860, 500
miles of track existed in Iowa. By 1876 the
North Western Railroad reached Council
Bluffs, and Iowa was the leading coal
producer west of the Mississippi and fifth in
the U.S. (Coal, 2002)
• By 1914 the state's rail network included
9,216 miles of track, and by 1918 annual
coal production in Iowa peaked at 9.3 million
tons.
• Production declined thereafter and the
industry shifted from underground to surface
mining operations. (Coal, 2002)
• By 1920, almost all Iowa coal mines had
been shut down, in favor of mining the
cleaner coal in Illinois. Mining operations
shifted from coal to gypsum and limestone
Iowa’s renewable resourcesIowa’s renewable resources
• The two major renewable energy sources
harvested in Iowa are wind energy and
bioenergy and biofuels
• Wind energy
– Iowa is the second largest producer of wind
energy in the US, just behind Texas. (IEC,
2010)
– Iowa has 3,670 MW of installed wind power
which is enough to power approximately
1,125,000 homes (IEC, 2010)
– Wind energy is producing jobs in Iowa
• Biomass/bioenergy
– Iowa has 31 ethanol plants in operation,
producing approximately 2.54 billion gallons
per year. (bottom picture)
– Iowa leads the nation in biofuels output
accounting for 26 percent of U.S. ethanol and
12 percent of biodiesel production capacity
(IARFA, 2010)
– Ethanol lowers harmful carbon monoxide
(CO) emissions by 30 percent and reduced
carbon dioxide (CO2) emissions by 27
percent. (IARFA, 2010)
– 11 landfills in Iowa that are candidates for
electric generation (Bird et. al, 2005)
http://iowa.com/wp-content/uploads/2008/12/ilive-weather.jpg
Human impact on our resourcesHuman impact on our resources
• As humans it is our responsibility to conserve
nonrenewable natural resources and replace
nonrenewable resources with cleaner, more
environmentally friendly renewable resources
• Going green can mean and increase in the
number of jobs. In Iowa alone, ethanol and
biodiesel production supported 83,000 jobs in
2008 (IARFA, 2010)
• Relying on alternate energy sources can cut our
dependence on foreign oil , since wind energy
and biofuels are produced right here in Iowa
ReferencesReferences
• (2004) Stratigraphic Column of Iowa, 2004. Natural Resources, Department of.
• Devonian Fossil Gorge photo: http://www.mvr.usace.army.mil/coralville/devonian_fossil_gorge.htm
• Flood of 1993 photo: http://www.igsb.uiowa.edu/browse/flood93/flood93.htm
• Gypsum photo: http://www.igsb.uiowa.edu/Browse/gypsum/gypsum.htm
• (2002) Coal Geology of Iowa. 2002 Keystone Coal Industry Manual ®
• Bedrock Geology map: http://www.igsb.uiowa.edu/browse/geoiowa/geoiowa.htm
• (1995) Iowa Biodiversity. Iowa Association of naturalists
• Iowa prairie map: http://www.igsb.uiowa.edu/portrait/3change/Change.htm
• Bird, L. et. al (2005) Iowa Renewable Resource Assessment
• Anderson, R.R. and Prior, J.C. (2010). Glacial Boulders in Iowa. Retrieved March 22, 2010 from
http://www.igsb.uiowa.edu/Browse/boulders/boulders.htm
• Harr, D.C. et. al (2010). Glacial Landmarks trail: Iowa’s Heritage of Ice. Retrieved March 22, 2010 from
http://www.igsb.uiowa.edu/Browse/glatrail/glatrail.htm
• Iowa Department of Natural Resources (DNR). (2010). General Geology. Retrieved March 23, 2010 from
http://www.igsb.uiowa.edu/service/geology.htm
• Prior, J.C. (1998) Devonian Fossil Gorge. Iowa Department of Natural resources. Retrieved March 20, 2010 from
http://www.igsb.uiowa.edu/browse/spillway/spillway.htm
• Iowa earthquake map: http://www.igsb.uiowa.edu/Browse/earthqua/iowa_quakes.htm
• Iowa Energy Center (IEC) (2010). Wind Energy in Iowa. Retrieved March 24, 2010 from http://www.energy.iastate.edu/renewable/wind/
• Iowa Wind Farm picture: http://iowa.com/wp-content/uploads/2008/12/ilive-weather.jpg
• Big Bluestem picture: http://www.nps.gov/archive/wica/images/Big_Blue_Stem.jpg
• Prairie cone flower picture: http://www.nps.gov/wica/naturescience/images/Prairie-Coneflower.jpg
• Black-eyed Susan picture: http://www.naturehills.com/images/productImages/black_eyed_susan_goldstrum_1.jpg
• Iowa Association of Naturalists (IAN) (1998). Iowa Prairies. Iowa Biological series. Iowa Association of Naturalists. (IAN-203)
• Mole picture: http://www.allstateanimalcontrol.com/images/large%20images/moleBig.jpg
• Iowa Renewable Fuel association (IARFA)(2010) . Ethanol Facts. Retrieved March 26, 20910 from
http://www.iowarfa.org/ethanol_facts.php

