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Vermont dating laws

The Green Mountain range forms a north–south spine running most of the length of the state, slightly west of its center.In the southwest portion of the state are the Taconic Mountains; the Granitic Mountains are in the northeast.

Its greatest width, from east to west, is 89 miles (143 km) at the Canada–U. border; the narrowest width is 37 miles (60 km) at the Massachusetts line. The state's geographic center is approximately three miles (5 km) east of Roxbury, in Washington County. The origin of the name "Vermont" is uncertain, but likely comes from the French les Verts Monts, meaning "the Green Mountains".The rural northeastern section known as the "Northeast Kingdom" often averages 10 °F (5.6 °C) colder than the southern areas of the state during winter.The annual snowfall averages between 60 and 100 inches (1,500 and 2,500 mm) depending on elevation.By the mid-19th century, wild turkeys were exterminated in the state through overhunting and destruction of habitat.Sixteen were re-introduced in 1969 and had grown to an estimated flock of 45,000 in 2009.Although these towns are large enough to be considered cities, they are not incorporated as such.Vermont has a humid continental climate, with muddy springs, in general a mild early summer, hot Augusts; it has colorful autumns: Vermont's hills reveal red, orange, and (on sugar maples) gold foliage as cold weather approaches.The remains of the Chazy Formation can be observed in Isle La Motte. It is the site of the limestone Fisk Quarry, which contains a collection of ancient marine fossils such as stromatoporoids that date back to years ago.It is believed that at one point, Vermont was connected to Africa (Pangaea) and the fossils found and the rock formations found on the coasts in both Africa and America are further evidence of the Pangaea theory.As a result of tectonic formation, Vermont east of the Green Mountains tends to be formed from rocks produced in the Silurian and Devonian periods.Western Vermont mainly from the older Pre-Cambrian and Cambrian material.

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