A River Walk
Our courthouse reflected in the Oostanaula
The confluence of the Oostanaula (left) and Etowah (right) rivers to form the Coosa River. The bridge at the right is the Robert Redden Footbridge, a former railroad bridge that rotated on the center column so steamboats could continue up the Oostanaula. The bridge at the right takes Broad Street across the Etowah to the foot of Myrtle Hill.
The Silver Creek Trail crosses the Etowah on another railroad bridge turned footbridge (above) then follows little Silver Creek for three-quarters of a mile as it cascades down to the river.
I've lived in Rome since 1962, but I was completely ignorant of these picturesque downtown views until last week!
Notice the nearly vertical sandstone and shale layers, evidence of the crumpling of the former sea floor here in the Ridge and Valley province between the Blue Ridge and the Cumberland Plateau. At our school I can take my kids out to the driveway cut and pull shell fossils and crinoid stems from the crumbly sandstone.
The creek flattens a little as it nears the river.
The 1913 postcard (above) shows a mill on Silver Creek. I suspect the foreground is a bridge over the Etowah and the mill was at the mouth of Silver Creek. Or else it is high water on some other section of the creek. If anyone knows where this picture was taken, please let me know.
The confluence of the Oostanaula (left) and Etowah (right) rivers to form the Coosa River. The bridge at the right is the Robert Redden Footbridge, a former railroad bridge that rotated on the center column so steamboats could continue up the Oostanaula. The bridge at the right takes Broad Street across the Etowah to the foot of Myrtle Hill.
The Silver Creek Trail crosses the Etowah on another railroad bridge turned footbridge (above) then follows little Silver Creek for three-quarters of a mile as it cascades down to the river.
I've lived in Rome since 1962, but I was completely ignorant of these picturesque downtown views until last week!
Notice the nearly vertical sandstone and shale layers, evidence of the crumpling of the former sea floor here in the Ridge and Valley province between the Blue Ridge and the Cumberland Plateau. At our school I can take my kids out to the driveway cut and pull shell fossils and crinoid stems from the crumbly sandstone.
The creek flattens a little as it nears the river.
The 1913 postcard (above) shows a mill on Silver Creek. I suspect the foreground is a bridge over the Etowah and the mill was at the mouth of Silver Creek. Or else it is high water on some other section of the creek. If anyone knows where this picture was taken, please let me know.
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