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Vermont geography

Vermont is located in the New England region
in the eastern United States and comprisesSeveral mountains have timberlines: Mount
9,614 square miles (24,902 km2), making itMansfield, the highest mountain in the state,
the 45th largest state. Of this, landas well as Killington are examples. About 77
comprises 9,250 square miles (23,955 km2) andpercent of the state is covered by forest;
water comprises 365 square miles (948 km2),the rest is covered in meadow, uplands,
making it the 43rd largest in land area andlakes,  ponds  and  swampy  wetlands.
the  47th  in  water  area.
Areas in Vermont administered by the National
The west bank of the Connecticut River marksPark Service include the Appalachian National
the eastern border of the state with NewScenic Trail and the
Hampshire (the river itself is part of NewMarsh-Billings-Rockefeller National
Hampshire). Lake Champlain, the major lake inHistorical  Park  in  Woodstock.
Vermont, is the sixth-largest body of fresh
water in the United States and separatesClimate
Vermont from New York in the northwest
portion of the state. From north to south,Vermont has a humid continental climate
Vermont is 159 miles (256 km). Its greatest(Koppen climate classification Dfb), with
width, from east to west, is 89 miles (143warm, humid summers and cold winters, which
km) at the Canadian border; the narrowestbecome colder at higher elevations. Vermont
width is 37 miles (60 km) at theis known for its mud season in spring
Massachusetts line. The state's geographicfollowed by a generally mild summer and a
center is Washington, three miles (5 km) eastcolorful autumn, and particularly for its
of  Roxbury.cold winters. The northern part of the state,
including the rural northeastern section
There are six distinct physiographic regions(dubbed the "Northeast Kingdom") is known for
of Vermont. Categorized by geological andexceptionally cold winters, often averaging
physical attributes, they are the10 °F (6 °C) colder than the southern
Northeastern Highlands, the Green Mountains,areas of the state. Annual snowfall averages
the Taconic Mountains, the Champlainbetween 60 to 100 inches (150–250 cm)
Lowlands, the Valley of Vermont and thedepending on elevation, giving Vermont some
Vermont  Piedmont.of New England's best cross-country and
downhill  ski  areas.
The origin of the name Green Mountains
(French: Verts monts) is uncertain. SomeIn the autumn, Vermont's hills experience an
authorities say that they are so namedexplosion of red, orange and gold foliage
because they have much more forestation thandisplayed on the sugar maple as cold weather
the higher White Mountains of New Hampshireapproaches. This famous display of color that
and Adirondacks of New York. Otheroccurs so abundantly in Vermont is not due so
authorities say that they are so namedmuch to the presence of a particular variant
because of the predominance ofof the sugar maple; rather it is caused by a
mica-quartz-chlorite schist, a green-huednumber of soil and climate conditions unique
metamorphosed shale. The range forms ato  the  area.
north-south spine running most of the length
of the state, slightly west of its center. InThe highest-recorded temperature was 105
the southwest portion of the state are the°F (41 °C), at Vernon on July 4, 1911;
Taconic Mountains; the Granitic Mountains arethe lowest-recorded temperature was -50 °F
in the northeast. In the northwest near Lake(-46 °C), at Bloomfield on December 30,
Champlain is the fertile Champlain Valley. In1933.
the  south  of  the  valley is Lake Bomoseen.



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