34-779: Passumpsic is a Native American word meaning "clear running water" and may refer to: Geography [ edit ] The Passumpsic River , a tributary of the Connecticut River in Vermont Ships [ edit ] USS Passumpsic (AO-107) , an oiler that served in the United States Navy from 1946 to 1973 before transferring to the Military Sealift Command and becoming USNS Passumpsic (T-AO-107) USNS Passumpsic (T-AO-107) , an oiler that served in
68-491: A household in the town was $ 35,268, and the median income for a family was $ 41,563. Males had a median income of $ 28,977 versus $ 19,509 for females. The per capita income for the town was $ 20,697. About 11.7% of families and 13.9% of the population were below the poverty line , including 18.0% of those under age 18 and 13.8% of those age 65 or over. Burke has the highest per capita income of any place in Caledonia County or
102-531: A mile downstream, it is joined on the south by Flower Brook which flows mainly from the east. Duck Pond drains into it. It is followed by Route 5A and flows through East Burke. It converges with the west branch before 5A joins US Route 5. The West Branch first exits out the west side of Newark Pond in Newark . It flows briefly through Barton , back into Newark, then into Burke . The northeast and northwest sides of Burke Mountain drain into Dish Mill Brook, thence into
136-482: A while, enters from the east. In Lyndon it passes through Folsom Village. Quimby and Calendar brooks enter from the west. The river turns south, near the Calendar Brook Road intersection with Route 5. The two branches merge near East Burke Road, just northeast of where VT 114 intersects with US 5. The joined river continues south. The river turns west, even west-northwest at times. An unnamed brook enters from
170-959: Is different from Wikidata All article disambiguation pages All disambiguation pages Passumpsic River The Passumpsic River ( / p ə ˈ s ʌ m p s ɪ k / ) is a 22.7-mile-long (36.5 km) tributary of the Connecticut River , in Vermont . Though primarily a Caledonia County river, it is the only river to flow through all three counties of the Northeast Kingdom . The river arises in two branches: east and west. The East Branch begins just north of East Haven . It flows southwest through Hartwellville in East Haven, then into East Burke . The West Branch starts as several small forks near Crystal Lake , northeast of Sutton . The Montreal, Maine and Atlantic Railway lines follows
204-489: Is joined by Jack Brook near Howard Brook Road in Newark . It then turns south southwest. Just before entering East Haven , it is joined by Mill Brook/King Brook entering from the east. It is then joined by the confluence of Bean Brook and Whetstone Brook just inside the town of East Haven, back in Essex County. It goes through Hartwellville, in the town of East Haven, then crosses into Caledonia County for good. In Burke ,
238-417: Is land and 0.15 square miles (0.4 km ), or 0.40%, is water. Burke is bordered by the towns of Lyndon and Kirby to the south, Victory to the southeast, East Haven to the northeast, Newark to the north, and Sutton to the west. U.S. Route 5 runs through the western part of the town, connecting Lyndonville to the south with Barton and Newport to the north. Vermont Route 5A leaves US-5 in
272-423: Is on this high terrace which is called "St. Johnsbury Plain". The base of the terraces at St. Johnsbury is composed of clay. The same terrace occurs on both sides of the river valley beyond Lyndon. There are lower terraces at intervals. Lyndonville has a high terrace. This may have once extended across the valley to form the end of a basin. Its lower strata are clayey, and are folded and curved. West of this terrace
306-565: Is small. The count never exceeds five which is unusual. The third basin includes the east branch of the Passumpsic River which runs through the Town of Burke. In East Burke there are several terraces. Near the village there are four on the west side, and two on the east side. Above East Burke the valley rises so that its bottom appears like a terrace. Its steep slope crosses the valley at right angles. There are indistinct terraces on its sides. Since
340-640: The East Branch of the Passumpsic River. The southwest end of Burke Mountain drains into Mountain Brook, thence into the East Branch of the Passumpsic River. The south slopes and southeast side of Burke Mountain drain into Weir Mill Brook, thence into Bog Brook, the Moose River , and the Passumpsic River. It proceeds south-southwest. Arcadia Brook flows into it from the north near Arcadia Lane. West Brook flows into it from
374-550: The Military Sealift Command , was redesignated USNS Passumpsic (T-AO-107) , and continued to serve in support of the U.S. Navy with a civilian crew as a United States Naval Ship until 1991. 44°19′14″N 72°01′56″W / 44.3206158°N 72.0323161°W / 44.3206158; -72.0323161 Burke, Vermont Burke is a town in Caledonia County , Vermont , United States. The population
