Located in the village of Howard, Wisconsin, the Duck Creek Quarry is a former limestone quarry that operated from 1827 to 2001. After its closure, it was naturally filled by an underground aquifer. The most unique features of this body of water are its steep stone drop-offs and deep blue coloration, caused by the way sunlight interacts with the limestone.
The underwater habitat contains several niches, including muddy and silty bottoms, sandy shorelines, and flat stone floors. With depths reaching up to 170 ft, the water quickly becomes cold just a few feet below the surface. Most biological activity is found along the muddy banks and shallow beds, where dense vegetation grows, including hornwort (Ceratophyllum demersum) and pondweed (Potamogeton spp.).
Along the stone walls, multiple rock shelves create additional habitat complexity. Former water levels exposed these shelves to the air, allowing large trees and bushes to grow on top. Hundreds of fish, including Bluegill (Lepomis macrochirus), school around these submerged tree structures, creating an environment that resembles an underwater reef.
- GPS
- 44.5665474, -88.0665970
- Geographical region
- Northern America
- Drainage Basin
- River catchment
- Water body type
- Artificial reservoir
- Water body name
- Duck Creek Quarry
- Water body part
- Water body course
- Water body: tributary of
- Tributary name





