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Category: Bodies of water of Addison County, Vermont. 1 language. ... This page was last edited on 26 June 2017, at 00:35 (UTC).
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Recharge is the primary method through which water enters an aquifer. This process usually occurs in the vadose zone below plant roots and is often expressed as a flux to the water table surface. Groundwater recharge also encompasses water moving away from the water table farther into the saturated zone. [1]
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[2] [3] Roughly 112 miles (180 km) long, it is the primary watercourse running through Rutland County and Addison County. The mouth of the river flows into Lake Champlain . Settled by indigenous peoples at least 10-11,000 years ago, the river was an important economic region for indigenous people before European settlement. [ 4 ]
Lake Dunmore is a freshwater lake in Addison County, Vermont.The lake spans the towns of Salisbury and Leicester and has a surface area of 985 acres (3.98 km 2). [1] Lake Dunmore is over 3 miles long (oriented north-south) and up to 1 mile wide.
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