As a beginner using
the Web Soil Survey tool was tricky for my study area since Lake Norman is in four
separate counties. Thankfully, the site separated each county, and they were
all included when I ran a report. This made it much easier, so I did not have
to look up each one individually. I suggest a smaller area of study and one on land
so that you can get more information. It is a lot of information (if available) and can easily be overwhelming but it can be a very helpful tool.
FINDINGS:
I
obtained specific data on erosion levels and flooding potential from the Web
Soil Survey tool. In Catawba County, 1 out of 15 areas is severely eroded. In
Iredell County, 13 out of 46 were labeled mildly eroded, and 5 out of the 46 were
labeled under rarely flooded to frequently flooded. Lincoln County had 2 out of
24 as flooded potential and 7 out of the 24 as mildly eroded, and lastly, in Mecklenburg
County, 2 out of 26 were mildly eroded, and 1 out of 26 were frequently
flooded (websoilsurvey.sc.egov.usda.gov, n.d.). The proximity of residential neighborhoods to the shoreline and each
other significantly contributes to the shoreline’s erosion through stormwater
runoff. To combat this, a regulation established in
2001 states a 50-foot buffer zone for all upcoming development, where
vegetation must be preserved to help prevent further erosion and pollution (Lake
Norman, 2024).
LKN SOIL:
"The lake is mainly underlain by interfingered
igneous and
metamorphic bedrock. The bottom of the lake consists of various clay and plastic
soils. These mechanically engineered soils are maintained and
constructed with artificial enforcing, which adds a stabilization
factor, and solidifies the lake so it will not break down and wear away.
Clay soil contains a high percentage of particles that becomes sticky
when wet, and therefore holds together better.
[4]
Lake Norman lies atop two geologic belts, the Charlotte belt and the Inner Piedmont belt.[5]
The Charlotte belt is made up of igneous rock that is 300 to 500
million years old. Igneous rocks are used in construction, hence why the
lake was built on top of them. The Inner Piedmont belt is the most
metamorphosed belt, and contains deformed metamorphosed volcanic and
sedimentary rocks approximately 500 to 700 million years old. The lake
is built on the Catawba River, and is underlain by inceptisol soils,
which are found in river floodplains. The soil is made of brown forest
soil deposits and includes a wide variety of dissimilar soil
characteristics. In North Carolina, inceptisols cover almost the whole
state, except areas around the east coast"
(Lake
Norman, 2024).