Ossipee MountainsThe Ossipee Mountains are a small mountain range in the New England state of New Hampshire, United States. The remains of an ancient volcanic ring dike, they lie north of Lake Winnipesaukee, east of Squam Lake, and south of the Sandwich Range, the southernmost of the White Mountains. At 2,990 ft (910 m), Mount Shaw is their highest point.
Moultonborough, New HampshireMoultonborough is a town in Carroll County, New Hampshire, United States. The population was 4,918 at the 2020 census, up from 4,044 in 2010. Moultonborough is bounded in large part by Lake Winnipesaukee in the southwest and to a lesser extent by Squam Lake in the northwestern corner. The town includes the census-designated place of Suissevale and the community of Lees Mill.
Carroll County, New HampshireCarroll County is a county in the U.S. state of New Hampshire. As of the 2020 census, the population was 50,107, making it the third-least populous county in New Hampshire. Its county seat is Ossipee. The county was created in 1840 and organized at Ossipee from towns removed from Strafford County. It was named in honor of Charles Carroll of Carrollton, who had died in 1832, the last surviving signer of the United States Declaration of Independence.
New HampshireU.S. stateState in the United StatesNew Hampshire ( ) is a state in the New England region of the Northeastern United States. It borders Massachusetts to the south, Vermont to the west, Maine and the Gulf of Maine to the east, and the Canadian province of Quebec to the north. Of the 50 U.S. states, New Hampshire is the seventh-smallest by land area and the tenth-least populous, with a population of 1,377,529 residents as of the 2020 census.
Ossipee, New HampshireOssipee is a town in Carroll County, New Hampshire, United States. The population was 4,372 at the 2020 census, and an estimated 4,599 in 2025. It is the county seat of Carroll County. Ossipee, which includes several villages, is a resort area and home to part of Pine River State Forest.
Sandwich RangeThe Sandwich Range is located in the White Mountains of New Hampshire in the United States, north of the Lakes Region and south of the Kancamagus Highway. Although the range is not outstanding for its elevation, it is very rugged and has excellent views of the surrounding lakes, mountains, and forests. The Sandwich Range extends east–west about 30 miles (48 km) from Conway, New Hampshire on the Saco River to Campton on the Pemigewasset River.
White Mountains (New England)The White Mountains are a mountain range covering about a quarter of the state of New Hampshire and a small portion of western Maine in the United States. They are a subrange of the northern Appalachian Mountains and the most rugged mountains in New England. Several of the higher peaks contain an Alpine tundra. The range is heavily visited due to its proximity to Boston, New York City, and Montreal.
Tuftonboro, New HampshireTuftonboro is a town in Carroll County, New Hampshire, United States. The population was 2,467 at the 2020 census. Bounded on the southwest by Lake Winnipesaukee, Tuftonboro includes the villages of Tuftonboro Corner, Center Tuftonboro, Melvin Village and Mirror Lake.
MountainA mountain is an elevated portion of the surface of a planet, generally with steep sides that show significant exposed bedrock. Although there are no universally accepted definitions, a mountain is usually considered higher than a hill. By definition, mountains are often thought of as being a landform which is higher than 2,000 feet (610 m). It may either have a limited summit area or be a smaller plateau with high elevation and steep sides.
Topographic prominenceIn topography, prominence (also referred to as autonomous height, and shoulder drop in US English, and drop in British English) is the height of the summit of a mountain or hill relative to the lowest contour line encircling it, but containing no higher summit within it. It is a measure of the independence of a summit. The key col ("saddle") around the peak is a unique point on this lowest contour line.
Ring dikeA ring dike or ring dyke is an intrusive igneous body that is circular, oval or arcuate in plan and has steep contacts. While the widths of ring dikes differ, they can be up to several thousand meters. The most commonly accepted method of ring dike formation is directly related to collapse calderas.
StratovolcanoA stratovolcano, also known as a composite volcano, is a typically conical volcano built up by many alternating layers (strata) of hardened lava and tephra. Unlike shield volcanoes, stratovolcanoes are characterized by a steep profile with a summit crater and explosive eruptions. Some have collapsed summit craters called calderas. The lava flowing from stratovolcanoes typically cools and solidifies before spreading far, due to high viscosity.
CretaceousThe Cretaceous (IPA: krih-TAY-shəss) is a geological period that lasted from about 143.1 to 66 Ma (million years ago). It is the third and final period of the Mesozoic Era, as well as the longest. At around 77.1 million years, it is the ninth and longest geological period of the entire Phanerozoic. The name is derived from the Latin creta, 'chalk', which is abundant in deposits from the latter half of the period.*As an Amazon Associate I earn from qualifying purchases.