Tuesday, September 10, 2019

McAline (#41) Dam and The "Falls of the Ohio" River at Louisville, KY

(Satellite)

USACE-recreation
"PL 97-137, passed by the U.S. Congress in 1982, designated the fossil beds and falls area as 'The Falls of the Ohio National Wildlife Conservation Area.'"
In the 981-mile length of the Ohio River, there is only one place where it flows over bedrock, the Falls of the Ohio. The rock here is an ancient Devonian Reef [nkytribune] and it is full of fossils. In this staircase diagram of the Ohio River where the vertical scale is exaggerated, you can clearly see the significant drop of the river bed near Louisville.
USACE-locks
The Falls of the Ohio is one of the largest naturally exposed Devonian Fossil Beds in the world.  The “Falls” is in fact not one waterfall, but a series of rapids, which prior to construction of the various locks and dams, dropped 26 feet in about 3 miles, forming a series of rapids, waterfalls, and chutes.  Now, the drop in elevation occurs entirely at the lock and dam structures.  The normal upper and lower water levels are 37 feet apart; the normal upper pool elevation is 420 feet above mean sea level and the lower pool is 383 feet above mean sea level.   The area has a rich cultural and natural history.  The area was used as a crossing point for animals, and as a hunting area for Native Americans.  More than 260 bird species have been sighted at the Falls, and a wide variety of other wildlife is present.  In the river’s natural state, boats could traverse the falls during periods of high water only, so the area became a stopping point while goods were unloaded and portaged, thus creating the towns of Louisville, Clarksville and Jeffersonville.  When there was enough water, boats could attempt to run one of three chutes, or passages through the Falls, but this required expertise and boats often wrecked during the attempt.  In 1830, the 1.9 mile privately owned and operated Portland Canal with a 3 flight lock at the lower end was finished.  By 1930, a new concrete and steel dam was built in conjunction with a hydroelectric plant project of the LG&E company.  The dam was constructed in an “L” shape, extending from the Indiana shore and gave the Falls area its present look.  See the webpage for McAlpine Locks and Dam for more history on the locks and dam. [Their link is broken. Try this one.] [USACE-recreation, expand the History heading]
I would call the Dam a Z shape. I marked up a satellite image to show the powerhouse and downstream control gates (red), the 2-mile fixed weir (orange), and the upstream control gates (blue).
Satellite plus Paint

This Z configuration is expensive because of the 2-mile fixed weir, but the two sets of control gates allow the USACE to emulate traditional summer-time flows (low) over the rapids by closing the five upstream gates and using the hydroelectric plant and the four lower gates to control the upper-pool depth. During the Spring and Fall wet seasons, it can give the upper gates priority to be open to maintain a strong flow across the rapids. This seasonal variance of the river flow helps preserve the wildlife that was established when the level of the river naturally varied significantly during the year. And it allows fossil viewing during the dry season.

See Louisville & Indiana/CSX/Pennsy Bridge for more photos of the upstream control structure.

Standing on the visitor's center viewing platform, I took a sequence of three photos from upstream (Southeast) to downstream (Northwest) to catch the weir wall and rapids.
20150508 1002


Gimp brightness +35, contrast +10
This view is looking at the upstream control structure from the path to the wheelchair accessible viewing platform.


Since there were people down by, and in, the river, I decided I should be able to get down there also.

But first I had to work my way over the debris field.
And then find a path over the rocks that did not require crossing deep crevasses. (This picture is taken looking down.)
This was as close to the river as I was willing to get.


But it was far enough out into the river bed to let me get a good view of the five Tainter gates (below). Note the water turbulence around the through-truss pier. It is a good thing it is built on rock. Even so, it is amazing that it has been able to avoid scouring after decades of turbulent flow around it. It does look like they have sheathed the base with a protective layer of concrete.


On the way back, I took an overview picture. Note that the dark rock in the foreground is significantly higher than the white rock below. And we can see another one of the crevasses in the upper layer. Most of the edge of the dark rock was a sharp drop off. That was part of the challenge of finding a path down to the white rock.
I didn't discover this ramp back to the parking lot until I went back up to the center. I came down the river bluff from the center using those stair steps peaking through the trees on the left. And I see now that I probably should have gone upstream from the base of those steps rather than the downstream path I took. The balcony of the interpretation center has a series of interpretive signs. They cover the topics of the Fossil Beds, Birds, Wildlife Conservation, and River Navigation.
The view below shows that the river is close to the visitation center when the river is high. That is, all of the foreground in the above photo is under water when the river is high.

High Water Images

Photo by Joe Virruso via Bridge Hunter
[Note that the Tainter gates are raised all the way and are practically parallel to the surface of the water.]

Bill Kalkman posted
In this view from the shoreline of the Ohio River, below the Falls of the Ohio Interpretive Center, your looking at the Louisville & Indiana Railroad's crossing of the river from Clarksville to Louisville. 6:52PM on 5-23-18 in Clarksville, IN.

Note how one photo taken by Andrew Raker in April, 2014, shows the lower pool at an intermediate level, but another photo by Andrew that same month shows the lower pool at a high level. And it was even higher in May, 2014.

Birds-Eye View
[In this view, you can see the Tainter gates are completely open. And the river is high enough that it is almost covering the dam walls.]
From the Wildlife Conservation sign

Low Water Images

Bridge Hunter photos taken by James Adorno in June, 2005; Robert Thompson in July, 2005; Ed Hollowell in July, 2005; and Andrew Raker in  September, and December of 2013, in August, 2011, in September, 2009, in June, July, August and October of 2008, and in September, 2007.

From the rest stop sign
From the Wildlife Conservation sign
[This picture taught me that they can create a low flow over the fossil beds during the Summer even if the river has a high flow by shutting the upper gates and opening the lower gates.]
In fact, Google Map captures that scenario.
Satellite, the upper gates are almost closed and the base of the dam wall is exposed
Satellite, while all of the lower gates are open
Bing's aerial view shows the case where both the upper and lower gates are partially open.
Satellite

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