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Bath, New Hampshire
Bath is a town in Grafton County, New Hampshire, United States. The population was 1,077 at the 2020 census, unchanged from the 2010 census. Now a tourist destination and commuter town for Littleton, the town is noted for its historic architecture, including the Brick Store and three covered bridges. Bath includes the village of Swiftwater and part of the district known as Mountain Lakes. History The town was granted to the Rev. Andrew Gardner and 61 others on September 10, 1761, by Governor Benning Wentworth, who named it for William Pulteney, 1st Earl of Bath. It was first settled in 1765 by John Herriman from Haverhill, Massachusetts. But the terms of the original grant were unfulfilled, so Bath was regranted on March 29, 1769, by Governor John Wentworth. The first census, taken in 1790, recorded 493 residents. Situated at the head of navigation on the Connecticut River, and shielded from strong winds by the Green Mountains to the west and White Mountains to the east, Ba ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Brick Store (Bath, New Hampshire)
The Brick Store, at 21 Lisbon Road in Bath, New Hampshire, claims to be the oldest continuously operating general store in the United States. History The initial construction date of this brick two-story structure is uncertain, and was claimed to be 1804 by a 1937 reference work. Its predominantly Federal styling supports a date in this timeframe. It is known through other documentation to have been standing in 1814, and was damaged by fire in 1824. Repairs at that time probably included the addition of Greek Revival elements to the building's exterior. Although numerous Federal-style brick buildings were built in Bath, this is the only commercial one to survive. The building was added to the National Register of Historic Places in 1985. Located on the Ammonoosuc River, the store is one of the most well-known landmarks of northern New Hampshire. Not only does it sell groceries, gas, and beer, at one time it was a place where customers could drop off UPS packages and dry-cleanin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Covered Bridge
A covered bridge is a timber-truss bridge with a roof, decking, and siding, which in most covered bridges create an almost complete enclosure. The purpose of the covering is to protect the wooden structural members from the weather. Uncovered wooden bridges typically have a lifespan of only 20 years because of the effects of rain and sun, but a covered bridge could last over 100 years. In the United States, only about 1 in 10 survived the 20th century. The relatively small number of surviving bridges is due to deliberate replacement, neglect, and the high cost of restoration. European and North American truss bridges Typically, covered bridges are structures with longitudinal timber-trusses which form the bridge's backbone. Some were built as railway bridges, using very heavy timbers and doubled up lattice work. In Canada and the U.S., numerous timber covered bridges were built in the late 1700s to the late 1800s, reminiscent of earlier designs in Germany and Switzerland. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Wild Ammonoosuc River
The Wild Ammonoosuc River is a tributary of the Ammonoosuc River, about long, in northwestern New Hampshire in the United States. Via the Ammonoosuc River, it is part of the watershed of the Connecticut River, which flows to Long Island Sound. The Wild Ammonoosuc flows for its entire length in Grafton County. It rises in the White Mountains at Kinsman Notch in the town of Woodstock and flows generally northwestwardly through the towns of Easton and Landaff to Bath, where it joins the Ammonoosuc.DeLorme (1999). ''New Hampshire Atlas & Gazetteer''. Yarmouth, Maine: DeLorme. New Hampshire Route 112 follows the river for its entire length. See also *List of New Hampshire rivers This is a list of rivers and significant streams in the U.S. state of New Hampshire. All watercourses named "River" (freshwater or tidal) are listed here, as well as other streams which are either subject to thNew Hampshire Comprehensive Shoreland ... References * Rivers of New Hampshire Ri ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ammonoosuc River
The Ammonoosuc River is a river in northwestern New Hampshire in the United States. It is a tributary of the Connecticut River, which flows to Long Island Sound. ''Ammonoosuc'' is Abnaki for "small, narrow fishing place". The Ammonoosuc rises on the western slope of Mount Washington, in Sargent's Purchase in the White Mountains of southern Coos County. One branch of the river is the outlet of the Lakes of the Clouds in the saddle between Mount Washington and Mount Monroe. Leaving the vicinity of the Presidential Range, the river flows westwardly into Grafton County, where it turns southwestwardly. Along its course the Ammonoosuc passes through Chandler's Purchase, Bean's Grant, and Crawford's Purchase; and the towns of Carroll, Bethlehem, Littleton, Lisbon, Landaff, Bath, and Haverhill to the village of Woodsville, where it flows into the Connecticut River. It collects the Gale River in Lisbon, and the Wild Ammonoosuc River in Bath. DeLorme (1999). ''New Hamp ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alluvial Plain
An alluvial plain is a largely flat landform created by the deposition of sediment over a long period of time by one or more rivers coming from highland regions, from which alluvial soil forms. A floodplain is part of the process, being the smaller area over which the rivers flood at a particular period of time, whereas the alluvial plain is the larger area representing the region over which the floodplains have shifted over geological time. As the highlands erode due to weathering and water flow, the sediment from the hills is transported to the lower plain. Various creeks will carry the water further to a river, lake, bay, or ocean. As the sediments are deposited during flood conditions in the floodplain of a creek, the elevation of the floodplain will be raised. As this reduces the channel floodwater capacity, the creek will, over time, seek new, lower paths, forming a meander (a curving sinuous path). The leftover higher locations, typically natural levees at the margins ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
White Mountains (New Hampshire)
