Day 139: Howell Heflin Lock & White Cliffs of Epes
Day 139: December 4: It was a nice morning on Gainsville Lake at our anchorage called Cooks Bend Cutoff. Still not as warm as I would like; its amazing how far south we have to go to feel warm.
At around 8:00 a.m. the 3 Musketeers (John, Frank and David) got in the dinghy to find our jugs and hopefully our dinner.
While we slept, a large grass pad had floated in between the boats. It looked like we had planted it overnight.
We untied Summer Fling and Zendeavor; pulled up our bow and stern anchors and got UW at 9:00 a.m. Skies turned sunny and temps got warm enough for us to shed our coats even while driving from the flybridge. We still haven't found 80 degrees yet! We've been chasing for a long time.
The Howell Heflin Lock, located at Mile 266.1 was only about 10 miles from our anchorage; we contacted the Lock-master while en-route; she came back with such a friendly attitude. In her lovely southern drawl, she told us to keep her coming and the lock would be ready for us. We had passed a sailboat named Just Right a few miles before the lock and alerted the lock that he was coming along and would be locking through with us as well. Shortly thereafter Just Right called the lock and offered to wait until the next locking cycle if the Lock-master preferred locking us through first; but she told him that we would wait on him which we had no problem with.
Our travels took us from Gainsville Lake to Demopolis Lake along the Tenn-Tom Waterway. Houses on stilts, shacks, eroded banks, floating logs, deadheads and warning signs kept our attention. From one river bend to another, things change and you never know what you might see.
We soon cruised by the White Cliffs of Epes in Epes, AL. They are part of the Selma Chalk formations which were deposited at about the same time as England's famous White Cliffs of Dover. The 80-foot cliffs towered over the river, catching the afternoon sunlight. Near the cliffs is Fort Tombecbe, built by the French in the late 1730's during skirmishes with the British and their Native American allies. It eventually became a supply post for European settlers and later gave the Tombigbee its name.
According to archeologists, the chalk is a form of limestone; it is exposed where the river cut through and also lies underneath the land of Alabama's Black Belt. It began forming in the Cretaceous Period millions of years ago and is composed of the remains of single-celled marine organisms and lime-producing algae. The stunning cliffs are a window into what Alabama might have been like when dinosaurs roamed the region.
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