Natural hazards in Colombia
Natural disasters in Colombia are the result of several different natural hazards that affect the country according to its particular geographic and geologic features. Human vulnerability, exacerbated by the lack of planning or lack of appropriate emergency management, and the fragility of the economy and infrastructure contribute to a high rate of financial, structural, and human losses.
Some of the natural hazards present in Colombia are:
- Earthquakes
- Floods
- Landslides
- Volcanoes
Geologic
Colombia is part of the Pacific Ring of Fire and Andean Volcanic Belt due to the collision of the South American Plate and the Nazca Plate. This produces an increased risk of earthquakes and volcanic eruptions. Some natural disasters of this type are:- The 1875 Cúcuta earthquake
- The 8.2 Tumaco earthquake shook Colombia and Ecuador with a maximum Mercalli intensity of IX, killing 300–600, and generating a large tsunami.
- The 1982 Popayán earthquake
- The 1985 eruption of Nevado del Ruiz volcano and subsequent Armero tragedy
- The 1994 Páez River earthquake
- The 1999 Armenia earthquake that affected heavily the city of Armenia, Colombia in the Quindío department.
Hydrologic
Rainfall is heaviest in the Pacific lowlands and in parts of eastern Colombia, where rain is almost a daily occurrence and rain forests predominate. Precipitation exceeds 760 centimeters annually in most of the Pacific lowlands, making this one of the wettest regions in the world. The highest average annual precipitation in the world is estimated to be in Lloro, Colombia, with 13,299 mm. In eastern Colombia, it decreases from 635 centimeters in portions of the Andean piedmont to 254 centimeters eastward. Extensive areas of the Caribbean interior are permanently flooded, more because of poor drainage than because of the moderately heavy precipitation during the rainy season.The Caribbean Region of Colombia, valleys of Magdalena River and Cauca River and the eastern savannahs are prone to floods during the two main monsoon seasons. The opposite phenomenon of drought is also frequent. January through March and July through September are the dry seasons, when abnormally dry periods cause shortage in the water supply to crops and urban centers.