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Millers River

Coordinates:42°35′50″N72°29′48″W / 42.59722°N 72.49667°W /42.59722; -72.49667
From Wikipedia, the free encyclopedia
River in Massachusetts, United States
This article is about the river in Massachusetts. For the river in Rhode Island, seeMillers River (Rhode Island). For the former river in eastern Massachusetts, seeMillers River (Middlesex). For the river in Washington, seeMiller River.

Millers River
Map
Physical characteristics
Source 
 • locationConfluence of Bear Meadow Brook and Bluefield Brook,Ashburnham, Massachusetts
 • elevation1,124 feet (343 m)
Mouth 
 • location
Connecticut River atMillers Falls, Massachusetts
 • elevation
175 feet (53 m)
Length52 miles (84 km)
Basin size390 square miles (1,000 km2)
Discharge 
 • average1,000 cu ft/s (28 m3/s)

TheMillers River is a 52.1-mile-long (83.8 km)[1] river in northernMassachusetts, originating inAshburnham[2] and joining theConnecticut River just downstream fromMillers Falls, Massachusetts. Sections of the river are used forwhitewater kayaking, and a section upriver is popular withflatwater racers (canoe racing), and the river is known locally as a good place for pike fishing.

Native names

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The river was formerly known asPapacontuckquash, aNipmuc word meaning "split banks river", frompapahe ("split"),akun ("bank"),tekw ("river"), andesh, a plural marker.Papacontuckquash is cited as the name for the Miller's River, signed and witnessed by the Native leaders on the "Indian Land Deeds for Hampshire County, Later Including Franklin . . . ",[3] where it is also noted that this name is given on "an ancient map" in the collections ofWilliams College. Additionally,Papcontuckquash is given by Sonskqua Mishalisk, 17th centuryPocumtuck leader, as the name for the Miller's River.[4]

Some have assigned "Paquag", "Baqaug", or "Pacquoag" as the name of the river.[5] However, "Paquoag" refers to the location of the town ofAthol.[6] This identification was confirmed by Kchisogmo (Grand Chief) Henry Lorne Masta in 1932 asPakwaik, meaning "arrows place", for the arrowwood (Viburnum dentatum) that grew there, used for making arrow shafts.[7] The termPachaug refers to "clear water" in Nipmuc for a creek and meadow in Squakheag, nowNorthfield, where the word displays the palatization of "k" that conforms to the northern and western dialect of Nipmuk, as indicated by Holly Gustafson inNipmuk Grammar,[8] and confirmed in Dr. Ives Goddard's "The 'Loup' Languages of Western Massachusetts: The Dialectal Diversity of Southern New England Algonquian",[9] whilePacoag retains the unpalatized feature associated withMassachusett andNatick dialect[10] and is associated on land documents withRutland in Worcester County.[11]

Topography

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The Millers River atAthol, MA

The Millers River drains a total area of about 390 square miles (1,000 km2), about 313 square miles (810 km2) of which are in Massachusetts, with the remainder inNew Hampshire. About 78 percent of the basin is forested, 11 percent is open land, 8 percent is wetland, and 3 percent contains urban areas. The watershed is made up of all or part of 17 municipalities, with a population of approximately 87,000 people. Population centers within the watershed are concentrated aroundWinchendon,Gardner,Athol, andOrange.[12]

Many wetlands in the basin indicate areas of former shallow lakes and ponds that have gradually been filled. There are a total of 107 lakes and ponds in the basin, 72 of which have an area of 10 acres (40,000 m2) or more. Only one lake, 592-acre (2.40 km2)Lake Monomonac inWinchendon, Massachusetts, andRindge, New Hampshire, is larger than 500 acres (2.0 km2).[12]

Origin

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The Millers River formed at the end of the last glacial period when several glacial lakes joined and, eventually, drained into the Connecticut River. The river's headwaters are in Ashburnham, Massachusetts, and the headwaters of theNorth Branch are in Mountain Pond, at the western foot of theWapack Range inNew Ipswich, New Hampshire.[12]

Course and connecting waterways

[edit]
Millers River near Erving at autumn

The North Branch and the main stem of the river join in Winchendon, and the river flows westward to the Connecticut River. Major tributaries of the Millers River areTarbell Brook, which enters about two miles west of Winchendon Center, theOtter River, which enters in Winchendon inOtter River State Forest, and the Tully River, which enters in Athol. These tributaries flow mainly through wetlands. Overall, the Millers River has a moderate gradient, averaging about 18 feet/mile from the headwaters area to the USGS streamflow-gaging station atErving, a stream distance of about 43 miles (69 km).

