Soils and Geology of Wisconsin Field Trip, May 2012
Steven Dutch, Natural and Applied Sciences, University
of Wisconsin - Green Bay
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May 14, 2012

Pemene Falls
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Loading up. |
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 | En
echelon fractures |
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Close-up of the volcanic rocks showing feldspar spherulites. |
Quiver Falls
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 | A
guidebook assured us that pillow lava was visible here. Maybe when the water
is lower. |
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 | An
impromptu stop to examine the metavolcanics. |
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Outcrop on US 141 with granitic dikes intruding mafic metavolcanics. |
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Piers Gorge
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short lunch stop |
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Planed-off phyllite on the Menominee River. The opposite shore is Wisconsin. |
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Phyllite outcrop |
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Potholes in the phyllite. |
 | Wonder what the soil is? |
 | A-a-a-a-nd it's a histosol! |
 | Jack
looks on approvingly from his pulpit. |
Lake Ellen Kimberlite
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 | In
2009, this area was being logged and we had to hike half a mile from the
parking area. This time we got to drive right up to it. |
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Archean Gneiss
Deformed Proterozoic Rocks
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 | Camp
at Van Riper State Park, with the usual obligatory Frisbee games. |
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May 15, 2012

Champion Mine
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Champion Mine brings a new meaning to the term "road metal" since the whole
ground sparkles with specular hematite. |
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Jasper Knob, Ishpeming
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folds are dramatic because they plunge at a very low angle into the surface.
When seen down-plunge, they're insignificant crinkles. |
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 | View
of Ishpeming |
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Archean Pillow Basalts
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 | There are two perfectly respectable geological uses for the term "cleavage,"
but Clarissa's shirt opts for the biological usage.
No, not that
usage, you creep. The cell division usage. |
 | It's
a mad sprint to get across the highway. |
Presque Isle Park, Marquette
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Precambrian Jacobsville Sandstone atop Archean ultramafic rocks. The contact
is halfway up the cliff. |
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edge of the cliff is fenced off and this is why. |
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Walking up the west side of the island. |
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 | Cross-bedding in the Jacobsville Sandstone. |
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Basal conglomerate. |
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| Above: views of the dike in the Archean rocks. | Below: Lake
Nipissing shorelines. |
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 | Note
the penny for scale. We estimated that this nugget would make 10 million
pennies or about $100,000 worth, back when they still made pennies out of
copper. |
 | Iron
ore dock |
Stromatolites
 | The
quarry across from the Michigan Visitor Center displays the pinched out end
of the Marquette Synclinorium. The Kona Dolomite hosts world-class
stromatolites. |
 | Another mad sprint across a busy highway. |
 | The
stromatolites are up a steep trail at the west end of the quarry. |
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Spaced cleavage |
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 | See,
Clarissa, this is what geologists mean by "cleavage!" |
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 | You
have to admire someone who starts out as a zygote and works her way up!
The T-shirt was a fund-raiser for TriBeta, an honor society in biology. |
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 | And
another mad sprint back to the vehicles. |
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 | View
of Presque Isle. |
Laughing Whitefish Falls
 | This
is the paved road. |
 | The
unpaved road was much improved from 2009 when we were here last and was
actually better than the "good" road. |
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Au Train Spillway

During the retreat of the glaciers, ice blocked the eastern outlet of
Lake Superior, causing water to spill through a low spot on the drainage
divide (white arrows).
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lake is actually a reservoir, the Cleveland Cliffs Basin, named for the
Cleveland Cliffs iron mining company.
Below: atop the dam. |
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 | The
view of Au Train Falls is spoiled by a pipe that runs to a small
hydroelectric plant. |
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Munising
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 | After a warm day, the wind picked up. By the time we pulled in, it was
screaming. |
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May 16, 2012

