The Penobscot River watershed
|Basin countries||United States|
|Length||109 miles (175 km)|
|Mouth elevation||sea level|
|Avg. discharge||12,080 cu ft/s (342 m3/s)|
|Basin area||8,610 sq mi (22,300 km2)|
|Left tributaries||East Branch Penobscot River,
|Right tributaries||West Branch Penobscot River,
The Penobscot River // is a 109-mile-long (175 km) river in the U.S. state of Maine. Including the river's West Branch and South Branch increases the Penobscot's length to 264 miles (425 km), making it the second longest river system in Maine and the longest entirely in the state. Its drainage basin contains 8,610 square miles (22,300 km2).
It arises from four branches in several lakes in north-central Maine, which flow generally east. After the uniting of the West Branch with the East Branch at Medway ( ), the Penobscot flows 109 miles (175 km) south, past the city of Bangor, where it becomes navigable. Also at Bangor is the tributary Kenduskeag Stream. It empties into the Atlantic Ocean in Penobscot Bay. It is home to the Penobscot people that live on Indian Island.
The United States government maintains three river flow gages on the Penobscot river. The first is on the East Branch in Grindstone (an unincorporated settlement approximately 10 miles (16 km) south of Stacyville) ( ) where the rivershed is 1,086 square miles (2,810 km2). Flow here has ranged from 400 to 1,300 cubic feet per second (37 m3/s). The second is in West Enfield ( ) where the rivershed is 6,671 square miles (17,280 km2). Flow here has ranged from 4,410 to 9,660 cubic feet per second (274 m3/s). The third is in Eddington ( ), 0.4 miles (0.64 km) downstream from the Veazie Dam where the rivershed is 7,764 square miles (20,110 km2).
Most historians have accepted the Penobscot region as Jean Allefonsce's source for Norumbega, though the matter was hotly contested by some nineteenth century antiquarians, who argued that the name should be identified with their own river or region.
The Penobscot River was an early trade corridor to interior Maine from the Atlantic coast. Ocean ships could navigate upstream to Bangor. The cities of Rockland, Belfast, Brewer and Bangor, and the towns of Rockport, Camden, Northport, Searsport, Stockton Springs, Castine, Bucksport, Frankfort, Winterport, Orrington, and Hampden developed adjacent to the Penobscot River estuary. The river upstream of Bangor became an important transportation corridor for log driving to bring wooden logs and pulpwood from interior forests to sawmills and paper mills built to use water power where the city of Howland and the towns of Veazie, Orono, Old Town, Milford, Passadumkeag, West Enfield, Lincoln, Winn, Mattawamkeag, Medway, and Millinocket developed.
The first European known to have explored the river was the Portuguese Estêvão Gomes in 1524, followed by the Frenchman Samuel de Champlain in 1605. A few years later French Jesuit priests came among the Penobscot people as missionaries and converted them to Catholicism. The French settlement of Pentagouet, now Castine, was founded at the point where the river becomes Penobscot Bay, and the Penobscot people made a permanent settlement at Indian Old Town, Maine on an island above the head of navigation, around the Catholic mission. Throughout the first half of the 17th centuries, these were likely the only permanent settlements on the river, although the Penobscots considered the entire river and bay their hunting ground and maintained other seasonal villages along its banks.
In 1669, the Mohawk tribe made raids from the west that were very destructive to the Penobscot people. During Father Rale's War, the English settlers in Massachusetts also sent periodic raiding parties to the Penobscot, destroying the primary native village in 1723. In a treaty of 1752, however, Massachusetts laid claim to the entire Penobscot watershed, and in 1759 the Pownall Expedition, led by Governor Thomas Pownall, established Fort Pownall on Cape Jellison in what is now Stockton Springs. This signaled the beginning of English domination, and the incorporation of the Penobscot River valley into New England.
The first permanent English settler on the river was Joshua Treat (1726–1802), who was initially the armorer and translator at Fort Pownall. His oldest son, Joshua Treat, Jr., built a log house and sawmill at Marsh Bay in what is now Frankfort, and other members of their extended family, joined by additional settlers from Massachusetts and New Hampshire, pushed ever further up-river, eventually restricting the Penobscot people to Indian Old Town, Maine, the present Penobscot Indian Reservation.
American Revolution and modern history
During the American Revolutionary War, the river and bay were the site of the disastrous 1779 Penobscot Expedition, where an entire American fleet was destroyed in a botched attempt to retake Maine from the British. During the War of 1812, the British again invaded Maine and defeated an American force at the Battle of Hampden, sacking the town of Bangor in the process. To prevent this from happening a third time, and because the nearby boundary between the United States and British Canada was still contested into the 1840s, the Federal government in 1844 began constructing a huge granite fort, Fort Knox, opposite the town of Bucksport, near the mouth of the river. The fort never fired a shot in anger, but remains one of the Penobscot's major man-made landmarks.
In the 19th century the river was a conduit for the transport of logs from Maine's Great North Woods, to be sawn into lumber at mills around Old Town and Orono, and transported on ships from Bangor, at the head of tide. (The average high tide at Bangor is 13 feet (4 m) as of 2009.) A secondary economic use made of the river late in the century was as a source of sawn ice for urban markets.
In the 20th century, lumbering was largely supplanted by papermaking, in the form of large wood pulp and paper mills located all along the river from Millinocket and East Millinocket in the north, to South Brewer and Bucksport in the south. The development of cheap hydropower also attracted other types of light manufacturing, like textiles and shoes.
In the 21st century, with the continuing decline of the Maine paper industry, and the divestiture of its woodlands, the Penobscot watershed is becoming more and more associated with recreational use (fishing, hunting, boating, and tourism) and less with manufacturing. Demolition began on the Veazie Dam in July, 2013.
