Putnam County Sinkhole, TN

Central Tennessee’s unique geology makes sinkholes common. The area sits on soluble limestone, a key feature of karst landscapes. Groundwater dissolves these rocks, creating voids that collapse under pressure.

This process shapes the landscape and affects city planning. It’s a big challenge.

Studies show how land use affects geological risks. A 2009 Sinkhole-Floodplain Report looked at 218 major sinkholes. GIS mapping found 45% of the area drains through these sinkholes.

Impervious surfaces like roads and buildings cover 22% of sinkhole watersheds. This shows stormwater management systems are at risk.

Advanced models predict flood risks with great accuracy. LiDAR surveys and 100-year storm simulations show where water will gather. They found 657 acres that could flood.

Over 225 structures and 7.8 miles of roads are at risk. This highlights the need for better infrastructure.

Knowing these risks helps plan safer development. As limestone erodes, finding a balance between growth and geology is key. Using data to plan ahead helps protect property and people.

Recent & Notable Sinkhole Incidents / Case Studies

Putnam County has seen 17 sinkholes from 2003 to now. The 2023 East Spring Street collapse was the worst. It took 11 days to fix the road and affected 42 businesses’ water.

The TDEC found it was due to old stormwater systems and limestone. Trog Sink near Burgess Falls fills up seasonally, making temporary lakes. These lakes support special ecosystems.

The Canal, a half-mile-long, shows underground caves through dye-tracing by Western Kentucky University.

Three examples show how to handle sinkholes differently:

• Window Cliffs State Park: Trails with small sinkholes are safe thanks to strong paths
• England Cove: It has equipment to watch sinkhole movements in a restricted area
• Stone Cove Arches: A gate keeps people away from unstable limestone bridges

The National Speleological Society (NSS) works in 4 sites in the county. They team up with Tennessee Tech University on projects. They use LiDAR and water tests to find risky areas.

Human actions have caused 38% of sinkholes, TDEC says. Bad waste management and building on thin limestone are big problems. Unlike natural karst, these sinkholes happen fast, not over years.

Risk Factors & What Homeowners Should Do

Properties in Putnam County face a higher risk of sinkholes because of karst geology. This is also due to the high concentration of development in flood-prone areas. Over 27% of homes in Cookeville’s city center are in FEMA flood zones.

These areas have lots of hard surfaces like driveways and roofs. These surfaces make more water flow into swallets. Keeping these drainage points clear is key to avoiding sinkholes.

Before making changes to your property, check Putnam County’s GIS floodplain maps. Using debris filters around swallets can cut down sediment buildup. Studies show a 40% drop in erosion incidents with these filters.

Joining Cookeville’s Stormwater Management Program lets you monitor drainage in real-time. It uses data from public and private drainage systems. This helps keep water flowing smoothly.

Landowners must keep swallets on their land in good condition, as per city code 14-307. The city handles issues in public areas. Regular checks before the spring rains start can spot problems early.

Working together with the Putnam County Planning Department helps follow zoning rules. This is important for building near areas prone to sinkholes.

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