Definition of Seneca Buffalo Creek: A Tributary to Lake Erie in New York State and its Surrounding Ecosystem.
Overview and Definition
Seneca Buffalo Creek is a significant tributary located in Western New York, specifically in the County of Erie. The creek originates from an extensive drainage area that includes parts of Orchard Park, Elma, Cheektowaga, Depew, Lancaster, Alden, and East Aurora. Its waters eventually flow into the Buffalo River, which then empties into Lake Erie, one of the five Great https://senecabuffalocreekcasino.ca/ Lakes.
Geological Formation
Seneca Buffalo Creek’s watershed spans approximately 40 square miles, with elevations ranging from about 850 feet above sea level in the north to around 560 feet in the south. The creek and its surrounding landscape were shaped by glacial activity during the Pleistocene era. Moraines deposited by retreating glaciers formed many of the hills and valleys within the watershed.
Hydrology
The Seneca Buffalo Creek Watershed is drained primarily through a combination of groundwater seepage, stream flow, and stormwater runoff. The creek’s hydrological cycle involves the natural interaction between precipitation, evapotranspiration, infiltration, and surface water flow. The main tributaries to Seneca Buffalo Creek include Cazenovia Creek, Black Rock Canal, Scajaquada Creek, and Pinehurst Branch.
Water Quality
Like many urban streams in developed areas, Seneca Buffalo Creek has experienced degradation of its water quality over the years due to human activities such as pollution from industrial and domestic sources. Water samples taken within the creek show elevated levels of Total Phosphorus (TP), Total Kjeldahl Nitrogen (TKN), Dissolved Oxygen (DO), BOD (Biochemical Oxygen Demand) and coliform bacteria counts above regulatory standards.
Biodiversity
Despite the negative impacts on water quality, Seneca Buffalo Creek still hosts a diverse array of plant and animal life. A variety of fish species such as Panfish, Trout, and Salmonid have been detected in the creek’s waters. Invasive species like Phragmites (Phragmites australis), Garlic Mustard, Japanese Stiltgrass, Eurasian Watermilfoil (Myriophyllum spicatum) and Zebra Mussels are also present.
Conservation Efforts
Recent attempts to restore water quality in the creek include installing stormwater management systems to capture excess runoff from nearby streets. This helps reduce pollution by slowing down stormflow peak rates which may otherwise cause flash flooding events within low-lying areas surrounding residential developments along Seneca Buffalo Creek’s banks.
Human Interaction with the Ecosystem
Throughout history, human settlements near the Seneca Buffalo Creek area date back thousands of years with evidence pointing to indigenous peoples’ presence in this region prior to European settlement. In present times, residents and business owners within the watershed rely heavily on its resources for recreation purposes such as fishing, hiking and kayaking; although many acknowledge concerns over potential risks associated with these uses when considering waterborne pollutants like bacterial contamination.
Impact of Climate Change
Projected climate change impacts will further affect Seneca Buffalo Creek by altering local weather patterns and subsequent effects on the creek’s hydrology. Rising temperatures during summer months could lead to more frequent and severe droughts or floods due to altered precipitation regimes affecting stormwater runoff rates within its catchment area.
The watershed’s aquatic life faces significant threats as warmer waters favor growth of invasive plant species such as Phragmites and facilitate proliferation of zebra mussels which block natural spawning habitats for native fish populations.