In 1931 the Waldo-Hancock Bridge was opened to carry US Route 1 across the river at the Penobscot Narrows between Prospect, in Waldo County, and Verona Island just below Bucksport. That bridge was closed and replaced in 2006 by the Penobscot Narrows Bridge, a 2,120 foot long, $85,000,000 structure with 135 feet between the water and the bridge’s deck, and the original bridge was subsequently demolished in 2013. The new bridge also features an observatory open to the public located 420 feet above the surface of the river in the support tower on the Waldo County side. It is the only bridge observatory in the United States, and only one of four bridge observatories in the world. The two 447 foot tall granite towers of the bridge are patterned after the Washington Monument which had been largely built with granite quarried from nearby Mt. Waldo.
Angling the Penobscot River
Angling, especially fly fishing, has always been popular on the river. The West Branch is known as a world class landlocked salmon river, while the East Branch is known for its smallmouth bass fishery. In 2008, the Atlantic Salmon Commission opened the main stem of the river to catch and release fly fishing for Atlantic salmon.
The West Branch is home to many types of fish such as landlocked salmon and Brook Trout. There are many deep pools within the river, due to the many slate ledges, making the river ideal for fishing from shore, though there are still areas that are good for canoe fishing. The river is great for a day fishing trip, however there are a few campsites located sporadically around for people who wish to stay more than one day. With the Ripogenus Dam by Chesuncook Lake, the West Branch is able to sustain the large landlocked salmon found there, with twelve miles of heavy rapids, deep runs, large pools, and slower moving water in some sections. Baxter State Park to the north adds to the natural beauty of the area, and natural protection as well.
Some of the river's rapids are class IV or even V, making this one of the roughest rivers in the area, which attracts many whitewater rafters. Until 1971 the West Branch was the main thoroughfare for the Great Northern Paper Company to sluice its logs to its mill in Millinocket, Maine. In 1971 Great Northern opened the Golden Road (Maine) for transporting the logs. The road parallels the river. The paper industry has been greatly diminished and the Millinocket mill is in the process of being torn down. The road now is extensively used by sportsmen on the river.
As for which flies hatch when (in order to use the right flies), May to June are usually when mayflies begin their first hatch. Caddisflies also start their massive hatch around this time, but it can extend into the fall at times. Stoneflies tend to hatch throughout the season, and often lead to very big catches. In the West Branch, fishermen are often required to use a variety of different techniques in order to catch the elusive fish.  
- Henry David Thoreau published an account of travelling up the Penobscot from Bangor in 1846, to climb Mount Katahdin in his work, Ktaadn.
- Author Stephen King placed his fictional town of Derry, Maine on the Penobscot.
- The Penobscot is also featured in the film adaptation of the Tom Clancy novel, The Hunt for Red October as the location chosen in which to hide the Soviet submarine from spy satellites.
- Discharge for West Enfield
- U.S. Geological Survey. National Hydrography Dataset high-resolution flowline data. The National Map, accessed June 22, 2011
- USGS 01029500 East Branch Penobscot River at Grindstone, Maine. U.S. Geological Survey. 10 October 2009. Accessed 10 October 2009.
- USGS 01034500 Penobscot River at West Enfield, Maine. U.S. Geological Survey. 10 October 2009. Accessed 10 October 2009.
- G.J. Stewart, J.P. Nielsen, J.M. Caldwell, A.R. Cloutier (2002). "Water Resources Data – Maine, Water Year 2001" (PDF). Water Resources Data – Maine, Water Year 2001. Archived from the original (PDF) on November 18, 2005. Retrieved 2006-05-07.
- John Fiske, The Dutch and Quaker Colonies in America (NY: 1899) p. 70: “the most common opinion is that the Penobscot was the River of Norumbega, with a village on its bank somewhere up country, where European skippers traded with the natives for furs”. Fiske argued for the Hudson being Norumbega.
- DeLorme Mapping Company The Maine Atlas and Gazetteer (13th edition) (1988) ISBN 0-89933-035-5 maps 15,23,33,43&44
- "Tidal Station Locations and Ranges". NOAA. Retrieved 2009-04-08.
- The Penobscot River Bridge Observatory Maine Department of Transportation
- Kreh, Lefty; Middleton, Harry (1993). Lefty's Favorite Fly Fishing Waters-Volume One-United States. Birmingham, Alabama: Odysseus Editions. pp. 13–16.
- Rules of the Atlantic Salmon Commission
- Penobscot River. http://www.visitmaine.com/attractions/outdoor_recreation_sports_adventure/fishing/river_country/rivers/penobscot_river/
- Penobscot River Fishing. http://www.maineriverguides.com/penobscot-river-fishing
- "Penobscot River". Geographic Names Information System. United States Geological Survey. 30 September 1980. Retrieved 2010-05-18.
- Real-time river flow data at Eddington – height only.
- Godfrey, John E. *The Ancient Penobscot, or Panawanskek. as transcribed from The HISTORICAL MAGAZINE and Notes and Queries concerning The Antiquities, History, and Biography of America. (Third Series, Vol. I, No. II; Whole Number, Vol. XXI, No. II) February, 1872. (Morrisina, N.Y., Henry B. Dawson) pp. 85–92 (illustrated & annotated)
- "Joshua Treat, The Pioneer Settler on Penobscot River." The Bangor Historical Magazine, Vol. IV, No. 9-10, pp. 169–176 April, 1889.
- USGS River Basin Info
- "The Penobscot River Restoration Project"
- National Weather Service forecast of river levels and flow.