Pinhook Bog is a unique bog in Indiana that has been designated a National Natural Landmark. It is part of the Indiana Dunes National Lakeshore, an area that many citizens, scientists, and politicians fought hard to preserve. Its sister bog, Volo Bog, is located nearby. The bog contains a large variety of plants, including insect eating plants, tamarack trees, stands of blueberry bushes, and floating mats of sphagnum moss. Pinhook Bog is about 580acre, a quarter of which is a floating mat of sphagnum peat moss. A "moat" separates the bog from the uplands.GeologyThe bog is a glacial kettle. At the end of the Wisconsin Glacial epoch about 14,000 to 15,000 years ago, a large chunk of ice remained buried at this location as the ice retreated northward. When the ice melted, the clay soil sealed the basins.The runoff from higher ground around the bog is the only water source. There is no stream or groundwater inflow or outflow. Evaporation from the open water and plants is the only loss of moisture. A bog differs from swamps, marshes, and ponds because of this limited exchange of water. The water in the bog is stagnant, acidic, and nutrient-poor.PlantsThe outstanding feature of Pinhook Bog is the tree-covered mat of sphagnum moss. Sphagnum moss is a stringy, delicate moss of a light-green color. The mat floats on top of the water and can become 3to thick, yet it can have a pocket only a few inches thick in the middle. As the mat thickens, larger and larger plants take root and grow. Under the mat a peat bed develops. The acidic water slows the decay of the sphagnum moss and other plants. With time, the peat may fill the bog from the mat to the bottom. As the moisture becomes less acidic, typical land plants take root and the bog disappears.
