Aroostook River

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Aroostook River
Aroostook River below Washburn, Maine

Aroostook River below Washburn, Maine

Data
Water code US581644
location Maine (USA), New Brunswick (Canada)
River system Saint John River
Drain over Saint John River  → Atlantic Ocean
Confluence of Munsungan Stream and Millinocket Stream
46 ° 20 ′ 42 ″  N , 68 ° 48 ′ 8 ″  W.
Source height 217  m
muzzle Saint John River Coordinates: 46 ° 48 ′ 36 "  N , 67 ° 43 ′ 5"  W 46 ° 48 ′ 36 "  N , 67 ° 43 ′ 5"  W.
Mouth height 75  m
Height difference 142 m
Bottom slope 0.79 ‰
length 180 km (of which 7.5 km in Canada)
Catchment area 6060 km² (of which 5957 km² in Maine)
Discharge at the Tinker
A Eo gauge : 6060 km².
Location: 3.5 km above the mouth
MQ 975/2015
Mq 975/2015
116 m³ / s
19.1 l / (s km²)
Left tributaries Mooseleuk Stream, Machias River , Little Madawaska River
Right tributaries Saint Croix Stream, Scopan Stream, Presque Isle Stream
Small towns Presque Isle , Caribou
Communities Ashland , Masardis , Washburn , Fort Fairfield
Catchment area of ​​the Aroostook River

Catchment area of ​​the Aroostook River

The Aroostook River [ əˈrʏstək ] is a 180 km long right tributary of the Saint John River in the US state of Maine and in the Canadian province of New Brunswick .

The Aroostook River is formed at the confluence of the Munsungan Stream and Millinocket Stream in Penobscot County in northeast Maine. The Aroostook River flows east and northeast through Aroostook County . The municipalities of Masardis , Ashland and Washburn as well as the small towns of Presque Isle and Caribou lie on the river . Major tributaries are Mooseleuk Stream , Machias River, and Little Madawaska Rivers from the left, and the Saint Croix Stream , Scopan Stream, and Presque Isle Stream from the right. The Aroostook River still passes the community of Fort Fairfield . Then it crosses the border into Canada and reaches the province of New Brunswick, where it flows into the Saint John River after 7.5 kilometers.

The region around the Aroostook River was the scene of the Aroostook War in the years 1838–1839 . This resulted in bloodless clashes between the United States and the United Kingdom of Great Britain and Ireland due to border disputes.

Hydrology

The catchment area of the Aroostook River covers 6060 km². Of this, 5957 km² are in Maine. At the gauge 3.5 km above the mouth, the mean discharge is 116 m³ / s. The months with the highest discharge are April and May with an average of 403 and 244 m³ / s.

The United States Geological Survey maintains two gauges along the river . The first measuring point is at Masardis ( ). The catchment area of ​​the river covers 2309 km² at this point. The highest flow rate recorded there was 600 m³ / s, the lowest 1.1 m³ / s. The second level measures data at Washburn ( ). The catchment area at this point covers 4282 km². The highest flow rate recorded at Washburn is 1230 m³ / s, the lowest value is 2.1 m³ / s. The maximum values ​​occur during the snowmelt in spring, the lowest water level is observed in autumn. The highest water levels caused floods caused by ice barriers at both measuring points. This happens relatively often on this river, for example in March and April 1999, in April and May 2003 or in April 2004.

Web links

Commons : Aroostook River  - collection of images, videos and audio files

Individual evidence

  1. Millinocket Stream in the Geographic Names Information System of the United States Geological Survey
  2. a b c d e f Government of Canada: Historical Hydrometric Data Search Results: Station 01AG003
  3. Aroostook River in the Geographic Names Information System of the United States Geological Survey
  4. GJ Stewart, JP Nielsen, JM Caldwell, AR Cloutier: Water Resources Data - Maine, Water Year 2001 (PDF; 4.6 MB) In: Water Resources Data - Maine, Water Year 2001 . 2002. Retrieved February 24, 2012.
  5. VT Hom, EJ Capone, and TW Econopouly: Table 1. Recent Ice Jam Events (PDF; 455 kB) In: Forecasting Ice-Affected Rivers at the Northeast River Forecast Center . 2004. Archived from the original on September 27, 2007. Retrieved January 29, 2008.