- My Forums
- Tiger Rant
- LSU Recruiting
- SEC Rant
- Saints Talk
- Pelicans Talk
- More Sports Board
- Fantasy Sports
- Golf Board
- Soccer Board
- O-T Lounge
- Tech Board
- Home/Garden Board
- Outdoor Board
- Health/Fitness Board
- Movie/TV Board
- Book Board
- Music Board
- Political Talk
- Money Talk
- Fark Board
- Gaming Board
- Travel Board
- Food/Drink Board
- Ticket Exchange
- TD Help Board
Customize My Forums- View All Forums
- Show Left Links
- Topic Sort Options
- Trending Topics
- Recent Topics
- Active Topics
Started By
Message
re: Topography/Geology of Vidalia vs Natchez
Posted on 5/20/14 at 8:50 am to oldcharlie8
Posted on 5/20/14 at 8:50 am to oldcharlie8
Loes bluffs
LINK
It's very errosove silt that was wind blown and accumulated over thousands of years. That's why kudzu was introduced to slow the erosion down. Mudslides happen often in Natchez. They set up retaining walls and other means to slow it down. Vidalia side is flat due to prevailing wind and the river wants to meander west.
LINK
It's very errosove silt that was wind blown and accumulated over thousands of years. That's why kudzu was introduced to slow the erosion down. Mudslides happen often in Natchez. They set up retaining walls and other means to slow it down. Vidalia side is flat due to prevailing wind and the river wants to meander west.
This post was edited on 5/20/14 at 8:51 am
Posted on 5/20/14 at 8:57 am to knuckleballer
I think you guys have all the parts, but it can be stated more simply that what you have.
1) all the sediments at one time were silt-sized, and these formed the loess deposits.
2) the river runs through and cuts loess deposits into loess cliffs
3) over time the river meanders making one side of the river flatter (point bar) and the other steeper (cut bank)
4) what we see today is the result of a continuous eastward migration of a meander cutting into the land leaving flat land on the west side. It is now a straight portion of the river.
1) all the sediments at one time were silt-sized, and these formed the loess deposits.
2) the river runs through and cuts loess deposits into loess cliffs
3) over time the river meanders making one side of the river flatter (point bar) and the other steeper (cut bank)
4) what we see today is the result of a continuous eastward migration of a meander cutting into the land leaving flat land on the west side. It is now a straight portion of the river.
Posted on 5/20/14 at 9:06 am to knuckleballer
quote:
. That's why kudzu was introduced to slow the erosion down.
My hometown is Vicksburg, that shite is everywhere. I thought it was a normal thing until I learned it wasn't lol
Popular
Back to top
Follow TigerDroppings for LSU Football News