shale & sandstone 2015 - iihr · lafarge corporation’s davenport cement plant operates the...

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Till (0.5-2.6 mil. yrs. old) Limestone & Dolomite (380-400 million yrs. old) Shale & Cherty Dolomite (445-450 million yrs. old) Cherty Dolomite (420-440 million yrs. old) Shale & Sandstone (~310 million yrs. old) Shale & Dolomite (360-380 million yrs. old) Wapsinonoc Creek Cedar River Sugar Creek Iowa River Mississippi River Daily Geology: Today’s ride is loaded with intriguing geologic features. The Iowa City - Clinton Fault Zone (western end of cross- section) is a similar fault system as the PRFZ that you rode over yesterday. Near the confluence of the Iowa and Cedar rivers was a huge lake that formed during the last ice age, called Glacial Lake Calvin. Of course you can’t miss the Cleona Channel, the deep bedrock vally near the eastern end of the ride. It’s obvious that Iowa’s glacial and bedrock geologic record are far from ordinary. At some time in the Pre- Illinoian (between about 0.5 and 2.5 million years ago) a continental glacier first pushed into Illinois and diverted the Mississippi River to the west through Scott, Muscatine and Louisa counties. The channel was incised about 300 feet into the bedrock, as seen in the bedrock elevation map above, making it one of Iowa’s most prominent bedrock channels. It was overridden by Pre- Illinoian glaciers, then reoccupied by the river on several occasions, most recently during the Illinoian about 100,000 years ago. RAGBRAI 2015 will ride above the Cleona Channel between Atalissa and Durant. Had you been there a few hundred thousand years ago you might be in the middle of a Mississippi River surging with glacial melt water. Cleona Channel RAGBRAI Day 7 2015 Saturday, July 25

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Page 1: Shale & Sandstone 2015 - IIHR · Lafarge Corporation’s Davenport Cement Plant operates the larger of the two quarries to produce stone for one of Iowa’s two cement plants. The

Till

(0.5

-2.6

m

il. y

rs. o

ld)

Lim

esto

ne &

Dol

omit

e(3

80-4

00 m

illio

n yr

s. ol

d)

Shal

e &

Che

rty

Dol

omit

e (4

45-4

50 m

illio

n yr

s. ol

d)

Cher

ty D

olom

ite

(420

-440

mill

ion

yrs.

old)

Shal

e &

San

dsto

ne(~

310

mill

ion

yrs.

old)

Shal

e &

Dol

omit

e(3

60-3

80 m

illio

n yr

s. ol

d)Wap

sino

noc

Cree

k

Ceda

rRi

ver

Suga

rCr

eek

Iow

aRi

ver

Mis

siss

ippi

Rive

r

Dai

ly G

eolo

gy:

Toda

y’s

ride

is lo

aded

with

in

trig

uing

geo

logi

c fe

atur

es.

The

Iow

a C

ity -

Clin

ton

Faul

t Zo

ne (w

este

rn e

nd o

f cro

ss-

sect

ion)

is a

sim

ilar f

ault

syst

em

as th

e PR

FZ th

at y

ou ro

de o

ver

yest

erda

y. N

ear t

he c

onflu

ence

of

the

Iow

a an

d C

edar

rive

rs

was

a h

uge

lake

that

form

ed

duri

ng th

e la

st ic

e ag

e, c

alle

d G

laci

al L

ake

Cal

vin.

Of c

ours

e yo

u ca

n’t m

iss

the

Cle

ona

Cha

nnel

, the

dee

p be

droc

k va

lly n

ear t

he e

aste

rn e

nd o

f the

ri

de.

It’s

obvi

ous

that

Iow

a’s

glac

ial a

nd b

edro

ck g

eolo

gic

reco

rd a

re fa

r fro

m o

rdin

ary.

