The purpose of this study was to evaluate the loss of soil and nutrients from the upland area of ten selected small watersheds or subwatersheds surrounding Conesus Lake. Macrophyte beds of mixed composition exist around the entire edge of Conesus Lake – perimeter beds. In addition, macrophyte beds consisting mainly of Eurasian milfoil exist at or near many of the creek mouths within the littoral zone of Conesus Lake. These creek-mouth associated beds are of interest because their presence may be associated with creeks that lose a large amount of nutrients and soils from their subwatershed
The western basin of Lake Erie, the shallowest of the Laurentian Great Lakes in North America, is no...
ABSTRACT Event sampling programs were conducted at 11 tributary monitoring stations in the Lake Eri...
Here we report on the status of Lake Neatahwanta and losses of materials and nutrients from the vari...
The State of Conesus Lake: Watershed Characterization Report (2001) identified areas that required a...
A program of research was developed at the State University of New York at Brockport\u27s Department...
The rivulets that drain small subwatersheds of Canandaigua Lake contributed significant amounts of t...
Stress stream analysis of two sub-watersheds of Conesus Lake. July 1993. Prepared for the Livingston...
Conesus Lake is fed by 18 tributaries and a number of smaller streams and rivulets (Forest et al. 19...
Stress stream analysis of a sub-watershed of Conesus Lake. July 1994. Prepared for the Livingston Co...
Mitigation of soil and nutrient loss from the landscape continues to be a concern within watersheds ...
A goal of this project is to demonstrate the effectiveness of various agricultural management plans ...
Thousands rely on the water of Canandaigua Lake for drinking water, fishing, boating and swimming ea...
Conesus Lake, considered a eutrophic lake in the late 1960s (Mills, 1975) and one of the smaller of ...
In response to public concern created by an abundance of nuisance weeds (i.e. macrophytes) within th...
During the summers of 2000, 2001 and 2002, the littoral zone of Conesus Lake (40°54\u27N, 77°43\u27W...
The western basin of Lake Erie, the shallowest of the Laurentian Great Lakes in North America, is no...
ABSTRACT Event sampling programs were conducted at 11 tributary monitoring stations in the Lake Eri...
Here we report on the status of Lake Neatahwanta and losses of materials and nutrients from the vari...
The State of Conesus Lake: Watershed Characterization Report (2001) identified areas that required a...
A program of research was developed at the State University of New York at Brockport\u27s Department...
The rivulets that drain small subwatersheds of Canandaigua Lake contributed significant amounts of t...
Stress stream analysis of two sub-watersheds of Conesus Lake. July 1993. Prepared for the Livingston...
Conesus Lake is fed by 18 tributaries and a number of smaller streams and rivulets (Forest et al. 19...
Stress stream analysis of a sub-watershed of Conesus Lake. July 1994. Prepared for the Livingston Co...
Mitigation of soil and nutrient loss from the landscape continues to be a concern within watersheds ...
A goal of this project is to demonstrate the effectiveness of various agricultural management plans ...
Thousands rely on the water of Canandaigua Lake for drinking water, fishing, boating and swimming ea...
Conesus Lake, considered a eutrophic lake in the late 1960s (Mills, 1975) and one of the smaller of ...
In response to public concern created by an abundance of nuisance weeds (i.e. macrophytes) within th...
During the summers of 2000, 2001 and 2002, the littoral zone of Conesus Lake (40°54\u27N, 77°43\u27W...
The western basin of Lake Erie, the shallowest of the Laurentian Great Lakes in North America, is no...
ABSTRACT Event sampling programs were conducted at 11 tributary monitoring stations in the Lake Eri...
Here we report on the status of Lake Neatahwanta and losses of materials and nutrients from the vari...
