Nauset Marsh Trail Footbridge Temporary Closure After Labor Day
A small footbridge on the Nauset Marsh trail will be closed for repair for two weeks following Labor Day. Ask at the visitor center for detour information.
Sections of Boardwalk Closed at Red Maple Swamp Trail
Sections of the boardwalk at the Red Maple Swamp Trail have been closed due to structural deterioration and safety concerns. Check at Salt Pond Visitor Center for the current status of this trail, and for your safety, remain out of closed areas.
Cape Cod National Seashore and the Herring River Restoration Committee Announce Second Public Scoping Meeting
Contact: Carrie Phillips, Chief, Natural Resources Management, 508 349 3785
Cape Cod National Seashore Superintendent George Price and Herring River Restoration Committee Chairman Gary Joseph invite the public to participate in an upcoming meeting to provide input on the Herring River Restoration Project to be held Wednesday, September 24, 2008, from 7 PM to 9:30 PM at the Wellfleet Senior Center. This is the second of two scoping meetings. The first was held August 14, 2008.
The Herring River is the largest estuary on outer Cape Cod. It stretches four miles from its headwater kettle ponds in north Wellfleet to its mouth at Wellfleet Harbor. The river's floodplain encompasses more than 1,100 acres of degraded wetlands occupying a complicated network of five valleys. The Chequessett Neck Road dike, built in 1908, along with smaller dikes, culverts, and ditches upstream have impeded natural tidal flows and effectively drained the normally saturated soil. The once expansive and thriving salt marshes have been transformed into almost impenetrable stands of non-native, invasive plants, shrubby thickets, and forests. The old salt marsh peat, deprived of the tides, has decomposed and compressed, effectively sinking the surface of the floodplain. The decaying peat also releases sulfuric acid which can leach into the river and kill fish and other aquatic life. At times, water in the Herring River is as acidic as vinegar. In addition to high acidity, low summertime dissolved oxygen - also caused by the lack of tidal flushing - makes survival tough for aquatic life.
In 2005, Cape Cod National Seashore and the Town of Wellfleet formed the Herring River Technical Committee to evaluate the feasibility of restoring tidal flows to the Herring River. The Technical Committee's work culminated in a Conceptual Restoration Plan that demonstrated restoration is feasible.
Inspired by the work and findings of the Technical Committee, Cape Cod National Seashore, the Town of Wellfleet, and the Town of Truro have joined with Massachusetts Coastal Zone Management, U.S. Fish and Wildlife Service, the National Oceanographic and Atmospheric Administration, and the Natural Resource Conservation Service to restore tide to the Herring River. Together, these entities have formed the Herring River Restoration Committee to guide to develop an Environmental Impact Statement (EIS) and an Environmental Impact Report (EIR) for restoration of the Herring River.
This public input meeting is the second scoping meeting. Scoping is the first step to involve the public in the environmental impact analysis process. It provides an opportunity to learn about the project and provide input on the issues, information, and alternatives that should be considered during development of an EIS/EIR. Because the EIS/EIR will analyze many complex ecological and social issues, your participation is encouraged and needed.
In addition to oral comment at the public meeting, written comments can be provided electronically at http://parkplanning.nps.gov (select “Cape Cod NS” and follow the link to the Herring River Restoration EIS) or by e-mail to e-mail us. Written comments may also be submitted by mail or hand delivery to Superintendent, Cape Cod National Seashore, 99 Marconi Site Road, Wellfleet, MA 02667.
Did You Know?
Kettle pond surface water levels are controlled by local groundwater levels. Around Cape Cod National Seashore ponds, these levels range from six to nine feet above average sea level. The bottoms of all the kettle ponds are below sea level.