Sidoarjo regency as one buffer capital of East Java Province, an area experiencing rapid development. This success was achieved due to various potentials in the region such as industry and trade, tourism, and small and medium enterprises can be packaged well and focused.
With the variety of potential areas and to support adequate human resources, then in its development Sidoarjo could be one of the strategic areas for the development of regional economy.
Sidoarjo District 112 is located between 5 'and 112 9' east longitude and between 7 3 'and 7 5' south latitude. Northern boundary is the municipality of Surabaya and Gresik regency, south is Pasuruan, east of the Madura Strait and the west is Mojokerto District.
With the variety of potential areas and to support adequate human resources, then in its development Sidoarjo could be one of the strategic areas for the development of regional economy.
Sidoarjo District 112 is located between 5 'and 112 9' east longitude and between 7 3 'and 7 5' south latitude. Northern boundary is the municipality of Surabaya and Gresik regency, south is Pasuruan, east of the Madura Strait and the west is Mojokerto District.
Topography:
- Delta plains with an altitude of between 0 s / d 25 m, height of 0-3m with an area of 19,006 hectares, covering 29.99%, an area pertambakkan located in the eastern part
- Middle part of the aqueous region with an altitude of 30-10 meters of freshwater from sea level is the residential areas, commerce and government. Includes 40.81%.
- Western region with a height of 10-25 meters above sea level is an agricultural area. Includes 29.20%
Hydrogeology
Regional groundwater, brackish, and saltwater reaches broad Ha 16.312.69. The depth of groundwater on average 0-5 m from ground level.
Hydrology
Sidoarjo regency is located between two rivers namely Kali Surabaya and Porong River which is a branch of the Brantas River are tipped in the district of Malang.
Climatology
Temperate topis with two seasons, dry season from June to October and the rainy season in November until May.
Soil structure:
Soil structure:
- Alluvial gray area of 6236.37 ha
- Association Alluvial and Alluvial brown gray area of 4970.23 ha
- An area of 29346.95 ha of alluvial Hidromart
- Dark gray Gromosal Covering an area of 870.70 hectares
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