Eastern Great Lakes and Hudson Lowlands (ecoregion)
The Eastern Great Lakes and Hudson Lowlands region extends along the south shores of Lakes Erie and Ontario and the St. Lawrence River to Lake Champlain, and south down the Hudson River. In the north it meets the Mixedwood Plains Ecozone of Canada. It is mostly deciduous forest and agricultural land. It is one of the 104 Level III ecoregions that occur within the United States, and one of the 35 that comprise the Eastern Temperate Forest Level 1 Ecoregion. This classification system was developed by the United States Environmental Protection Agency.
This region was glaciated during the last ice age, and contains prominent glacial features including till and drumlins, as well as the valleys containing the Finger Lakes. Part of the area was covered by Glacial Lake Iroquois, while regions further to the east were flooded under the Champlain Sea. At one point during the melting of the glaciers, the Great Lakes drained down the Hudson River to the Atlantic Ocean. This area is mostly temperate deciduous forest, dominated by trees including oak, maple, beech and oak. Unlike forests further to the north, southern tree species such as hickory also occur (see Bitternut hickory, Shagbark hickory). Many other plant and animal species reach their northern limits in this ecoregion. A few more examples follow. The wetland plant, Arrow arum (Peltandra virginica) reaches the St. Lawrence River and the Richelieu River. The Bog Turtle (Clemmys muhlenbergii) reaches the southern shores of Lake Ontario, while the Eastern Box Turtle reaches the southern shores of Lake Erie. Along the shores of the lakes and rivers, there are significant areas of wetland, principally marshes and swamps. Some of the many significant natural areas include El Dorado Beach Preserve on Lake Ontario, the Chaumont Barrens alvar grassland, and the Rome Sand Plains.
Large areas of this forest have been cleared for agriculture, particularly dairy farms and row crops. The presence of the Great Lakes moderates the climate, but increases snowfall. Major cities in this region include Cleveland, Buffalo, Rochester, Syracuse and Albany.
There can be some problems with understanding the naming of this ecological region, since the Canadian government has its own classification system of ecozones, which can have different names. In this case, the Mixedwood Plains occur on the Canadian side of the border while the Eastern Great Lakes and Hudson Lowlands occur on the American side. Hence, the Commission for Environmental Cooperation has worked toward giving each ecological region of North America a consistent name. In the CEC system, this ecoregion is named the Eastern Great Lakes and Hudson Lowlands, and is identified as region 8.1.1. In the west it meets ecoregion 8.1.2, the Lake Erie Lowland. In the east it meets 5.3.1, the North Appalachian and Atlantic Maritime Highlands. In northern New York, there are two high altitude areas, one being the Adirondacks, that are colder and so fall within ecoregion 5.3.1. In addition the World Wildlife Fund developed its own classification system, in which much of this region is called the Eastern Great Lakes lowland forests.
- Eyles, N. Ontario Rocks: Three Billion Years of Environmental Change. Fitzhenry & Whiteside, Markham, Ontario. 339 p.
- Marie-Victorin, Frere. 1964, Flore Laurentienne. University of Montreal Press, Montreal. 924 p, p.846
- Harding, James H. 2006. Amphibians and Reptiles of the Great Lakes Region. University of Michigan Press, Ann Arbor. 378 p.
- "Eastern Great Lakes and Hudson Lowlands, Land Cover Trends Project". Retrieved June 26, 2012.
- "North American Environmental Atlas; Terrestrial Ecoregions". Retrieved June 26, 2012.
This relief map shows the lowlands in the centre of this ecoregion, and the Mohawk Valley linking to the Hudson River.