1. Present River Condition    


The present river condition of Cagayan River is described as follows:

1.1 River System
The total basin area and river length of the Cagayan are 27,300 sq.km and 520 km, respectively. The major tributaries of the Cagayan River are the Chico (basin area: 4,550 sq.km), Siffu-Mallig (2,015 sq.km), Magat (5,110 sq.km) in the left bank, and Pared (970 sq.km), Tuguegarao (660 sq.km), Tumauini (960 sq.km) and Ilagan (3,130 sq.km) in the right bank.


 

The main Cagayan River originates in the Caraballo mountain range. Passing through the mountainous areas towards north-northeast, it joins the largest tributary, the Magat, at the left bank and the right tributary, the Ilagan, in succession. According to site reconnaissance, denuded areas exist in various places in the upper Magat river watershed, especially of the Santa Cruz river, while vegetation in the mountainous areas extending over the right bank of the Cagayan river is relatively rich. The total basin area of the Cagayan at the confluence with the Ilagan is around 15,100 sq.km.

Magat dam located at the gorge of the upper Magat, has two functions of irrigation water supply and hydroelectric power generation. The dam is in operation by National Irrigation Administration (NIA). The dam has basically no flood control space in its reservoir, although it can be said that the dam is being substantially contributing to flood peak reduction. According to the recent operation records of the reservoir obtained so far, flood peak reduction will be ranging from 3,000 to 2,000 cu.m/s in average.


 
Just downstream from the confluence with the Ilagan, the Cagayan River changes its direction towards north-northwest, and flows down in the alluvial plain and reaches Alcala. The Cagayan river channel in this reach meanders remarkably, especially in the downstream of Tuguegarao. The major tributaries in this reach are the Siffu-Mallig in the left bank and Tumauini, Tuguegarao and Pared in the right bank. The total basin area at Alcala is around 21,400 sq.km.

 
From Alcala to Magapit, the Cagayan River runs further towards north-northwest passing through the valley area called as the Magapit Narrows. The river width becomes narrow with around 350 m over 30 km stretch. Particularly, there exist two (2) narrow sites of Nassiping and Magapit. Just upstream of the Magapit suspension bridge, the Magapit irrigation pump station locates at the right bank. The pump station is in operation by NIA and covers a total service area of 11,500 ha extending over the right bank. In the reach of the Magapit Narrows, the Cagayan river joins the second largest tributary, the Chico at the left bank, and minor tributaries, the Zinundungan at the left bank and the Dummon at the right bank. The total basin area of the Cagayan at Magapit is around 26,600 sq.km. After passing through the Magapit Narrows, the Cagayan flows down in the flat area (so called as delta) changing its direction to north, and finally discharges into the Babuyan channel at Aparri

 

1.2 Bank Erosion  
Bank erosions are observed in various places of the main Cagayan and its tributaries, especially of the main Cagayan. There exist some bank protection works to protect residential areas, trunk roads, etc., although protected areas are extremely limited. Only bank protection works by spur dike and revetment are major existing flood control works.

Several sites are being exposed to possible destructive damage. Such districts as Cabagan, Namabbalan, Bagumbayan, Cataggaman, Enrille, San Vicente near Iguig, Babayuan etc., are in the critical condition. Bank erosion is one of the most serious flood control problems in the Cagayan river basin. Critical sites prone to destructive damage against urban areas, villages, trunk roads, etc., will be further studied in the later section.



1.3 Sedimentation  
According to site reconnaissance, it proves that vegetation in the mountainous areas extending over the left bank (Cordillera Central Mountains) of the main Cagayan is poor whereas that of the right bank (Sierra Madre Mountains), is relatively rich. In addition, violent landslides are widely observed especially in the upper watersheds of the Magat. The historical earthquake occurred in 1990, brought about such landslides.

Resulting in such devastating natural situation, sediment discharges from the upper watersheds are abruptly being increased especially from those of the left serious flood control problems in the Cagayan river basin.