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#1732851865341408-507: The Northeast Kingdom . Burke Mountain is home to Burke Mountain Resort, a mid-size ski area open to skiing and snowboarding in winter and downhill mountain biking in summer. The Resort includes a hotel with a pool, two restaurants, and an arcade. It is a popular location for weddings and other events. The mountain is also home to Burke Mountain Academy, a premier ski academy. East Burke is home to
442-589: The Military Sealift Command from 1973 to 1991 after service in the United States Navy as USS Passumpsic (AO-107) Topics referred to by the same term [REDACTED] This disambiguation page lists articles associated with the title Passumpsic . If an internal link led you here, you may wish to change the link to point directly to the intended article. Retrieved from " https://en.wikipedia.org/w/index.php?title=Passumpsic&oldid=846210244 " Categories : Disambiguation pages Ship disambiguation pages Hidden categories: Short description
476-548: The Passumpsic River Valley south. H.P. Lovecraft refers to the river in his horror short story The Whisperer in Darkness as a river in which unusual bodies were seen floating after the heavy Vermont floods of 1927. One United States Navy ship has been named for the river. USS Passumpsic (AO-107) was an oiler that served in commission in the U.S. Navy from 1946 to 1973. She then decommissioned, transferred to
510-511: The Passumpsic River in Barnet, to the northwest corner of the town of Waterford, on the railroad. It is about 4 miles (6.4 km) long. The river runs through a narrow valley in Barnet, a gorge with no terraces. Narrow terraces in the Town of Passumpsic expand and form a basin. The fourth terrace on the west side of the river is part of the next basin, which is in St. Johnsbury and Lyndon. St. Johnsbury Village
544-574: The Price Chopper store on the corner where river and the railroad come close together. From here it flows downstream to the confluence of the Moose River. It noticeably widens here after merging coming from the west. The river is often 100-200 wide as it runs south from here on. The Sleepers River runs into it. Next downstream is the Gage Hydro Dam. The Passumpsic flows through the western corner of
578-637: The Sheldon River enters from the east. The river encounters the Vail Hydro Dam and runs to a gravel pit. The Little Falls, about a mile above the Great Falls, have about a 20-foot (6.1 m) descent. The river proceeds from the gravel pit and railroad tracks to the Great Falls Dam downstream. It briefly widens to pond size south of Murray Circle. It encounters the Great Falls Dam and runs downstream to
612-413: The St. Johnsbury Pierce Mills Dam. Roberts Brook enters from the east. Stark Brook enters from the north and west, north of St. Johnsbury Center. A second Roberts Brook enters from the east. A third Roberts Brook enters from the west. The river proceeds through the center of St. Johnsbury from north to south. From its valley the higher lands rise on either side to the east and west. In the southern part of
646-672: The West Branch of the Passumpsic until it converges with the East Branch in Lyndonville . From Lyndonville, the river proceeds southerly through St. Johnsbury Center, St. Johnsbury , Passumpsic, and Barnet , and into the Connecticut River near Nine Island. The East Branch originates about 1/2 mile southeast of Sukes Pond, Brighton , in Essex County . Route 114 nearly parallels it as it runs south-southeast. It soon enters Caledonia County . It
680-426: The level is lower. There is the course of a former river bed which ran towards the east. At the upper village of Lyndon the first terrace is about 1 mile (1.6 km) wide. There is a lot of sand and fine gravel adjoining. Every stream from either side of the valley has its large terraces to correspond with those of the Passumpsic River. It is a characteristic of these terraces that they are large while their quantity
714-454: The mouth of Joes Brook. Joes Brook comes from Joes Pond in Danville and flows in a southeasterly direction through the town, and enters the Passumpsic about 1.5 miles (2.4 km) from its mouth. Next it encounters Pass Hydro. Water Andric enters from the west and south just north of Kitchell Hill. Joes Brook flows into it. Next the river flows through East Barnet Hydro. Joes Brook enters it from
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#1732851865341748-449: The north. The river turns south. Miller Run enters from the west. Miller Run Valley is a sufficiently prominent feature to be followed by Interstate 91 instead of Route 5. South Wheelock Branch enters from the west southwest just south of Riverside Court. The river proceeds to the Route 5 bridge and from there to the Vail Hydro Dam. The river runs southeast, then takes a turn west northwest, as
782-416: The northwest near VT 5A , which nearly parallels it from then on south. The river flows south from that point. After it crosses 5A going south southwest, another unnamed brook enters it from the east Sutton River enters it from the southwest, near U.S. Route 5 at West Burke . Route 5 now nearly parallels it southbound. The river then turns south-southeast. An unnamed brook, which Brook Road parallels for
