Bear Pond (Hancock County, Maine)
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Bear Pond (Hancock County, Maine)
Bear Pond is a lake in Hancock County, Maine, United States. It is located less than west of the Washington County border, approximately southeast of the summit of Lead Mountain, and northwest of Maine State Route 9 near the town of Beddington Beddington is a suburban settlement in the London Borough of Sutton on the boundary with the London Borough of Croydon. Beddington is formed from a village of the same name which until early the 20th century still included land which became t .... The inflow to Bear Pond comes primarily from Bear Brook, which drains the southeastern slopes of Lead Mountain, which comprises primarily the Bear Brook Watershed in Maine (BBWM), an experimental forest. There are two USGS stream gauges on the East and West Branches of Bear Brook. An unpaved road provides access to the BBWM from state route 9 and passes about from the eastern end of the pond. Bear Pond is surrounded by forest and is drained at its western end by the Little Narraguag ...
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Hancock County, Maine
Hancock County is a county located in the U.S. state of Maine. As of the 2020 census, the population was 55,478. Its county seat is Ellsworth. The county was incorporated on June 25, 1789, and named for John Hancock, the first governor of the Commonwealth of Massachusetts. Geography According to the U.S. Census Bureau, the county has a total area of , of which is land and (32%) is water. The county high point is Cadillac Mountain, 1527 feet, the highest summit on the U.S. Atlantic seaboard. Adjacent counties * Penobscot County — north * Washington County — northeast *Waldo County — west * Knox County — southwest Demographics 2000 census As of the census of 2000, there were 51,791 people, 21,864 households, and 14,233 families living in the county. The population density was 33 people per square mile (13/km2). There were 33,945 housing units at an average density of 21 per square mile (8/km2). The racial makeup of the county was 97.61% White, 0.25% Bla ...
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Maine
Maine () is a state in the New England and Northeastern regions of the United States. It borders New Hampshire to the west, the Gulf of Maine to the southeast, and the Canadian provinces of New Brunswick and Quebec to the northeast and northwest, respectively. The largest state by total area in New England, Maine is the 12th-smallest by area, the 9th-least populous, the 13th-least densely populated, and the most rural of the 50 U.S. states. It is also the northeasternmost among the contiguous United States, the northernmost state east of the Great Lakes, the only state whose name consists of a single syllable, and the only state to border exactly one other U.S. state. Approximately half the area of Maine lies on each side of the 45th parallel north in latitude. The most populous city in Maine is Portland, while its capital is Augusta. Maine has traditionally been known for its jagged, rocky Atlantic Ocean and bayshore coastlines; smoothly contoured mountains; heavily f ...
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United States
The United States of America (U.S.A. or USA), commonly known as the United States (U.S. or US) or America, is a country primarily located in North America. It consists of 50 states, a federal district, five major unincorporated territories, nine Minor Outlying Islands, and 326 Indian reservations. The United States is also in free association with three Pacific Island sovereign states: the Federated States of Micronesia, the Marshall Islands, and the Republic of Palau. It is the world's third-largest country by both land and total area. It shares land borders with Canada to its north and with Mexico to its south and has maritime borders with the Bahamas, Cuba, Russia, and other nations. With a population of over 333 million, it is the most populous country in the Americas and the third most populous in the world. The national capital of the United States is Washington, D.C. and its most populous city and principal financial center is New York City. Paleo-Americ ...
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Glacial Lake
A glacial lake is a body of water with origins from glacier activity. They are formed when a glacier erodes the land and then melts, filling the depression created by the glacier. Formation Near the end of the last glacial period, roughly 10,000 years ago, glaciers began to retreat. A retreating glacier often left behind large deposits of ice in hollows between drumlins or hills. As the ice age ended, these melted to create lakes. This is apparent in the Lake District in Northwestern England where post-glacial sediments are normally between 4 and 6 metres deep. These lakes are often surrounded by drumlins, along with other evidence of the glacier such as moraines, eskers and erosional features such as striations and chatter marks. These lakes are clearly visible in aerial photos of landforms in regions that were glaciated during the last ice age. The formation and characteristics of glacial lakes vary between location and can be classified into glacial erosion lake, ice-bloc ...
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Little Narraguagus River
The Little Narraguagus River is a short stream in Maine. From the outflow of Bear Pond () in Maine Township 28, MD, Hancock County, the river runs U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map, accessed June 22, 2011 southeast and east to its confluence with the Narraguagus River in Beddington, Washington County. See also *List of rivers of Maine A ''list'' is any set of items in a row. List or lists may also refer to: People * List (surname) Organizations * List College, an undergraduate division of the Jewish Theological Seminary of America * SC Germania List, German rugby union ... References *Maine Streamflow Data from the USGSMaine Watershed Data From Environmental Protection Agency

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Narraguagus River
The Narraguagus River is a river located in the U.S. state of Maine with its mouth in the Narraguagus Bay of the Gulf of Maine. It flows through the town of Cherryfield, Maine, Cherryfield and was formerly well known for its sport fly fishing for Atlantic salmon. This was a traditional highlight of late spring with anglers gathering from afar for the Memorial Day weekend fishing kick-off. The native salmon run has been much reduced due to many different factors. From the outlet of Eagle Lake () in Maine Township 34 MD, Hancock County, Maine, Hancock County, the river runs U.S. Geological Survey. National Hydrography Dataset high-resolution flowline dataThe National Map accessed June 22, 2011 southeast to its mouth in Milbridge, Maine, Milbridge, Washington County, Maine, Washington County. During its course, the river passes Lead Mountain (Maine), Lead Mountain before flowing into and out of Beddington Lake. See also * List of Maine rivers References

Rivers ...