1.4 Flood Inundation Hazard Map
The Cagayan river basin has about 1,860 sq.km of flood prone areas which are presently used as production areas of rice, corn, legumes, and vegetables, according to the data: Integrated Regional Disaster Management, RDCC Region II. The flood prone areas of 1,860 sq.km were estimated for inundation areas brought by the 1973 flood, the recorded biggest one in the past. Fifty-two municipalities extend over the above areas. Afterwards, a big flood occurred in 1980 and the inundation areas by the 1980 flood reached about 1,740 sq.km. The remarkable and historical floods caused such extensive inundation areas extending over the higher alluvial plain that is being explained later.

 
On the other hand, delineation of the inundation areas by the 1998 flood, based on the data obtained from the Office of Civil Defense (OCD) Region II and interview surveys were within the limited areas of lower alluvial plain in case of normal flood magnitude.

Inundation Area Map


October 1973 Flood

October 1998 Flood

CAGAYAN RIVER BASIN

Location:
The Cagayan River basin, of which the catchment area is 27,281km2, is located in the northeastern part of the Luzon Island. The basin lies between 15°52 and 18°25 north latitude and between 120°51 and 122°18 east longitude. It is bounded in the east, west and south by the Sierra Madre, Cordillera Central and Caraballo-Maparang mountain ranges.



Socio-economy:
In the Cagayan River basin, a population was estimated at 2.55 million in the 1995 census year, distributing 2.13 million or 84% of the basin population in Region 2, 0.50 million or 16% in CAR, and 9 thousand or 0% in Region 4. Thus, Region 2 would represent a basin socio-economic character.  GRDP of Region 2 in 1998 was 55.2 billion pesos, accounting for 2.0% of the national GDP. GRDP per capita of Region 2 was 20,200 pesos in the same year, accounting for 56% of the national one due to low agricultural productivity caused by habitual flood inundation. At present, thus, the regional economy is backward in economic condition in the country. In the region, agricultural production attained the largest share (43%) among the major economic sectors. It accounted for 5.3% of the national agricultural production. In order to accelerate economic growth, the governments have to intensify their effort to increase production factors such as capital and labor, to increase productivity by improving technology level.

Topography and Geology:
The Cagayan River basin is mostly hilly to mountainous. Land with a slope of less than 8% is around 9,500km2, which has been rather well developed as the agricultural land. Hilly land with slopes between 8% and 18% covers about 3,800km2. The substantial parts of the hilly land are left to be grass land. The remaining 14,000km2 are mountainous.  Rocks of the Cagayan River basin is represented by a thick sequence of pre-Tertiary metamorphic and plutonic rocks. An Oligocene to Pliocene Marine section occupies the main basin area. Although many earthquakes were experienced in northern Luzon, relatively fewer earthquakes occurred within the Cagayan valley. Intense earthquakes are assumed to be tectonic origin and rarely of volcanic nature. The magnitude of the earthquake occurred in July 1990 about 70km south from Santa Fe was recorded at 7.8 in Richter scale.

Hydrology:
The climate in the Cagayan River basin consists of monsoons, i.e. the southwest monsoon and northeast monsoon. Typhoons normally strike during July to December with about 8 times a year on an average. A primal portion of annual rainfall of 2,600mm is, however, ascribed to the southwest monsoon. The record indicates that the basin is affected by El Nino almost every three years.  Average annual runoff is estimated to be 1,343m3/s at the mouth of the Cagayan River. The 100 year probable flood is estimated to be 21,400m3/s at the mouth under the present river condition.

River System:
The total basin area and river length of the Cagayan are 27,281km2 and 520km, respectively. The major tributaries of the Cagayan River are Chico River (basin area of 4,550km2), Siffu-Mallig River (2,015km2), Magat River (5,110km2) on the left bank, and Pared River (970km2), Tuguegarao River (660km2), Tumauini River (960km2) and Ilagan River (3,130km2) on the right bank. 

Major Dimensions: Major dimensions of the main Cagayan River are as follows:

Riverbed Slope
- River mouth to Magapit Bridge: 1/13,000
- Magapit Bridge to Alcala: 1/8,500
- Alcala to confluence with the Tuguegarao River: 1/9,000
- Tuguegarao River confluence to Cabagan: 1/7,000

Channel Width
- River mouth to Magapit Bridge: 1,000 to 2,000 m
- Magapit Bridge to Alcala: 300 to 1,000 m
- Alcala to Tuguegarao: 500 m - Upstream of Tuguegarao: 600 m

Carrying Capacity
- River mouth to Magapit Bridge: 10,000 to 18,000 m3/sec
- Magapit Bridge to Alcala: 5,000 to 15,000 m3/sec
- Alcala to Cabagan: 3,000 to 6,000 m3/sec

The carrying capacities below the riverbank elevation of both the rivers Chico and Tuguegarao are summarized below.