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Geology, ecology, and resources of iowa (1)

  • 1. Geology, Ecology, andGeology, Ecology, and Resources of IowaResources of Iowa By Danielle JannuschBy Danielle Jannusch
  • 2. Welcome to theWelcome to the Hawkeye StateHawkeye State • Iowa was a tremendous geologic and ecologic history. This presentation will discuss: – Geologic Feature: Devonian Fossil Gorge – Ecologic Feature: Iowa Prairie – Renewable and nonrenewable resources of Iowa
  • 4. Iowa Geologic historyIowa Geologic history • The oldest rocks in Iowa are buried deep underground. • Most of Iowa’s geologic history is written in sedimentary rocks, such as sandstone, limestone, dolomite and shale, which are over 3,000 feet thick in places. (DNR, 2010) • Iowa sedimentary rocks originated as layers of loose sediment accumulating in shallow seas and along coastal and floodplain environments between 74 million years ago (Cretaceous) and 530 million years ago (Cambrian). • Over time, this sediment was lithified into rock containing fossil remains of past animal and plant life. • Fossiliferous sedimentary rocks are found among the abundant outcrops of northeastern, eastern, and central Iowa • Most sedimentary rock exposures in Iowa are found along river valleys, at roadcuts, and in quarries. • Since most of our geologic history is buried, most of our knowledge comes from rock samples brought up to the land surface during the drilling of wells. • The oldest known formation in Iowa the Otter Creek Mafic Complex (about 2.95 billion years old), the youngest is the Wisconsinan glacial drift (about 10,000 years old). (DNR, 2010) • Additionally, river sediments that are still being deposited today.
  • 5. Iowa StratigraphicIowa Stratigraphic Column:Column: This column shows allThis column shows all the different rock typesthe different rock types found on the surfacefound on the surface and in the subsurfaceand in the subsurface of Iowa terrain Column.of Iowa terrain Column. This column has beenThis column has been used to correlate Iowaused to correlate Iowa rocks with sedimentaryrocks with sedimentary strata throughout thestrata throughout the Midwest and theMidwest and the countrycountry Source: http://publicatio ns.iowa.gov/48 62/1/EM-40.pdf
  • 6. Geologic Feature:Geologic Feature: Devonian FossilDevonian Fossil GorgeGorge • Discovered during the Flood of 1993 when floodwaters from Coralville Lake came over the spillway eroded away 15 feet of glacial-age sediments to expose 375-million-year old fossiliferous bedrock. • The rocks of the gorge: The dominant rock type at Devonian fossils gorge is fossiliferous limestone. The limestone is rich in crinoids, corals, stromatoporoids and several species of brachiopod fossils. • Limestone is comprised of calcite. • History of the sediments: These sediments were deposited during the Devonian Period about 375 million years ago, when eastern Iowa was covered with a shallow sea. The fossils suggest that this was a reefal normal marine environment with a moderate undercurrent (Prior, 1998) A recreation of the Devonian of Iowa 1993- The fossil sea is discovered after the flood of 1993 Newly designed entrance to the Gorge http://www.igsb.uiowa.edu/browse/spillway/spillway.htm
  • 7. How has plate tectonics affectedHow has plate tectonics affected the Gorge?the Gorge? • Current earthquake activity: Only 13 earthquakes with epicenters in Iowa are known in historic times. The first known occurrence was in 1867 near Sidney in southwest Iowa; the most recent occurrence was in 2004 near Shenandoah in SW Iowa. The largest Iowa earthquake (Mercalli magnitude VI) occurred near Davenport in southeast Iowa in 1934. (DNR, 2010) • Activity around the Gorge is rare, but some of the strata are inclined. • Looking north toward the Coralville Lake Spillway some of the limestone strata are inclined and domed. (DNR, 2010) • It has been suggested that this inclination may be the result of irregular settling of the sedimentary layers when they were still soft, or the result of much later, broad-scale warping of rock units across the Midwest. • Small geologic faults are also exposed here, with vertically displaced strata and tiny gouges along the rock faces indicating movement in the geologic past (about 310 million years ago) (Prior, 1998) •http://www.igsb.uiowa.edu/Browse/earthqua/iowa_quakes.htm