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Washington County, Maine
Washington County is a county located in the U.S. state of Maine. As of the 2010 census, its population was 31,095, making it the third-least populous county in Maine. Its county seat is Machias. The county was established on June 25, 1789. It borders the Canadian province of New Brunswick. It is sometimes referred to as "Sunrise County" because it includes the easternmost point in the 48 contiguous United States. Claims have been made that Washington County is where the sun first rises on the 48 contiguous states. Many small seaside communities have small-scale fishing-based economies. Tourism is also important along the county's shoreline, but it is not as important as elsewhere in the state. The blueberry crop plays a major role in the county's economy. Geography According to the U.S. Census Bureau, the county has a total area of , of which is land and (21%) is water. Adjacent counties * Hancock County – southwest * Aroostook County – northwest * Penobscot Co ...
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Lead Mountain (Maine)
Lead Mountain, at high is a peak in eastern Maine. Lead Mountain is located north of the town of Beddington on the border of Hancock and Washington counties in Downeast Maine. The isolation of Lead Mountain is 35.73 miles, and it is easily visible from miles away along Maine state routes 9 and 193 The southern slopes of Lead Mountain are the location of the Bear Brook Watershed in Maine, a long-term research site dedicated to studying the effects of acid deposition on a landscape. Likewise, the southeast slopes of the mountain are drained by Bear Brook. The bedrock of the area contains small blebs of pyrrhotite, which may be mistaken for lead. Lead Mountain is located on private land, but can be hiked by the public. The primary route to Lead Mountain begins just north of the at the gated end of a dirt road southeast of the peak. The route follows the dirt road beyond the gate before turning up a path that ascends southeast of the summit before continuing up the east side of ...
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Maine State Route 9
State Route 9 (SR 9) is a numbered state highway in Maine, running from the New Hampshire border at Berwick in the west to the Canada–US border with New Brunswick at Calais in the east. SR 9 runs a total of . Route description State Route 9 is a meandering highway that works its way from New Hampshire to Canada. It frequently runs concurrent with other highways listed below and also frequently changes direction. For instance, in Kennebunk, State Route 9 travels in a westerly direction even though it is signed as eastbound. State Route 9 runs through most of Maine's major cities including Biddeford, Saco, South Portland, Portland, Augusta, and Bangor. Over the years, a number of improvements have been made by the Route 9 Committee, a partnership of local government officials and business interests in the Baileyville-Calais area. The Airline The leg from Bangor to Calais is often referred to as "The Airline" commonly thought to be due to its shorter route than ...
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Beddington, Maine
Beddington is a town in Washington County, Maine, United States. The population was 60 at the 2020 census. It is the third-smallest organized town in Maine after Frye Island and Frenchboro. Salmon migrate upstream to spawn in the town's rivers and lakes, which are part of their migration route. The majority of the town consists of blueberry fields. Geography According to the United States Census Bureau, the town has a total area of , of which, of it is land and is water. Lead Mountain is located north of the town. Demographics 2010 census As of the census of 2010, there were 50 people, 28 households, and 15 families living in the town. The population density was . There were 321 housing units at an average density of . The racial makeup of the town was 94.0% White, 2.0% Asian, and 4.0% from other races. There were 28 households, of which 10.7% had children under the age of 18 living with them, 50.0% were married couples living together, 3.6% had a female householder ...
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Bear Brook Watershed In Maine
The Bear Brook Watershed in Maine (BBWM) is an experimental forest operated by the University of Maine in Hancock County, Maine, United States. The BBWM focuses around the two small first order branches of Bear Brook on the southeastern slopes of Lead Mountain above Bear Pond. Two years of monitoring studies began in 1987, after which the two watersheds of East and West Bear Brook were determined to be nearly identical. The West Bear Brook watershed was experimentally acidified with ammonium sulfate every other month from November 1989 until August 2016 to study the effects of sulfur and nitrogen acid deposition. East Bear Brook has been used as an untreated reference. Related research topics at BBWM include climate change, carbon sequestration Carbon sequestration is the process of storing carbon in a carbon pool. Carbon dioxide () is naturally captured from the atmosphere through biological, chemical, and physical processes. These changes can be accelerated through cha ...
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Lakes Of Hancock County, Maine
A lake is an area filled with water, localized in a basin, surrounded by land, and distinct from any river or other outlet that serves to feed or drain the lake. Lakes lie on land and are not part of the ocean, although, like the much larger oceans, they do form part of the Earth's water cycle. Lakes are distinct from lagoons, which are generally coastal parts of the ocean. Lakes are typically larger and deeper than ponds, which also lie on land, though there are no official or scientific definitions. Lakes can be contrasted with rivers or streams, which usually flow in a channel on land. Most lakes are fed and drained by rivers and streams. Natural lakes are generally found in mountainous areas, rift zones, and areas with ongoing glaciation. Other lakes are found in endorheic basins or along the courses of mature rivers, where a river channel has widened into a basin. Some parts of the world have many lakes formed by the chaotic drainage patterns left over from the last ...
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