Chapel Rock
 | We
got up to a frosty but much less windy sunrise. |
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Ongoing improvements to the parking area meant another half mile to the lake shore. |
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Chapel Falls |
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 | At
one time Chapel Rock was connected to the bluffs by an arch, which collapsed
sometime in the 1940's. One root remains, connecting the tree to the bluffs.
One good storm could easily take that tree down. |
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Enormous trough cross-beds in the sandstones. |
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 | How
current ripple marks form. |
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 | This is what Chapel Rock looked like in 2000, seen from a boat. It hasn't
had any major alterations since then. |
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 | Sara
had the most interesting footwear I've ever seen. |
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 | Jill
and Kevin Fermanich |
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Recharging their solar cells. |
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 | This
time we took the trail up the western side of the valley. |
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Soils Stop
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 | Even
from here it's an obvious spodosol. |
Lake Superior Overlook
Log Slide, Grand Sable Dunes
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 | A
log hauler. Logs weere strapped to the underside of the axle. |
 | A
sledge. Logging was often easier in the winter when the ground was frozen. |
 | A
chute once extended down the dunes here, where logs were skidded to barges
offshore. |
 | A
newspaper article at the overlook recounts a tragic freak accident where a
large log slid down the chute, but instead of plunging into the lake, hit
the surface and skipped. It struck two men on a barge, killing both
instantly. |
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 | The
overlook here gives a sweeping view of the Grand Sable Dunes. The dunes are
perched, that is, accumulated on top of an elevated surface. "Sable" in
French simply means "sand;" the name of the fur "sable" has a different
origin.
So "Grand Sable" just means "large sand." I agree. |
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Grand Sable Dunes
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A blowout or deflation basin. An "enud" (that's "dune" spelled backwards.) |
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Tree roots exposed by wind erosion. |
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A stabilized, vegetated blowout. |
Grand Marais
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general store in Grand Marais has a little Zen garden of "omars." These are
metapelites from the Omaralluk Formation in Hudson's Bay, the only known
source. The spherical holes were made when concretions weathered out. The
store owner said that, after agates, these were the most collected rocks on
the shore. Curiously enough, there are apparently none on the shore at
Munising. |
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Grand Sable Lake
Panoramas
Miners' Castle
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 | Miners' Castle is the promontory at far left. |
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Miners Castle in 2000 when it really did look like a castle. The rear tower
collapsed in 2006. |
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 | Note
the large arch just left of the nearer point. |
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 | Rangers on patrol. |
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Carbonate cap rocks determine the topography at Pictured Rocks but are hard
to see and all but impossible to look at close up. Here they form the blocky
top ten meters or so of the cliff. |
May 17, 2012

Breaking Camp
Munising Overlook
Outwash Terraces
 | Fire
towers like this once dotted the wooded parts of the U.S. Now, with
satellites, cell phones and aircraft, they're mostly gone and most of the
rest are unmanned. |
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 | O
horizon, check. E horizon, yes indeed. Dark upper B horizon with iron
enrichment, yep. Spodosol. |
 | Seen
from the south (beyond the teraces) the last terrace has a raised lip. |
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Burnt Bluff Group
Kitchi-ti-Kipi (Big Spring)
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Kitchi-ti-Kipi is part of the oddly named Palms Book State Park, which isn't
really that odd a name. The land was sold for a token amount by the
Palms-Book Land Company, founded by Charles Louis Palms and Frank Book.
Dropping the hyphen doesn't help. |
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Captain Luczaj at the helm.
Below: Thar she blows! |
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Above: Instead of a glass bottom, the raft simply has an open well where you
can look down.
Left and below: Sand boils up continually where spring
water enters the pool. The configuration of the bottom is constantly
changing.
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About to dock |
 | View
across the spring. The cable guides the raft. |
 | Another group takes the raft out for a spin. |
Stephenson Moraines
 | A
roadside stop to look at the material of a drumlin. |
 | It's
a very sandy and rocky, angular till. |
 | And
it's an alfisol, sorta. |
 | On
the crest of a drumlin.
Below: panorama of the southeast side of the
drumlin |
 | View
along the crest of the drumlin |
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 | Hey
Kevin, any chance we can do some aridisols for a change? Something where
we're not in the water? |
 | View
from the top of a drumlin. |
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Created 21 May 2012, Last Update
22 May 2012
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