  • 8. Glacial and Surficial Processes andGlacial and Surficial Processes and their impact on Iowatheir impact on Iowa • Glacial processes are responsible for many of the geologic features throughout the state. • The “lake district” area of northern Iowa is dominated by natural lakes and bogs, among irregularly shaped hills, and in the boulders- all evidence of glacial activity (Anderson and Prior, 2010) • This region is called the "Des Moines Lobe," Its name refers to the location of Iowa's capital city at the southernmost limit of this former ice mass. (Harr et al, 2010) • The geologically fresh deposits of the Des Moines Lobe still display the special landscape shapes that result from direct contact with melting and disintegrating glacial ice. (Anderson and Prior, 2010) • The Flood of 1993 was the defining erosional process that uncovered Devonian Fossil Gorge. Moderate wind and water erosion is responsible for the current weathering of the Gorge. Acid rain leads to chemical weathering of the Gorge’s limestone. http://www.igsb.uiowa.edu/Bro wse/glatrail/glatrail.htm
  • 10. Ecological feature: Iowa PrairieEcological feature: Iowa Prairie • Iowa had the largest percentage of its area covered by tallgrass prairie - 30 million acres before European settlement (IAN, 1998) • Now, only 0.01% of the original prairie is left • Iowa prairie originated nine to ten thousand years ago, following the retreat of Iowa’s most recent glaciers. (IAN,1998) – Prairies formed in much of north and central Iowa due to warm, dry climatic conditions • Once established, prairie plants held their ground. The dense roots of prairie plants did not allow invading trees and shrubs to grow. (IAN, 1998)
  • 11. Plants and Animals in the IowaPlants and Animals in the Iowa Prairie (IAN, 1998)Prairie (IAN, 1998) • Plants (Autotrophs): – Big bluestem – Grasses: Indian grass, Code grass, Switch grass – Wildflowers: Compass plant, black-eyed Susan, lead plants, prairie coneflower • Wildlife (Heterotrophs): – Bison, elk, antelope, wolves, prairie dogs, red fox, coyote, moles, shrew – Birds: meadowlark, red-tailed hawk – Insects: spittelbugs, ants, grasshoppers – Reptiles and amphibians: ornate box turtle, western hognoose snakehttp://www.nps.gov/archive/wica/images/Big_Blue_Stem.jpg http://www.nps.gov/wica/naturescience/images/Prairie-Coneflower.jpg
  • 12. Food webFood web in an Iowain an Iowa PrairiePrairie (arrows in the(arrows in the direction of energydirection of energy flow)flow) http://www.nps.g ov/archive/wica/i mages/Big_Blue _Stem.jpg http://www.natur ehills.com/image s/productImages /black_eyed_sus an_goldstrum_1. jpg http://www.nps.g ov/wica/naturesc ience/images/Pr airie- Coneflower.jpg
  • 13. Endangered/Exploited species inEndangered/Exploited species in IowaIowa • In Iowa, Chapter 481B of the Code of Iowa protects endangered species • Violations of the provisions of Chapter 481B for threatened or endangered species are misdemeanors punishable by a fine of up to $100. • Complete list: http://www.iowadnr.gov/w ildlife/files/wildinfo.html http://www.iowadnr.gov/other/threatened.html Iowa Pleistocene land snail Higgins eye pearly mussel Osprey Western prairie fringed orchid
  • 14. Local biodiversityLocal biodiversity • Iowa’s landscape and biodiversity have changed drastically over the past 150 years and the prairie has been destroyed (IAN, 1998) • Alteration and redirection of many Iowa streams has caused a decrease in the marshland and marshland communities throughout the state • Pollution and land clearing are the major forces that have changed Iowa’s biodiversity (IAN, 1998)
  • 15. Renewable andRenewable and Nonrenewable resources ofNonrenewable resources of IowaIowa
  • 16. Mineral/ Rock ResourcesMineral/ Rock Resources • Most of the mineral resources in Iowa are used for construction and building materials Examples are: – Clay and shale – Crushed limestone – Gypsum – Cement – Sand and gravel • These minerals and rocks are extracted from quarries throughout the state http://www.igsb.uiowa.edu/Browse/gypsum/gypsum.htm