816-541: The south and west just north of Barnet Center. It flows through East Barnet Hydro downstream to where the Passumpsic enters the Connecticut River from Barnet, about 1 mile (1.6 km) west of the Comerford Dam . The Passumpsic Valley esker is the longest in Vermont and New Hampshire, if not in all of New England. It extends from St. Johnsbury northward past Lyndonville, where it splits into two branches, one extending up
850-540: The town from the Gage Hydro Dam downstream to the Passumpsic Hydro Dam. The river enters from St. Johnsbury through the corner of Waterford, in the northeastern part, and gradually turns and flows south, emptying into the Connecticut about 2.5 miles (4.0 km) from the northeastern corner of the town. It encounters Enerick Brook which comes from Danville and enters the Passumpsic about 1 mile (1.6 km) above
884-646: The town it is joined by the Moose River at St. Johnsbury, a large stream from the east, and the Sleepers River, a smaller tributary, from the northwest. It encounters the Pierce Mills Hydro Dam. It proceeds to the Rapids after a sharp bend downstream across from the Green Mountain Trailer Park above the mall at St. Johnsbury Center. Across from the Green Mountain Trailer Park, it flows downstream to
918-602: The town of Lyndonville, VT . In 2006, the Passumpsic Valley Land Trust was given a grant by the federal government to remove the East Burke Dam from the eastern branch of the Passumpsic. Major Rogers led his rangers to the mouth of the Passumpsic on their retreat from the attack on the Abenaki Indians at St. Francis, Quebec in 1759. Coming south, they had split up into three groups with one following
952-539: The town was 97.14% White , 0.25% African American , 0.57% Native American , 0.19% Asian , 0.38% from other races , and 1.46% from two or more races. Hispanic or Latino of any race were 1.08% of the population. There were 641 households, out of which 30.4% had children under the age of 18 living with them, 58.0% were married couples living together, 9.8% had a female householder with no husband present, and 29.0% were non-families. 21.7% of all households were made up of individuals, and 5.8% had someone living alone who
986-416: The valley seems to be too wide to correspond with the size of the river, the valley may have been formed by water from unknown sources in prehistoric times. The Passumpsic River sustains several dams that produce hydroelectric power for the region. Central Vermont Public Service (CVPS), operates the Passumpsic, Pierce Mills, Arnold Falls, and Gage dams. Great Falls Dam and Vail Dam are locally owned by
1020-465: The valley of the Sutton River to West Burke and the other extending on up the Passumpsic River valley to East Haven. In some places it is over 150 feet (46 m) thick and two or three hundred feet wide. Based on research by Edward Hitchcock two or three basins can be identified based on a larger number of interconnected terraces in the Passumpsic River Valley. The first extends from the mouth of
1054-624: The village of West Burke, leading north past Lake Willoughby to Derby . Vermont Route 114 runs through East Burke, leading north to Island Pond and south to US-5 in Lyndonville. The highest point in town is Burke Mountain , at 3,271 feet (997 m). According to the Köppen Climate Classification system, Burke has a warm-summer humid continental climate , abbreviated "Dfb" on climate maps. The hottest temperature recorded in Burke
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1088-548: Was 1,651 at the 2020 census . The town contains the villages of East Burke , West Burke and Burke Hollow. The town is home to Burke Mountain and Burke Mountain Academy . The town was named for Sir Edmund Burke , a member of the English Parliament . According to the United States Census Bureau , the town has a total area of 34.0 square miles (88.1 km ), of which 33.9 square miles (87.8 km )
1122-454: Was 65 years of age or older. The average household size was 2.45 and the average family size was 2.83. In the town, the population was spread out, with 23.6% under the age of 18, 8.0% from 18 to 24, 28.8% from 25 to 44, 28.3% from 45 to 64, and 11.4% who were 65 years of age or older. The median age was 39 years. For every 100 females, there were 108.6 males. For every 100 females age 18 and over, there were 102.7 males. The median income for
1156-439: Was 98 °F (36.7 °C) on July 19, 1953, while the coldest temperature recorded was −41 °F (−40.6 °C) on February 2–3, 1962. As of the census of 2000, there were 1,571 people, 641 households, and 455 families residing in the town. The population density was 46.1 people per square mile (17.8/km ). There were 892 housing units at an average density of 26.2 per square mile (10.1/km ). The racial makeup of
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