Carrying Capacity of the Lower Chico River
- Confluence to 10 km upstream: 5,000 to 10,000 m3/sec
- 10 km to 14 km upstream: 2,000 to 4,000 m3/sec

Carrying Capacity of the Lower Tuguegarao River
- Confluence to 3 km upstream: 3,000 m3/sec
- 3 km to 9 km upstream: 6,000 m3/sec
- 9 km to 14 km upstream: 2,000 m3/sec

River Geomorphology:
Compound actions of repeated upheaval and lowering ground movements in the prehistoric time formed a Cagayan Valley with bottlenecks of Magapit Narrows, in the zone between tectonic lines of north-south and east-west directions. Afterwards, alluvial plain in the Cagayan River was gradually developed in combination with the repeated both the actions of sedimentation by rivers and fluctuation of seawater level. The present alluvial plain extending over the upstream at Alcala was thus formed largely by backwater phenomena due to the bottlenecks in the Magapit Narrows. Similarly, river meandering naturally and violently proceeded in the alluvial plain because of gentle slope gradient.

Variation of River Channel:
River course shifting in the reach from Alcala to upstream of Tuguegarao is so significant. Active shifting is caused by fairly gentle water surface slope due to backwater from the bottlenecks in the Magapit Narrows. Just upstream at Iguig, the extent of shifting reaches 5 km in an interval for only the past 50 years. Such shifting generally occurs not gradually through years but suddenly or accidentally in the flood time. The tendency of the riverbed variation is
1) no significant change in the reaches from the river mouth to Magapit bridge and from confluence with the Tuguegarao River to Cabagan, and
2) slightly raised in the reaches from Magapit bridge to confluence with the Tuguegarao River.
There is no remarkable increase of the sandbars near the Cagayan River mouth, although its local shifting has been observed. In the Cagayan River, river channel meanders especially in the reach from Alcala to upstream of Tuguegarao. There is a tendency of the said reach changing to a straight river course.

Bank Erosion and Sedimentation:
Bank erosion is observed in various places of the main Cagayan River and its tributaries, and is one of the flood control problems. Average annual bank erosion rate in the downstream of the Magapit Narrows reaches 10m, while that in the upstream of Alcala reaches 24m. The existing bank protection works consist of spur dike and revetment. The sedimentation in the Magat reservoir is serious, of which the accumulated sediment volume was recorded at 188 million m3 in 1999. In the lower Cagayan River, it can be said that sedimentation is not serious in view of the actual variation of riverbed and sandbars, although local sedimentation is observed at the inlet of Amulung pumping station and the confluence with a small tributary of the Appagonan River at Aparri.

Inundation Area:
The Cagayan River has about 1,860km2 flood prone areas, which are presently used as production areas of rice, corn, legumes and vegetables. The area of 1,860km2 was estimated from that brought by the 1973 flood, which was the biggest one in the past. The inundation areas are within the limited areas of lower alluvial plain except for some natural levees with higher elevations. Afterwards, alluvial plain in the Cagayan River was gradually developed in combination with the repeated both the actions of sedimentation by rivers and fluctuation of seawater level. The present alluvial plain extending over the upstream at Alcala was thus formed largely by backwater phenomena due to the bottlenecks in the Magapit Narrows. Similarly, river meandering naturally and violently proceeded in the alluvial plain because of gentle slope gradient.