  • 17. NonrenewableNonrenewable resources found inresources found in Iowa: CoalIowa: Coal • Small quantities of coal were first mined in the 1840's near Fort Des Moines and along the lower Des Moines River (Coal, 2002) • In 1854 the Rock Island Railroad reached the Mississippi River, and by 1860, 500 miles of track existed in Iowa. By 1876 the North Western Railroad reached Council Bluffs, and Iowa was the leading coal producer west of the Mississippi and fifth in the U.S. (Coal, 2002) • By 1914 the state's rail network included 9,216 miles of track, and by 1918 annual coal production in Iowa peaked at 9.3 million tons. • Production declined thereafter and the industry shifted from underground to surface mining operations. (Coal, 2002) • By 1920, almost all Iowa coal mines had been shut down, in favor of mining the cleaner coal in Illinois. Mining operations shifted from coal to gypsum and limestone
  • 18. Iowa’s renewable resourcesIowa’s renewable resources • The two major renewable energy sources harvested in Iowa are wind energy and bioenergy and biofuels • Wind energy – Iowa is the second largest producer of wind energy in the US, just behind Texas. (IEC, 2010) – Iowa has 3,670 MW of installed wind power which is enough to power approximately 1,125,000 homes (IEC, 2010) – Wind energy is producing jobs in Iowa • Biomass/bioenergy – Iowa has 31 ethanol plants in operation, producing approximately 2.54 billion gallons per year. (bottom picture) – Iowa leads the nation in biofuels output accounting for 26 percent of U.S. ethanol and 12 percent of biodiesel production capacity (IARFA, 2010) – Ethanol lowers harmful carbon monoxide (CO) emissions by 30 percent and reduced carbon dioxide (CO2) emissions by 27 percent. (IARFA, 2010) – 11 landfills in Iowa that are candidates for electric generation (Bird et. al, 2005) http://iowa.com/wp-content/uploads/2008/12/ilive-weather.jpg
  • 19. Human impact on our resourcesHuman impact on our resources • As humans it is our responsibility to conserve nonrenewable natural resources and replace nonrenewable resources with cleaner, more environmentally friendly renewable resources • Going green can mean and increase in the number of jobs. In Iowa alone, ethanol and biodiesel production supported 83,000 jobs in 2008 (IARFA, 2010) • Relying on alternate energy sources can cut our dependence on foreign oil , since wind energy and biofuels are produced right here in Iowa
  • 20. ReferencesReferences • (2004) Stratigraphic Column of Iowa, 2004. Natural Resources, Department of. • Devonian Fossil Gorge photo: http://www.mvr.usace.army.mil/coralville/devonian_fossil_gorge.htm • Flood of 1993 photo: http://www.igsb.uiowa.edu/browse/flood93/flood93.htm • Gypsum photo: http://www.igsb.uiowa.edu/Browse/gypsum/gypsum.htm • (2002) Coal Geology of Iowa. 2002 Keystone Coal Industry Manual ® • Bedrock Geology map: http://www.igsb.uiowa.edu/browse/geoiowa/geoiowa.htm • (1995) Iowa Biodiversity. Iowa Association of naturalists • Iowa prairie map: http://www.igsb.uiowa.edu/portrait/3change/Change.htm • Bird, L. et. al (2005) Iowa Renewable Resource Assessment • Anderson, R.R. and Prior, J.C. (2010). Glacial Boulders in Iowa. Retrieved March 22, 2010 from http://www.igsb.uiowa.edu/Browse/boulders/boulders.htm • Harr, D.C. et. al (2010). Glacial Landmarks trail: Iowa’s Heritage of Ice. Retrieved March 22, 2010 from http://www.igsb.uiowa.edu/Browse/glatrail/glatrail.htm • Iowa Department of Natural Resources (DNR). (2010). General Geology. Retrieved March 23, 2010 from http://www.igsb.uiowa.edu/service/geology.htm • Prior, J.C. (1998) Devonian Fossil Gorge. Iowa Department of Natural resources. Retrieved March 20, 2010 from http://www.igsb.uiowa.edu/browse/spillway/spillway.htm • Iowa earthquake map: http://www.igsb.uiowa.edu/Browse/earthqua/iowa_quakes.htm • Iowa Energy Center (IEC) (2010). Wind Energy in Iowa. Retrieved March 24, 2010 from http://www.energy.iastate.edu/renewable/wind/ • Iowa Wind Farm picture: http://iowa.com/wp-content/uploads/2008/12/ilive-weather.jpg • Big Bluestem picture: http://www.nps.gov/archive/wica/images/Big_Blue_Stem.jpg • Prairie cone flower picture: http://www.nps.gov/wica/naturescience/images/Prairie-Coneflower.jpg • Black-eyed Susan picture: http://www.naturehills.com/images/productImages/black_eyed_susan_goldstrum_1.jpg • Iowa Association of Naturalists (IAN) (1998). Iowa Prairies. Iowa Biological series. Iowa Association of Naturalists. (IAN-203) • Mole picture: http://www.allstateanimalcontrol.com/images/large%20images/moleBig.jpg • Iowa Renewable Fuel association (IARFA)(2010) . Ethanol Facts. Retrieved March 26, 20910 from http://www.iowarfa.org/ethanol_facts.php