At some time in the Pre-Illinoian (between about 0.5 and 2.5 million years ago) a continental glacier first pushed into Illinois and diverted the Mississippi River to the west through Scott, Muscatine and Louisa counties. The channel was incised about 300 feet into the bedrock, as seen in the bedrock elevation map above, making it one of Iowa’s most prominent bedrock channels. It was overridden by Pre-Illinoian glaciers, then reoccupied by the river on several occasions, most recently during the Illinoian about 100,000 years ago. RAGBRAI 2015 will ride above the Cleona Channel between Atalissa and Durant. Had you been there a few hundred thousand years ago you might be in the middle of a Mississippi River surging with glacial melt water.

Cleona Channel

RAGBRAIDay 7

2015Saturday, July 25

Page 2: Shale & Sandstone 2015 - IIHR · Lafarge Corporation’s Davenport Cement Plant operates the larger of the two quarries to produce stone for one of Iowa’s two cement plants. The

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850 ft.

545 ft.

Elevation

Coralville

IowaCity

West Liberty

Atalissa

Moscow

Durant

Wilton Walcott

Davenport

Duck CreekIowa

River

* Cover photo: Limestone quarry near Moscow, right on the western edge of the Cleona Channel.

Just southwest of Davenport, on Iowa Highway 20 along the Mississippi River, two large limestone quarries produce high calcium limestone (>96%) from Middle Devonian (~ 385 million years old) shallow marine rocks. Lafarge Corporation’s Davenport Cement Plant operates the larger of the two quarries to produce stone for one of Iowa’s two cement plants. The limestone is mixed with clay, iron, and other materials then fired to 2,700ºF in a huge rotary kiln to form ‘clinker’. The cooled clinker is ground to fine powder producing Portland Cement. The smaller quarry is associated with an underground mine, where Linwood Mining and Materials produces high calcium limestone and aggregates. The high calcium limestone is produced for the manufacturing of glass, calcium supplements in animal feed, calcium oxide for steel production and water pH control, and a variety of other uses. Both companies have access to Mississippi River barges to transport their finished products.

Parks and preserves

Cities and towns

Nahant Marsh, a 265-acre preserve nestled in southwest Davenport, is the largest urban wetland on the Upper Mississippi River. It is part of a 513-acre wetland complex that is bordered by the Mississippi River, Interstate 280, and Highway 22. Nahant is an Algonquin word that roughly translate to almost an island. Nahant is indeed a fitting name, considering that Nahant Marsh had been a former side channel of the Mississippi River and a portion of the land was at one time, an island in the river. Occasionally when the river floods, the area again becomes an island.Much later, a portion of the area became a gun club and then an EPA Superfund site. Following the clean-up of lead shot in 1999, the Nahant Marsh Education Center was formed to educate the public about the preserve and to protect the ecosystems that comprise the preserve.Today, thousands of people from all walks of life enjoy educational experiences at the marsh. Just as important, Nahant Marsh is home to over 150 species of birds, 400 species of plants, and a wide variety of mammals, fish, reptiles, amphibians and insects, including several rare and endangered species. Hiking trails, boardwalks, a dock, and bird blind at Nahant Marsh allow visitors to experience different habitats, including prairies, sedge meadows, bottomland forests, and the marsh.

The Old Capitol building in the heart of Iowa City began construction in 1840. The lower 2/3 of the structure was built using limestone blocks quarried from along the banks of the Iowa River in several places within about half a mile of the construction site. The Devonian age (~385 million years old) Coralville Formation is a very fossiliferous limestone unit with a highly variable composition. Luckily another rock formation, the State Quarry Member (also Devonian), was discovered about 13 miles upriver. It is a coarse-grained skeletal calcarenite consisting entirely of broken pieces of fossil shells in a calcite cement matrix. The uniformity of the State Quarry Member was ideal for construction, and thus the top 1/3 of the Old Capital was finished with this rock. State Quarry Member limestone was also used in the foundation of the current state capitol building in Des Moines, built in the 1870’s.

Davenport Limestone Mines

Nahant: Almost an Island Old Cappy