Present Prevention System:
Disaster Coordinating Council (DCC) prepares damage reports upon occurrence of disasters. According to the damage reports, the damages were estimated in Region 2 to be 1.8 billion pesos for Typhoon Iliang in 1998, 0.5 billion pesos for Typhoon Loleng in 1998 and 0.3 billion pesos for Typhoon Pepang in 1999. In Region 2, RDCC2 prepared the general action plan for typhoons/floods OPLAN BAGYO/LAYOS in May 1998. Cordillera RDCC also prepared Cordillera Regional Disaster Management Plan in 1994. The purposes of the disaster action plans are to implement effective disaster preparedness, mitigation and prevention activities to minimize damage to property and human suffering. In the Cagayan River basin, some joint operation on the disaster management is conducted between RDCC2 and Cordillera RDCC so that an assistance of the RDCC2 is given on the occasion of emergency in the Chico or other river basins. There are two existing flood forecasting and warning systems, one is the Cagayan Flood Forecasting and Warning System operated by PAGASA and the another is Magat Dam Flood Forecasting and Warning System under NIA. Both systems have problems of malfunction of equipment and insufficient operation and maintenance of the system. The existing evacuation system is operated and maintained by RDCC, PDCC, CDCC/MDCC and BDCC. There are 464 designated evacuation centers in Region 2. Major problems are insufficient supply of drinking water and food, and lack of cooking facilities and comfort rooms in the evacuation centers.

Present Watershed Condition:
The forest cover of the Cagayan River basin has been decreased and the SAFDZ data shows the present forest cover of 37% of the basin. The erosion map of BSWM indicates moderate to severe erosion areas in the upper Magat, upper Cagayan and upper Chico watersheds. In the upper Magat River basin, issues on land collapse and sediment deposit caused by the earthquake occurred in 1990 are remarkable, which affect the reservoir sedimentation of the Magat Dam.

Present Watershed Management:
DENR Region 2 has several forest plantation and other programs/projects focused on the rehabilitation, development and protection of the watershed in the Cagayan River basin. DENR CAR has also implemented some projects such as check dam construction and stone masonry. Other government agencies such as NIA and NPC and LGUs also worked hand in hand with DENR in the watershed management projects including Magat River basin and Casecnan Project. Some foreign assisted watershed management projects were implemented or ongoing, which include forestry sector project of JBIC, DENR-ITTO project and OISCA project. DENR Region 2 and CAR have their respective regional master plan for forestry development.

Present Land Use: 
Out of 27,281 km2 of the Cagayan River basin, about a half of the area is more than 400 m in elevation and area of land slope over 18% covers more than 50%. Forest occupies 37%, grassland 34%, agricultural area 27% and others such as settlement, water area, etc. 2% in the basin. The agricultural area of 741,000 ha consists of fruit tree area (44,000 ha) and crop field (697,000 ha). The crop field comprises paddy field (474,000 ha), corn field (151,000 ha) and other upland crop field (72,000 ha). Most of the potentially cultivable area is already used as the agricultural land.

Present Agricultural Condition:
The Philippine is currently insufficient in staple food supply. Averaged imported rice (1995-99) is estimated at 12% of national consumption, although rice production has an increasing trend. Corn production in the Philippines has been slightly decreasing mainly due to decreasing of white corn production. Department of Agriculture (DA) is the leading agency to extend agricultural support services. The progress of CARP in Region 2 and CAR is 87% and 84%, respectively. About 70% of the primary cooperatives in the area are multipurpose agricultural cooperatives followed by multipurpose non-agricultural cooperatives.

Problems on Agriculture:
The problems on marketing and post-harvest in the area are,
1) deficit of working capital,
2) poor condition of farm to market roads,
3) shortage of labor for harvesting,
4) lack of drying floors and facilities, and
5) low price of product.
The existing constraints/challenges for the development in the basin are;
a) environmental degradation in agriculture,
b) inadequacy of economic opportunities, limited investment to the sector and weak global competitiveness,
c) inadequacy of rural infrastructure, and d) high poverty incidence in the rural areas.

Needs of Agriculture:
Further growth of agricultural sector will need to be attained through expansion of areas under irrigated agriculture with effective water use, higher crop yields, improved cropping patterns, and increased productivity of livestock and coastal fisheries activities. At the same time, particular attention is required to be paid to increasing small farm productivity.