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 part of the northern Appalachian Mountains and the most rugged mountains in New England. The range is heavily visited due to its proximity to Boston, New York City, and Montreal. Most of the area is public land, including the White Mountain National Forest and a number of state parks. Its most famous mountain is Mount Washington, which is the highest peak in the Northeastern U.S. and for 76 years held the record for fastest surface wind gust in the world ( in 1934). Mount Washington is part of a line of summits, the Presidential Range, that are named after U.S. presidents and other prominent Americans. The White Mountains also include the Franconia Range, Sandwich Range, Carter-Moriah Range and Kinsman Range in New Hampshire, and the Mahoosuc Range straddling the border between it and Maine. In all, there are 48 peak ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Green Mountains
The Green Mountains are a mountain range in the U.S. state of Vermont. The range runs primarily south to north and extends approximately from the border with Massachusetts to the border with Quebec, Canada. The part of the same range that is in Massachusetts and Connecticut is known as The Berkshires or the Berkshire Hills (with the Connecticut portion, mostly in Litchfield County, locally called the Northwest Hills or Litchfield Hills) and the Quebec portion is called the Sutton Mountains, or ' in French. All mountains in Vermont are often referred to as the "Green Mountains". However, other ranges within Vermont, including the Taconic Mountains in southwestern Vermont and the Northeastern Highlands, are not geologically part of the Green Mountains. Peaks The best-known mountains—for reasons such as high elevation, ease of public access by road or trail (especially the Long Trail and Appalachian Trail), or with ski resorts or towns nearby—in the range include: # Mount ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Connecticut River
The Connecticut River is the longest river in the New England region of the United States, flowing roughly southward for through four states. It rises 300 yards (270 m) south of the U.S. border with Quebec, Canada, and discharges at Long Island Sound. Its watershed encompasses , covering parts of five U.S. states and one Canadian province, via 148 tributaries, 38 of which are major rivers. It produces 70% of Long Island Sound's fresh water, discharging at per second. The Connecticut River Valley is home to some of the northeastern United States' most productive farmland, as well as the Hartford–Springfield Knowledge Corridor, a metropolitan region of approximately two million people surrounding Springfield, Massachusetts, and Hartford, Connecticut. History The word "Connecticut" is a corruption of the Mohegan word ''quinetucket'', which means "beside the long, tidal river". The word came into English during the early 1600s to name the river, which was also called simply "Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Head Of Navigation
The head of navigation is the farthest point above the mouth of a river that can be navigated by ships. Determining the head of navigation can be subjective on many streams, as the point may vary greatly with the size or the draft of the ship being contemplated for navigation and the seasonal water level. On others, it is quite objective, being caused by a waterfall, a low bridge that is not a drawbridge, or a dam without navigation locks. Several rivers in a region may have their heads of navigation along a line called the fall line. Longer rivers such as the River Thames may have several heads of navigation depending on boat size. In the case of the Thames, that includes London Bridge, which historically served as the head of navigation for tall ships; Osney Bridge in Oxford, which has the lowest headroom of any bridge on the Thames that generally restricts navigation to smaller vessels such as narrowboats and cabin cruisers, and the long reach above St John's Lock, the first ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sir John Wentworth, 1st Baronet
Sir John Wentworth, 1st Baronet (9 August 1737 – 8 April 1820) was the British colonial governor of New Hampshire at the time of the American Revolution. He was later also Lieutenant-Governor of Nova Scotia. He is buried in the crypt of St. Paul's Church in Halifax. Early years Wentworth was born in Portsmouth, New Hampshire, on August 9, 1737. His ancestry went back to some of the earliest settlers of the Province of New Hampshire, and he was a grandson of John Wentworth, who served as the province's lieutenant governor in the 1720s, a nephew to Governor Benning Wentworth, and a descendant of "Elder" William Wentworth. His father Mark was a major landowner and merchant in the province, and his mother, Elizabeth Rindge Wentworth, was also from the upper echelons of New Hampshire society. In 1751, he enrolled in Harvard College, receiving a bachelor's degree in 1755 and a master's degree in 1758. During his time at Harvard, he was a classmate and became a close friend ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Haverhill, Massachusetts
Haverhill ( ) is a city in Essex County, Massachusetts, United States. Haverhill is located 35 miles north of Boston on the New Hampshire border and about 17 miles from the Atlantic Ocean. The population was 67,787 at the 2020 United States Census. Located on the Merrimack River, Haverhill began as a farming community of Puritans, largely from Newbury Plantation. The land was officially purchased from the Pentuckets on November 15, 1642 (One year after incorporation) for three pounds, and ten shillings. Pentucket was renamed Haverhill (after the Ward family's hometown in England) and evolved into an important industrial center, beginning with sawmills and gristmills run by water power. In the 18th and 19th century, Haverhill developed woolen mills, tanneries, shipping and shipbuilding. The town was home to a significant shoe-making industry for many decades. By the end of 1913, one tenth of the shoes produced in the United States were made in Haverhill, and because of this the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
William Pulteney, 1st Earl Of Bath
William Pulteney, 1st Earl of Bath, (22 March 16847 July 1764) was a British Whig politician who sat in the House of Commons from 1707 to 1742, when he was created the first Earl of Bath by King George II. Bath is sometimes stated to have been First Lord of the Treasury and British prime minister, for the shortest term ever (two days) in 1746, although most modern sources do not consider him to have held the office. Background and early career The son of William Pulteney by his first wife, Mary Floyd, he was born in March 1684 into an old Leicestershire family. He was educated at Westminster School and at Christ Church, Oxford, matriculating on 31 October 1700. He acquired extensive classical knowledge, and on leaving Oxford made the usual tour on the continent. In 1705, he was brought into parliament by Henry Guy (former secretary of the Treasury) for the Yorkshire borough of Hedon. This seat was held by him without a break until 1734. Throughout the reign of Queen Anne ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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