Agno River

Coordinates: 16°02′17″N 120°12′00″E / 16.03806°N 120.20000°E / 16.03806; 120.20000
Source: Wikipedia, the free encyclopedia.

Agno River
Rio Grande de Pangasinan
Lingayen
Physical characteristics
SourceMount Data
 • locationBenguet, Cordillera mountains
 • coordinates16°49′34″N 120°53′17″E / 16.826°N 120.888°E / 16.826; 120.888
 • elevation2,090 m (6,860 ft)
Lingayen, Pangasinan, Ilocos Region
 • coordinates
16°02′17″N 120°12′00″E / 16.03806°N 120.20000°E / 16.03806; 120.20000
 • elevation
0 m (0 ft)
Length248 km (154 mi)
Basin size5,952 km2 (2,298 sq mi)[1]
Basin features
Tributaries 
 • leftTarlac River

The Agno River, also known as the Pangasinan River, is a river on the island of

drainage area of 5,952 square kilometres (2,298 sq mi).[2][3][4][5]

The river originates in the Cordillera Mountains and empties into the South China Sea via Lingayen Gulf. The river is 248 kilometres (154 mi) long, making it the sixth longest river in the country.[6] Roughly two million people live in the Agno River Valley, making it one of Philippines' larger population clusters.

The river is

Itogon, and the San Roque Dam in San Manuel
.

Geography

The Agno River is the main drainage system of the area and has a catchment area of 5,952 square kilometres (2,298 sq mi). 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

basement rocks, and marine siliciclastic and carbonate rocks. Of its total length, about 90 kilometres (56 mi) 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

Bayambang
. The swamp has an area of about 25 square kilometres (9.7 sq mi) and temporarily retains flood waters from Tarlac River.

After passing through mountains at an average elevation of some 2,000 feet (610 m) ASL, the Agno River forms a vast alluvial fan and delta called the Pangasinan Plain, a historically vital economic 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 July 16 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

The river's headwaters and upstream basin in the Cordillera Central range are designated conservation areas that lie within the Mount Data National Park, the Upper Agno River Basin Resource Reserve and the Lower Agno Watershed Forest Reserve.

Flora and fauna

Spanish explorers who documented the catchment area of the river in the 16th century say the mouth of the Agno was an extensive

nipa palm
trees which served as habitat to many marshland wildlife species.

But the catchment area is now severely

ASL. The forests have been replaced by grassland and riceland
.

Flooding

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 millimetres (79 in) in the neighborhood of Tarlac to 4,000 millimetres (160 in) 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

floodplains
of the Tarlac River.

The

PAGASA
, the national weather bureau, has established a flood monitoring and warning center in Pangasinan.

People

The Agno traverses several towns in Benguet province where some 35,000 indigenous

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

The river has three

hydroelectric plants: Binga Dam in Itogon, Benguet (29 kilometres (18 mi) upstream); Ambuklao Dam in Bokod, Benguet (37 kilometres (23 mi) 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.

Crossings

This is listed from mouth to source.

  1. Domalandan Bridge (Lingayen–Labrador Road, Lingayen)
  2. Bugallon Bridge ( )
  3. Bocboc Bridge (Gallego Street, AguilarSan Carlos boundary)
  4. Mangatarem–Urbiztondo Road (Mangatarem, PangasinanUrbiztondo, Pangasinan boundary)
  5. President Carlos P. Romulo Bridge (Camiling–Malasiqui–Santa Barbara Rd, Bayambang–Camiling, Tarlac boundary)
  6. Calvo Bridge (Alcala–Bayambang Road, BayambangBautista boundary)
  7. Teofilo Sison Bridge ( ), Rosales–Villasis boundary)
  8. Tomana Underpass ( E1 (Tarlac–Pangasinan–La Union Expressway), RosalesVillasis boundary)
  9. Narciso Ramos Bridge (Santa Maria–Binalonan Road, Asingan, Pangasinan)
  10. Ambuklao By-pass Bridge ( ), Bokod)
  11. Liboong Hanging Bridge (Bokod)
  12. Bokod–Kabayan–Buguias–Abatan Road (Buguias, Benguet)

Cities and municipalities

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

References

  1. ^ Tuddao, Vicente B. Jr. (September 21, 2011). "Water Quality Management in the Context of Basin Management: Water Quality, River Basin Management and Governance Dynamics in the Philippines" (PDF) (Deck). Department of Environment and Natural Resources. Archived (PDF) from the original on August 29, 2016. Retrieved April 5, 2017.
  2. ^ "The Agno River Basin". ABSCBNNEws.com. October 23, 2009. Archived from the original on December 3, 2013. Retrieved October 25, 2013.
  3. ^ "Agno River Basin". PAGASA Regional Service Division. Archived from the original on October 21, 2013. Retrieved October 21, 2013.
  4. .
  5. ^ Kundel, Jim (April 3, 2008). "Water Profile of Philippines". The Encyclopedia of Earth. Archived from the original on September 21, 2008. Retrieved September 30, 2008.
  6. ^ Kenneth Kimutai too (July 24, 2018). "Longest Rivers in the Philippines". WorldAtlas. Archived from the original on August 26, 2019. Retrieved September 9, 2019.
  7. ^ Bagamaspad, Anavic; Hamada-Pawid, Zenaida (1985). A People's History of Benguet Province. Philippines: Baguio Printing & Publishing Company. p. 72.
  8. .

Further reading

  • 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 July 16, 1990, Earthquake Philippine Institute of Volcanology and Seismology and University of the Philippines National Institute of Geological Sciences

External links