Geology of New Hampshire
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The geology of New Hampshire is similar to that of the rest of New England in comprising a series of metamorphosed sedimentary and volcanic rocks of Late Proterozoic to Devonian age, intruded by many plutons and dikes ranging in age from Late Proterozoic to early Cretaceous. New Hampshire is known as "the Granite State", but less than half is underlain by granite; much of it is schist or gneiss, both of which are metamorphic rocks.[1]
The state straddles three composite tectonostratigraphic terranes. The larger part of the state lies on the Central Maine composite terrane, comprising the Central Maine trough in the east and the Bronson Hill mantled gneiss domes in the west. A small area of the first composite terrane belongs to the Hurricane Mountain belt and olistostrome belt. The northernmost corner of the state lies in the Connecticut Valley trough of the Boundary Mountains composite terrane. In the coastal region in the southeast is the Merrimack–Orrington Belt of the Nashoba–Casco–Miramichi composite terrane.[2]
Geography
The state is bounded by Quebec, Canada, to the north and northwest; Maine and the Atlantic Ocean to the east; Massachusetts to the south; and Vermont to the west. New Hampshire's major regions are the Great North Woods, the White Mountains, the Lakes Region, the Seacoast, the Merrimack Valley, the Monadnock Region, and the Dartmouth-Lake Sunapee area. New Hampshire has the shortest ocean coastline of any U.S. coastal state, with a length of 18 miles (29 km),[3] sometimes measured as only 13 miles (21 km).[4] New Hampshire was home to the rock formation called the Old Man of the Mountain, a face-like profile in Franconia Notch, until the formation disintegrated in May 2003.
The White Mountains in New Hampshire span the north-central portion of the state, with the summit of Mount Washington the highest point in the northeastern United States.

In the southwest corner of New Hampshire, the landmark Mount Monadnock has given its name to a class of earth-forms – a monadnock – signifying, in geomorphology, any isolated resistant peak rising from a less resistant eroded plain.
Major rivers include the 110-mile (177 km) Merrimack River, which bisects the lower half of the state north-south and reaches the Atlantic Ocean in Newburyport, Massachusetts. Its New Hampshire tributaries include the Contoocook River, Pemigewasset River, and Winnipesaukee River. The 410-mile (660 km) Connecticut River, which starts at New Hampshire's Connecticut Lakes and flows south to Connecticut, defines the western border with Vermont. The state border is not in the center of that river, as is usually the case, but at the low-water mark on the Vermont side; meaning that the entire river along the Vermont border (save for areas where the water level has been raised by a dam) lies within New Hampshire.[5] Only one town – Pittsburg – shares a land border with the state of Vermont. The "northwesternmost headwaters" of the Connecticut, now known as Halls Stream, define Canada's border with New Hampshire.
The Piscataqua River forms the state's only significant ocean port where it flows into the Atlantic at Portsmouth. The Salmon Falls River and the Piscataqua define the southern portion of the border with Maine. The largest of New Hampshire's lakes is Lake Winnipesaukee, which covers 71 square miles (184 km2) in the east-central part of New Hampshire. Umbagog Lake along the Maine border, approximately 12.3 square miles (31.9 km2), is a distant second. Squam Lake is the second largest lake entirely in New Hampshire.
New Hampshire has the shortest ocean coastline of any state in the United States, approximately 18 miles (29 km) long.[6] About 7 miles (11 km) offshore are the Isles of Shoals, nine small islands (four in New Hampshire and five in Maine).