The Davao River catchment is the third largest river catchment on the Southern Philippines Island of Mindanao. It drains an area of over 1700km² with a river length of 160km. Most of the area is uplands. Average flows within the river near to the mouth are estimated at 70-80 cubic meters per second. The climate type is relatively uniform throughout the year with evenly distributed rainfall and temperatures and humidity (rainfall = 2600mm, Actual Evap 1028mm). The area rarely experiences typhoons. A catchment is any device or structure that captures water. ... Mindanao is the second largest and easternmost island in the Philippines. ... In meteorology, precipitation is any kind of water that falls from the sky as part of the weather. ... For other uses, see Temperature (disambiguation). ...

Stats

• River Length: 180km
• Maximum Elevation: 1875m
• Rainfall Average: Mean annual rainfall is 1800mm. Rainfall is evenly distributed throughout the year.

Topography/Soil Type

Plains and Valley: Parent Material:

• San Maguel Silty Clay Loam: Alluvium of igneous
• Matina Clay Loam : Alluvium from limestone, shale and sandstones

Intermediate Upland: Alluvium (from the Latin, alluvius, from alluere, to wash against) is soil or sediments deposited by a river or other running water. ... For other uses, see Limestone (disambiguation). ... Shale Shale is a fine-grained sedimentary rock whose original constituents were clays or muds. ... Red sandstone interior of Lower Antelope Canyon, Arizona, worn smooth due to erosion by flash flooding over millions of years Sandstone is a sedimentary rock composed mainly of sand-size mineral or rock grains. ...

• Tugbok Clay: Igneous rock Andesites
• Faraon Clay: Soft Corraline limestone
• Cabantain Clay: Soft shales with mix of weathered gravels and pebbles

Hills and Mountains: Volcanic rock on North America Plutonic rock on North America Igneous rocks (etymology from latin ignis, fire) are rocks formed by solidification of cooled magma (molten rock), with or without crystallization, either below the surface as intrusive (plutonic) rocks or on the surface as extrusive (volcanic) rocks. ... A sample of andesite (dark groundmass) with amygdaloidal vesicules filled with zeolite. ...

• Camansa sandy clay loam: Shale and sandstone with weathered gravel and sand
• Mountain Soils: undifferentiated : Various igneous and metamorphic rock

Quartzite, a form of metamorphic rock, from the Museum of Geology at University of Tartu collection. ...

Demographic properties

• DRW Population: ~ 800,000
• Average per capita income: 144,039 per family per annum (2000 National average)
• Industrial and agricultural Gross Domestic Product: 64.1 Billion Peso for Region XI
• Population Below Poverty Line: 45% in rural areas ; 27% in urban areas (for southern Mindanao)
• Water Poverty Index parameters: Medium (WPI 56-61.9).

Land uses

The landform and landcover within the basin is highly diverse. Ranging from lowland urban, agricultural, wetland and mangrove to natural riparian, plantations, upland agriculture and mountainous forest including primary forest. The area is classified by DENR as 77.5% forestlands and 22.5% alienable and disposable land. This is not a true land uses (or land cover) classification. Detailed land use is not available. Information is available from several sources including the Comprehensive Land Use Plan of the City, however this data is as yet theoretical and does not represent the realities or suitability of land at the barangay (lowest tier of local government) level. However the City Planning Office is collecting and digitizing data for land use maps. A landform comprises a geomorphological unit, and is largely defined by its surface form and location in the landscape, as part of the terrain, and as such, is typically an element of topography. ... Above and below water view at the edge of the mangal. ...

Water resources and uses in the basin

River discharge measurements taken from 1984 to 1990 indicated an average river flow of approximately 78 cubic meters per second for the period.

The main drinking water sources for Davao City are in the neighboring Talomo watershed. These sources are under pressure and the Davao River Basin is likely to be required for water abstraction in the near future. Drinking water Mineral Water Drinking water is water that is intended to be ingested by humans. ...

The Environmental Management Bureau samples 8 sites from the confluence of the Tamugan river downsteam to the mouth of the river. From the Tamugan River confluence with the Davao River down stream to DDF Subdivison, Mandug the water is classified as Class A – Public Water Supply Class II. Downstream of this point to the sea is classified as Class B or recreational water class I. Analyses for dissolved oxygen over the past 4 years has indicated no significant change in quality. The current monitoring of water quality is insufficient to monitor and evaluate pollution levels and trends in the river.

External links

• Basin Properties
• " Pictures

References

• D Hearne, crs, proposal to HELP UNESCO, 2004