However, a 5-mile (8.0 km) reach of the Millers River through a wooded area betweenSouth Royalston and Athol (the "Bear's Den") has an average gradient of about 43 feet/mile, which is about five times the average for rivers in Massachusetts, and some of the most rugged and steep terrain of the state's central upland. The gradient of the tributary Otter River averages about 18 feet/mile for a distance of about 11.5 miles (18.5 km), and that of the East Branch Tully River, the major tributary of the Tully River, averages about 52 feet/mile over a distance of about 13 miles (21 km).[12]

Birch Hill Dam

[edit]
Birch Hill Dam on the Millers River

The Birch Hill Dam is aflood control dam located on the Millers River in SouthRoyalston, Massachusetts. It is a part of a network of flood control dams on tributaries of the Connecticut River. Completed in 1941 at a cost of US$4 million, Birch Hill Dam was one of the first dams theArmy Corps of Engineers built inNew England to prevent floods like those that devastated Athol andOrange in 1936 and 1938. It has a storage capacity of 16.3 billion US gallons (62,000,000 m3).[13]

The Reservoir Regulation Team (RRT) is the "nerve center" for the New England flood control dams such as Birch Hill Dam. Using radio and satellite communications, RRT constantly monitors river levels and weather conditions that influence flood control decisions.[13] Corps personnel, in conjunction with RRT, regulate the amount of water released downstream by raising or lowering the four 6 ft (1.8 m) by 12 ft (3.7 m) gates located in the gatehouse at the dam. In a time of high water, the gates are lowered in order to hold back the water, only to be released when downstream river conditions begin to recede. In April 1987, two storms dropped over 6 inches (150 mm) of rain, raising the water level to over 33 feet (10 m) at the dam, utilizing 80% of the storage capacity. It is estimated that Birch Hill Dam prevented over $9 million in damages to downstream property from this one storm.[13]

See also

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References

[edit]
  1. ^U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data.The National MapArchived March 29, 2012, at theWayback Machine, accessed April 1, 2011
  2. ^"TopoQuest map for main branch". RetrievedJune 29, 2008.
  3. ^Indian Land Deeds for Hampshire, etc. Liber A, pages 86-88/
  4. ^"Indian Land Deeds For Hampshire, Etc". RetrievedDecember 2, 2020.
  5. ^"NIAC Publications ~ Nipmuc Place Names - Maine & Massachusetts".www.nativetech.org. RetrievedAugust 13, 2018.
  6. ^"First Settlers of Pequoig". RetrievedJanuary 22, 2021.
  7. ^Abenaki Indian Legends, Grammar, and Place Names, Masta 1932
  8. ^"Nipmuk Grammar"(PDF). Archived from the original on April 13, 2017. RetrievedJanuary 22, 2021.
  9. ^Personal communication with author 2018-5-7.Papers of the Forty-Fourth Algonquian Conference/Actes du Congrès des Algonquinistes, 2016;ISBN 978-1-4384-5992-9
  10. ^Bragdon and Goddard,Writings in Massachusett, Volume I.ISBN 978-0871691859
  11. ^"Historical Collections Relating to the History and Antiquities of Every town in Massachusetts with Geographical Descriptions", John Warner Barber, Worcester, 1848
  12. ^abcd"Millers River Drainage Basin". Archived fromthe original on September 23, 2006. RetrievedJanuary 2, 2007.
  13. ^abc"USACE Birch Hill Dam". Archived fromthe original on January 26, 2007. RetrievedJanuary 2, 2007.

External links

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