Present Irrigation Condition:
Out of total potential irrigable area of about 3.1 million ha in the Philippines, 43% or some 1.3 million ha is counted as the service area by NIA. Increase rate of irrigation service area became dull in 1990s from various reasons. Potential irrigation development area in the Cagayan River basin is estimated around 511,000 ha. Existing irrigation service area is obtained to be 222,000 ha or 43% of total irrigable area. Irrigated cropping intensity (ICI) in NIS and CIS is 132% in average in the basin. Constraints in irrigation development and in existing system include technical and financial insufficiency, natural calamities including flood by typhoon, land slide by earthquake, drought, etc., and social problems.

Terrestrial Flora:
The number of family and species recorded is 79 and 298, respectively. Of all the species recorded, there are 7 species that are considered endangered being pressured by human activities and/or due to its habitat loss. The results of on-site survey shows that tree species still dominate the lower Cagayan River area in terms of number of species (88 species). They are followed by the shrub (24 species) and then the grass species (10 species).

Terrestrial Fauna:
A total of 75 families and 182 species of terrestrial fauna were recorded in the Cagayan Valley based on secondary data. Among those recorded, the number of species listed in IUCN Red List and CITES List is 19 and 29, respectively. The results of on-site survey show that a total of 54 species were recorded on sampling areas, including 42 species of birds, 6 of mammals, 4 of reptiles and 2 of amphibians.

Protected Area:
DENR, Region 2, designated eighteen protected areas in the whole Cagayan basin, eleven of which are located in Region 2, six are in CAR, and one straddles over the 2 regions. None of those are located within riverbed of the Lower Cagayan River although Peņablanca Protected Landscape lies over Pinacanauan de Tuguegarao River, a tributary of the Cagayan River.

Aquatic Ecology:
There are some fifty nekton species, or Class Pisces, Class Crustacea and Class Mollusca, found in the river system. The results of on-site survey shows that a total of 141 species were noted for the entire Cagayan River System, which is composed of 44 phytoplankton, 18 zooplankton, 15 benthos, 47 fishes, 7 macro crustaceans and 10 molluscs. There are 16 migratory species in the river and all are catadromous.

Water Quality:
Results of water quality sampling shows that Cagayan River and its tributaries are of good water quality under Class C Category especially in terms of high DO and low BOD, EC, nitrogen, and phosphate. However, microbial quality as Coliform Bacteia of surface water generally exceeded the standards set. This implies that sewage from residences and buildings including domestic waste is inflowing to the Cagayan River system. As a whole, however, the water quality of the Cagayan river is usable for agricultural irrigation. Groundwater is of good quality, except those that exhibit acidic water pH with increased conductivity, turbidity, and total solids. Microbial quality indicates Coliform contamination, rendering these wells unsuitable for drinking without treatment such as by boiling or chlorination.

Air Quality and Noise:
Results of the ambient air quality sampling indicate that the values of all air quality parameters are much lower than the corresponding air quality standards as defined in DAO 14 suggesting ambient air quality is possibly not of major concern within the study area at the present. Noise levels in residential areas were less than any class of Ambient Noise level Criteria provided by DENR. In town centers, noise levels were within 57 to 76 except that of Town Market in Ilagan with noise level of 90.9 dBA.

Fisheries:
The fishing industry in Region 2 is one of the most productive in the Philippines. A considerable portion of the population in the region relies on the industry for food and for income generation. The total number of fishing households is 31,301 in 1996, occupying 5.7% of total households. Cagayan River and Magat Dam are listed as one of the major fishing grounds in the Region. At least 30 species of edible fishes and shellfishes are recognized in the lower Cagayan River.

Navigation:
17 routes for navigation currently exist along the river. The navigation routes are important for economic activities in this area in terms of trip, transportation and commute under such conditions that insufficient road network or lack of bridges. Of the 17 navigation routes, six are located in the lowest reach between river mouth and Gattaran. Five are located between Alcala and Tuguegarao, and the rest are over the upstream reach of Tuguegarao.

Water Rights:
The total number of the grantees is 1,584 as of 1999, including private person, company and Government, i.e. NIA, FSDC, NPC, and so on. Sources of water intake are surface water and groundwater. The main use of water is irrigation with the number of 1,427, counting for 90.1% of all the water intakes. The rest is as domestic (111), power (26), industrial (7), livestock (6), fisheries (5) and recreational (2).


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