Agno River

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Coordinates: 16°02′17″N 120°12′00″E / 16.03806°N 120.20000°E / 16.03806; 120.20000
Agno River
Agno river.jpg
A portion of the Agno River that is flowing down from San Roque Dam to in between the town of Asingan and Sta. Maria, Pangasinan.
Country Philippines
Regions Central Luzon, Cordillera Administrative Region, Ilocos Region
Tributaries
 - left Tarlac River
Source
 - location Cordillera Mountains
 - elevation 2,090 m (6,857 ft)
Mouth Lingayen Gulf
 - location Lingayen, Pangasinan, Ilocos Region
 - elevation 0 m (0 ft)
 - coordinates 16°02′17″N 120°12′00″E / 16.03806°N 120.20000°E / 16.03806; 120.20000
Length 206 km (128 mi)
Basin 5,952 km2 (2,298 sq mi)
Discharge for Lingayen Gulf
 - average 660 m3/s (23,300 cu ft/s)
Watershed of the Agno River

Agno River is a river in the Philippine island of Luzon, in the province of Pangasinan. It is the fifth largest river system in the country with drainage area of 5,952 km².[1] [2][3] [4] It originates in the Cordillera Mountains and empties into the South China Sea via the Lingayen Gulf. The river is 206 km long. Roughly 2 million people live in the Agno River Valley and it comprises one of Philippines' larger population clusters.

Geography[edit]

The Agno River is the main drainage system of the area and has a catchment area of 5,952 square kilometers. It is the third largest river in Luzon (next to Cagayan River and Pampanga River) and the fifth largest river in the Philippines.

The Agno is the largest Philippine river in terms of water discharge, draining around 6.6 cubic kilometers of fresh water into Lingayen Gulf, or almost 70% of the total fresh water input into the gulf.

The headwaters of Agno River are at the slopes of Mount Data in the Cordillera Mountains at an elevation of 2,090 m, where it drains Cretaceous to Paleocene igneous basement rocks, and marine siliciclastic and carbonate rocks. Of its total length, about 90 kilometers runs through mountainous terrain and canyons.

Agno River (view from Rosales, Pangasinan bridge)

As the river descends following a southerly course, it exhibits a braided channel pattern. It then transforms into a southwest-directed meandering river as it crosses the Central Luzon Plain. From its confluence with the Tarlac River emanating from the south, the Agno River then veers northward while draining the eastern flanks of the Zambales Mountains.

The Agno's principal tributaries include the Pila, Camiling, Tarlac and Ambayoan Rivers. The main branch of the Agno River is Tarlac River which originates from Mount Pinatubo (elevation 1,745 m) in Tarlac and joins the Agno River at Poponto Swamp near Bayambang. The swamp has an area of about 25 square kilometers and temporarily retains flood waters from Tarlac River.

After passing through mountains at an average elevation of some 2,000 feet (600 m) ASL, the Agno River forms a vast alluvial fan and delta called the Pangasinan Plain, a historically vital ecoonomic hub on Luzon Island.

A number of faults of local and regional significance cut across the river. Joint systems are also found in the area. These faults and joints reduce the rock strength and rock coherence through which water could pass or slippage could occur.

The Philippine Fault System, including the Digdig Fault, which has been assessed as the causative fault of the 16 July 1990 Luzon earthquake, and the San Manuel Fault, Bulangit Fault and the San Roque Fault are some of the major fault lines crossing the river.

Agno River in Pangasinan

Flora and fauna[edit]

Spanish explorers who documented the catchment area of the river in the 16th century say the mouth of the Agno was an extensive marshland with rich alluvial soil. It was thickly covered with mangrove and nipa palm trees which served as habitat to many marshland wildlife species.

But the catchment area is now severely deforested. Primary forest has almost completely disappeared apart from a few areas above 800 m ASL. The forests have been replaced by grassland and riceland.

Flooding[edit]

Since the Agno River basin is characterized by mountainous topography, the Ambuklao water reservoir was built to keep it from gushing down and causing devastating effects on the lower levels of the river, the flood runoff estimated annually at about 6,654 million cubic meters reaches the plain in several hours in the river mouth in about a day. Average annual rainfall varies from 2,000 mm in the neighborhood of Tarlac to 4,000 mm in the upper reaches of the Agno River.

The Pangasinan Plain suffers from recurrent and destructive floods. The catastrophic floods of July-August 1972,May 1976, and September 2009 inundated the entire Pangasinan Plain, including the flood plains of the Tarlac River.

The Philippine Atmospheric, Geophysical and Astronomical Services Administration, the national weather bureau, has established a flood monitoring and warning center in Pangasinan.

People[edit]

The Agno traverses several towns in Benguet province where some 35,000 indigenous Ibaloi, Kankanaey and Kalanguya people live. The Ibaloi people of Benguet regard the river as sacred because it gives life.

Barangay Dalupirip, Itogon in Benguet province is held sacred by its people. Portions of the land serve as the burial grounds of their ancestors. The place holds great historical value and is considered one of the remaining seats of Ibaloi culture.

Archaeological sites were discovered at Sitio Camanggaan, Barangay San Roque in San Manuel, Pangasinan and in surrounding areas. Yields consisted of tradeware and earthenware shards and Palaeolithic and Neolithic stone tools.

Economic importance[edit]

The river has three hydroelectric plants: Binga Dam in Itogon, Benguet (29 km upstream); Ambuklao Dam in Bokod, Benguet (37 km upstream) and the San Roque Dam in San Manuel, Pangasinan. Binga has been operational since 1960 and Ambuklao since 1956.

There are several mining concessions in the upper reaches of the river.

The government has also established the Agno River irrigation system to provide irrigation water to some 60 to 100 square kilometers of ricelands in Pangasinan.

Cities and Municipalities[edit]

The following list shows the cities and towns traversed by the Agno River, ordered upstream going downstream:

References[edit]

  1. ^ "The Agno River Basin". ABSCBNNEws.com. 23 October 2009. Retrieved 25 October 2013. 
  2. ^ "Agno River Basin". PAGASA Regional Service Division. Retrieved 21 October 2013. 
  3. ^ Petr, edited by T. (1985). Inland fisheries in multiple-purpose river basin planning and development in tropical Asian countries : three case studies. Rome: Food and Agriculture Organization of the United Nations. p. 20. ISBN 9251023271. 
  4. ^ Kundel, Jim (June 7, 2007). "Water profile of Philippines". Encyclopedia of Earth. Archived from the original on 21 September 2008. Retrieved 2008-09-30. 

Further reading[edit]

  • Siringan, Fernando P. and Mateo, Zenon Richard P. Sediment load partitioning of the Agno River and changes in the shoreline position, National Institute of Geological Sciences, University of the Philippines, Diliman, Quezon City
  • Torres, Ronnie C.; Paladio, Ma. Lynn O.; Punongbayan, Raymundo S.; and Alonso, Rosalito A. Mapping of Areas Affected by Liquefaction during the 16 July 1990 Earthquake Philippine Institute of Volcanology and Seismology and University of the Philippines National Institute of Geological Sciences

External links[edit]