| Bicol River | |
| Map: | Bicol river watershed.png |
| Pushpin Map: | Luzon mainland#Philippines |
| Pushpin Map Caption: | Bicol River mouth |
| Subdivision Type1: | Country |
| Subdivision Name1: | Philippines |
| Subdivision Type2: | Region |
| Subdivision Name2: | Bicol Region |
| Subdivision Type3: | Province |
| Subdivision Name3: | Camarines Sur |
| Subdivision Type4: | Cities |
| Length: | 94km (58miles) |
| Discharge1 Location: | San Miguel Bay (when the sea level is low) |
| Discharge1 Min: | 123m3/s |
| Discharge1 Avg: | 165m3/s |
| Discharge1 Max: | 205m3/s |
| Source1: | Lake Bato |
| Source1 Location: | Bato, Camarines Sur and Libon, Albay, Bicol Region |
| Source1 Coordinates: | 13.3319°N 123.3589°W |
| Source1 Elevation: | 6m (20feet) |
| Mouth Location: | Between Cabusao and Calabanga, Camarines Sur, Bicol Region |
| Mouth Coordinates: | 13.7167°N 123.1069°W |
| Mouth Elevation: | 0m (00feet) |
| Basin Size: | 3770km2 |
The Bicol River is the eighth largest river in the Philippines in terms of drainage basin size with an estimated catchment area of . The river drains a large part of southwestern Bicol Peninsula of the island of Luzon and passes through Camarines Sur province.[1]
The river starts from Lake Bato, above sea level, and flows downstream to its estuarine mouth at San Miguel Bay. It passes through Naga City, the alluvial and coastal plains of the vast Bicol Valley, an elongated, northwesterly trending depression in the Bicol Region, which contains alluvial plains to the coastal plain. Average slope within the river's drainage basin is 0.006%.
The basin has an influence area of including its drainage basin. It lies between 13°0 to 14°N and 123°0 and 124°0 E. It is extensively a coastal flood plain.
The Bicol River is bounded on the northeast by the Bicol Cordillera, which consists of a chain of volcanic mountains including Mount Iriga, Mount Malinao, Mount Masaraga and Mount Mayon. On the southwestern side lie the Ragay Hills, which consists of folded and faulted sedimentary formations including limestones, siltstones, conglomerates and shale. In between these higher areas lies the Bicol plain, which is composed of thick alluvial deposits of sand silt and clay.[2]
The main geo-morphological features found in the area include the estuarine plain, a river flood plain, the piedmont plain and the valleys of incised creeks. The estuarine plain is level to nearly level and consists of fine fluvial-marine deposits over sandy layers with marine shells. The fluvial marine deposits are usually saline at depths of approximately and includes depresses areas along the Bicol River. The river floodplain is made up of mixed alluvium. The piedmont plain on the fringe of the Ragay Hills consists of fine alluvium clay and reworked colluviums.
The climate is influenced by the Northeast Monsoon winds and the Pacific trade winds. These Monsoon winds create the low pressure area in the Pacific Ocean, resulting in tropical cyclones that affect the area in November and December.
Rainfall occurs throughout the year with low rainfall between January and May and high rainfall between June and December. In the lower basin, mean annual rainfall ranges between 1850and. The main factors influencing rainfall are the air streams, the intertropical convergence zone and topography.
The mean temperatures are high throughout the year with the daily mean temperatures in the range of 24.1to and an annual mean temperature of .
This is listed from mouth to source.