Traveling north to Superior along Highway 53 one can catch a
sign that you are crossing part of the Continental Divide, which is you have
moved from one drainage basin to another--on a continental scale. In this case,
water on one side runs to the Mississippi River and Gulf of Mexico, while water
on the other side runs into the Lake Superior, and ultimately the Atlantic
Ocean. Of course, there is also THE Continental
Divide which splits the nation between the Atlantic and Pacific Ocean watersheds. Each watershed is made up of a number of
smaller watersheds. For example, part of
Sun Prairie is in the Koshkonong Creek watershed, which is part of the Rock River watershed, and eventually to the Mississippi River watershed, which empties into the Gulf of Mexico. A lonely drop from Sun Prairie co-mingles with water from the far reaches of the large Mississippi River watershed. The Mississippi River watershed is the fourth
largest in the world.
Major streams are denoted on the Wisconsin State Highway
map. Following each stream you can see
its point of confluence with another stream, and its farthest reach; using
basic knowledge you will be able to ascertain the general direction of stream
flow and into which basin the water flows—Mississippi River, Lake
Michigan-Green Bay, or Lake Superior. One
of my earliest lessons in a physical geography course was looking at a
topographic map and delineating watersheds.
Often, two different watersheds have navigable waters that come near
each other. The City of Portage, WI is
so named as it is short walk between two different rivers serving two different
watersheds. To the north-easterly side of
Portage is the Fox River which eventually enters Green Bay, after a journey
through such great and well-known communities
as Berlin, and Omro. The remaining area
around Portage is the Wisconsin River, and part of its watershed, which flows
to the Mississippi River. The first
European settler to arrive at this location and discern its unique nature, as
being between two different watersheds, was Jesuit explorer Fr. Jacques
Marquette and his traveling companion Louis Joliet. In 1673 they had found the route they were
searching for—a primarily water route to
the Mississippi River. It only required a short portage between the Fox and the
Wisconsin.
General Location of the Niagara Escarpment |
Physical geography is formed by actions of climate and
weather, and various geological forces, such as volcanoes, earthquakes, folding
or faulting. Much of Wisconsin was
subject to various glacial activities over 10,000 years ago. But, not all of Wisconsin was affected by the
large ice sheets, with the last ice sheet being known as the Wisconsin Glacier. We have the driftless region which occupies
southwestern Wisconsin. We know this by
simply looking at the terrain of the glacial area which lacks the ridges and valleys
of the driftless region. Often hills in
the glacial region are related more to glacial features such as moraines,
kames, drumlins, eskers and kettles. Glacial
valleys are U shaped, stream valleys are V shaped. The glacier formed a unique topography. One of the largest drumlin fields in the
world is between Sun Prairie and Beaver Dam.
Holy Hill, in Washington County, is a unique feature as it is a kame
located on the pre-glacial Niagara escarpment.
This is the same escarpment that forms the eastern edge of Lake
Winnebago, arcs north to form the land area between Green Bay and Lake Michigan
(Door peninsula) and continues an arc
north and then south east to Lake Ontario, and Niagara Falls.
Holy Hill, Hubertus, WI |
The world, however, is made up of unique natural features,
of which Holy Hill is only one, and while significant to Wisconsin, would be an
afterthought within the nation. One unique
feature is an accident of geography. It
is a stream that would be a politician’s dream.
The head waters of this stream is a small lake in northwest Wyoming, and when that water outfalls
into a small creek, a drop does not know if it is bound for the Gulf of Mexico
and the Atlantic Ocean, or the Pacific Ocean.
This creek is in the Teton Wilderness and is known, quite appropriately
as Two Ocean Creek. Discovery, at least
as far as European settlers go, was in 1835 by Osborne Russell. Not recorded (as far as I know), but quite
likely, is that tribes indigenous to the area knew of its unique nature. Its headwaters is not unique, a small lake
forming the headwaters of a stream is rather common. Two Ocean Creek becomes unique as it heads
southerly and reaches an area known as Two Ocean Pass, which became a National
Natural Landmark in 1965. This small
creek divides at a specific location known as Parting of the Waters, which one
anal observer noted is .4 miles northwest of the low point of Two Ocean
Pass. You can likely guess from the name
what happens. A freak of nature, a gift
from God, the intractability of forces that form our landscape, or an accident
of geography, this stream splits into two streams, which itself is not unusual,
but what is unique is that water in one stream is in the Pacific basin, and
water in the other is in the Atlantic basin.
The two creeks formed by the split are known as Pacific Creek and
Atlantic Creek. There is a hole, so to
speak, in the Continental Divide and as water splashes against a not so easily
discernable ridge of the Continental Divide the way the splash droplets end will
tell if the drop of water will be going to the Pacific or Atlantic. It is said
that the water in Two Ocean Creek is more or less equally distributed between
these two major watersheds.
Estimated Two Ocean Creek Watershed, Wyoming |
When we hear about the Continental Divide, we usually think
of the tops of mountain ranges with a discernable split, and a discernable water
travel pattern. But, nature and
geography always have a gift in store for us.
A drop of rain that falls in the Two Ocean Creek drainage basin has an
equal chance of being swum in by the great whales of the northwest or by the
sharks of the Gulf of Mexico. Or a less
ignoble, but just as important, is that the drop may be evaporated, form as
part of cloud and eventually fall back to earth as rain. But in between is a journey that defines not
only importance of the water cycle to life on earth, but also recounts a journey
that represents the history of the nation.
Split of Two Ocean Creek into Atlantic Creek and Pacific Creek |
Atlantic Creek will travel 3,488 miles becoming part of the Yellowstone,
Missouri, and Mississippi Rivers, and end up in the Gulf of Mexico, which is
part of the Atlantic. Pacific Creek will
feed into the Snake and Columbia Rivers before entering the Pacific Ocean. Water actually covers the Continental Divide
at Parting of the Waters, such that a fish could swim between the two the world’s
major water bodies. In fact, it is
thought that this pass allowed the Yellowstone cutthroat trout to migrate from
the Snake River (Pacific basin) to the Yellowstone River (Atlantic basin). It was 110 years ago this coming month that
the Lewis and Clark expedition began their exploration of territory gained from
the Louisiana Purchase, and into the Oregon territory to the Pacific. One goal was to find a water route to the
Pacific. They never found it, but if
they had been in Wyoming, perhaps they would have.
Natural beauty is present in the earth, whether it is an
unnamed creek that starts from a spring, the Wisconsin River, Holy Hill, or the
magnificence of the Niagara Falls, and little recognized Two Ocean Creek. Although this comes a week past earth day, we
should think of every day as earth day, and be respectful of the natural
resources and beauty provided for wise use and enjoyment.
Note: All images courtesy of Google Images
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