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DanEE
Electrical
- Apr 20, 2005
- 288
I've posted the two links below from the NC DOT traffic cams with the thought that many of you might enjoy watching this bridge being built.
Above URLs from
Not a disaster (yet), but in the long debates, geology studys, lawsuits about where the new bridge under construction to replace the Herbert C Bonner bridge on the outer banks of North Carolina was to go, the possibility of becoming a bridge at sea that connects to no land was brought up given anticipated sea level rise. A major factor in the deterioration of the existing bridge and need to replace is movement of the channel to the South threating the sound end of the old bridge and also erosion around the in channel bridge support foundations.
The geological history of the Outer Banks is quite interesting in that it is a thin ribbon of sand on an approximately 50 - 75 mile wide sloping base from inland extending out to the continental shelf. The banks move inland with sea level rise and moved outward as sea level fell during the periods of colder earth temperatures.
One proposed plan was the build a much longer bridge inland and parallel to this section of more unstable outer banks as that is likely where the outer banks will end up somewhere down the road. Needless to say local real estate interests didn't care for that plan. Bridge to NoWhere
Early resident fisherman built their small houses where they could be rolled on logs to move them as the barrier islands moved and had trap doors in the floor that could be opened to help them stay in place during flooding. Visible in satellite photos and research in the area has found reminants of the outer banks on what is dry land well in land in North Carolina.
Enjoy the photos. While still images, they update frequently.
Above URLs from
Not a disaster (yet), but in the long debates, geology studys, lawsuits about where the new bridge under construction to replace the Herbert C Bonner bridge on the outer banks of North Carolina was to go, the possibility of becoming a bridge at sea that connects to no land was brought up given anticipated sea level rise. A major factor in the deterioration of the existing bridge and need to replace is movement of the channel to the South threating the sound end of the old bridge and also erosion around the in channel bridge support foundations.
The geological history of the Outer Banks is quite interesting in that it is a thin ribbon of sand on an approximately 50 - 75 mile wide sloping base from inland extending out to the continental shelf. The banks move inland with sea level rise and moved outward as sea level fell during the periods of colder earth temperatures.
One proposed plan was the build a much longer bridge inland and parallel to this section of more unstable outer banks as that is likely where the outer banks will end up somewhere down the road. Needless to say local real estate interests didn't care for that plan. Bridge to NoWhere
Early resident fisherman built their small houses where they could be rolled on logs to move them as the barrier islands moved and had trap doors in the floor that could be opened to help them stay in place during flooding. Visible in satellite photos and research in the area has found reminants of the outer banks on what is dry land well in land in North Carolina.
Enjoy the photos. While still images, they update frequently.