The Mocoa landslide was a natural disaster that took place in 2017. During the pre-dawn hours of 1 April 2017, locally heavy rain triggered flash flooding and landslides in the city of Mocoa, Putumayo, Colombia, killing at least 254 people, injuring 332, and leaving 70 others missing. It is the third-deadliest weather-related disaster in Colombian history, and is regarded as the worst catastrophe in the history of Mocoa.
|2017 Mocoa landslide|
2017 Mocoa landslide (Colombia)
|Date||1 April 2017|
|Time||≈3:00 a.m. COT (UTC−05:00)|
|Type||Landslide, flash flood|
Situated in the Andes, the department of Putumayo is notorious for deadly landslides. The region's mountainous terrain and frequent rainfall makes it prone to such disasters. Much the same as the Himalayas, the Andean mountains in this region have ultra steep drops, from over 5,000 meters to 500 meters within 50–100 km, with that kind of drop, heavy rains tend to take boulders at high speeds along with them (locally called huaycos), not just water. Throughout much of the first three months of 2017, the northwestern coast of South America saw above-average rainfall, leading to deadly floods in Peru and Ecuador. The rainy season in Colombia typically begins in mid-March and continues through mid-June. March 2017 proved unusually wet, with areas around Mocoa receiving 150 percent the average monthly rainfall.[nb 1]
On 31 March 2017, moist tropical air from the Atlantic Ocean flowed west across the Amazon toward the Andes. A broad swath of ample precipitable water, or atmospheric moisture, extended across this region. During the evening hours, a slow-moving mesoscale convective complex developed within this region and produced heavy rainfall in southern Colombia. Infrared satellite imagery from GOES-13 depicted cloud tops of −90 °C (−130 °F), indicating the storms were capable of producing torrential rain. With the system moving perpendicular to tall mountains, orographic influence likely enhanced rainfall and further contributed to the subsequent disaster. According to residents, the rain became particularly intense between 11:00 p.m. and 1 a.m. local time. A total of 130 mm (5.1 in) of rain fell during the event, largely within a few hours. This caused the Mocoa, Sangoyaco and Mulato rivers to overflow and send mudflows towards residences and infrastructure in the city of Mocoa by 3:00 a.m.
Neighborhoods built along the banks of the aforementioned rivers were completely devastated. Numerous poorly constructed homes were leveled, and large portions of the city were left buried in several feet of mud. The disaster adversely affected 17 of the city's neighborhoods, with the mayor of Mocoa, José Antonio Castro, stating some areas "[had] basically been erased". The Independencia neighborhood was entirely destroyed. Approximately 45,000 people were directly affected throughout the city.
At least 329 people are known to have died in the disaster. An additional 332 were injured and a further 70 were missing. At least 22 of the injured were in a "delicate health situation" and transferred to Neiva. Another 21 victims were flown to Popayán.
President Juan Manuel Santos declared a state of emergency and stated that his "heart and the hearts of all Colombians are with the victims of this tragedy." More than 1,100 soldiers and police officers deployed to assist in search and rescue efforts. Santos labeled the incident "a disaster caused by nature, by climate change." A temporary morgue was established to handle the large number of deceased. The Colombian Red Cross activated its National Crisis Room in response to the disaster and deployed a team of 47 people to assist in recovery. Hospitals in the city were overwhelmed with the influx of patients, and much of the area was left without power and water.
By 2 April, more than 2,500 personnel — including 1,400 soldiers and 800 police officers — were scouring debris for survivors. The army provided 63 vehicles, 10 helicopters, 7 boats, and 6 planes for the rescue operation. Médecins Sans Frontières deployed an assessment team to the affected area on 2 April.
Farc rebels offered to help rebuild town.
The term landslide or less frequently, landslip, refers to several forms of mass wasting that include a wide range of ground movements, such as rockfalls, deep-seated slope failures, mudflows, and debris flows. Landslides occur in a variety of environments, characterized by either steep or gentle slope gradients, from mountain ranges to coastal cliffs or even underwater, in which case they are called submarine landslides. Gravity is the primary driving force for a landslide to occur, but there are other factors affecting slope stability that produce specific conditions that make a slope prone to failure. In many cases, the landslide is triggered by a specific event (such as a heavy rainfall, an earthquake, a slope cut to build a road, and many others), although this is not always identifiable.List of landslides
This list of landslides is a list of notable landslides and mudflows divided into sections by date and type. This list is very incomplete as there is no central catalogue for landslides, although some for individual countries/areas do exist. Volumes of landslides are recorded in the scientific literature using cubic kilometres (km3) for the largest and millions of cubic metres (normally given the non-standard shortening of MCM) for most events.