Cotopaxi


Cotopaxi is an active stratovolcano in the Andes Mountains, located in the Latacunga canton of Cotopaxi Province, about south of Quito, and northeast of the city of Latacunga, Ecuador, in South America. It is the second highest summit in Ecuador, reaching a height of. It is one of the world's highest volcanoes.
Since 1738, Cotopaxi has erupted more than 50 times, resulting in the creation of numerous valleys formed by lahars around the volcano. The last eruption lasted from August 2015 to January 2016. Cotopaxi was officially closed by the authorities to climbing until it reopened on October 7, 2017.

Description

On a clear day, Cotopaxi is clearly visible on the skyline from Quito. It is part of the chain of volcanoes around the Pacific plate known as the Pacific Ring of Fire. It has an almost symmetrical cone that rises from a highland plain of about, with a width at its base of about. It has one of the few equatorial glaciers in the world, which starts at the height of. At its summit, Cotopaxi has an wide crater which is deep. The crater consists of two concentric crater rims, the outer one being partly free of snow and irregular in shape. The crater interior is covered with ice cornices and rather flat. The highest point is on the outer rim of the crater on the north side.

History

Name

Many sources claim that Cotopaxi means shining pile or mountain in an indigenous language, but this is unproven. According to locals who speak Quechua, “coto” means neck and “paxi” means moon. This refers to the crater of Cotopaxi that looks like a crescent moon. The mountain was honored as a "Sacred Mountain" by local Andean people, even before the Inca invasion in the 15th century. It was worshiped as “rain sender”, which served as the guarantor of the land's fertility, and at the same time its summit was revered as a place where gods lived.

Historic eruptions

With 87 known eruptions, Cotopaxi is one of Ecuador's most active volcanoes. The first recorded eruption of Cotopaxi was in 1534.
Cotopaxi's most violent eruptions in historical times occurred in the years 1742, 1744, 1768, and 1877. The 1744 and 1768 events destroyed the colonial town of Latacunga. During the June 26, 1877 eruption, pyroclastic flows descended on all sides of the mountain melting the entire ice cap, with lahars traveling more than 100 km into the Pacific Ocean and western Amazon basin draining the valley. The city of Latacunga was again leveled completely due to the mudslide deposits.
The eruption on 19 June 1742 was witnessed by the scientists Pierre Bouguer and Charles-Marie de La Condamine, members of the French Geodesic Mission, as they descended from nearby Guagua Pichincha.
– products of different types of eruption at Cotopaxi
There was a major eruption from 1903 to 1904, and minor activity persisted until at least 1940 and possibly 1942. The same source also reported increased thermal/seismic, non-eruptive activity in 1975 and 2002. In the increased activity of 2002, fumarolic activity and sulfuric emissions increased and ice around the inside and on the southeastern side of the cone started to melt. However, no actual eruption was observed.
In 2015, two large phreatic eruptions on the morning of August 14 marked a new phase of volcanic activity. The volcano "remains in a very abnormal situation. In August, 2,100 earthquakes were recorded and emission rates of sulfur dioxide reach approximately 20,000 tonnes per day". The government estimates some 300,000 people are at risk from the volcano in the provinces of Cotopaxi, Tungurahua, Napo and Pichincha.

Climbing

The first European who tried to climb the mountain was Alexander von Humboldt in 1802; however, he only reached a height of about. In 1858 Moritz Wagner investigated the mountain, but he could not reach the summit either.
On November 28, 1872, German geologist Wilhelm Reiss and his Colombian partner, Angel Escobar, finally reached the summit of Cotopaxi.
In 1873 it was summitted by German Geologist Moritz Alphons Stübel and four Ecuadorians, Rafael Jantui, Melchor Páez, Vicente Ramón and Eusebio Rodriguez.
In 1880 British mountaineer Edward Whymper and the Italian guides Jean-Antoine Carrel and Louis Carrel made the third recorded ascent of Cotopaxi and spent a night on the summit.
Painters and Hans Meyer reached the summit in 1903, and many of Reschreiter's paintings feature a view of Cotopaxi.
In the late 20th century, summiting Cotopaxi became a major tourist draw. The José F. Ribas Refuge was built in 1971 at an elevation of and enlarged in 2005.
A tragedy occurred here on Easter Sunday 1996 when an avalanche partially buried the Refuge and dozens of tourists. The glacier above the Refuge was probably weakened by an earthquake that had shaken the entire Province of Cotopaxi for several days prior to the avalanche. In the warm midday sun a huge portion of the ice wall broke loose. Being Easter, there were many day visitors on the mountain who were buried in the ice and snow. Those trapped in the Refuge broke windows on the downhill side to climb to safety, but 13 people died on the slope above. The Refuge itself is located in a valley and consequently vulnerable to future avalanches.

Today

Recreation

Climbing Cotopaxi to the summit is quite popular, with up to 100 climbers attempting it on weekends. Today, mountain guide companies offer regular guided climbs of the mountain. Climbers grade the conventional route alpine PD or WS — or PD/WS+. Use of crampons and ice axes is mandatory as snow and ice slopes of up to 50 degrees are encountered, and climbers should be on belay and use aluminum ladders to cross one or two of the crevasses. A 4WD track goes up from the national park entrance to a carpark at 4600 m altitude on north side, just below the José F. Ribas Refuge. This stone mountain hut — owned and operated by Grupo Ascensionismo del Colegio San Gabriel — is situated 200 m higher at 4800 m. Here climbers can spend the night and begin their summit bid in the early morning without any intermediate camps. Summiting normally starts around 12:30 am, to reach the summit at latest 7:30 am and then return to the hut before the snow melts and glacier crevasses move/evolve. As of July 28, 2014, the Ribas Refuge is under construction. Tour operators shuttle their clients up to the top of the 4WD track once in the afternoon for a glacier skills class, and then again to start the climb around midnight, spending the intervening hours eating dinner and resting at a hostel lower down by the lakes. Adventure tourism operators in Quito also offer mountain biking tours from the Refuge downhill along the dirt track.

Recent activity

In April 2015, the volcano began to show signs of unrest, and came back to life. There was a large increase in earthquakes and SO2 emissions. IGEPN reported slight deformation of the edifice, suggesting an intrusion of magma under the volcano. As of 25 July, the unrest continued, and the most recent significant eruption was a phreatic eruption that occurred on August 14 and 15, 2015. Ash was deposited heavily in areas close to the volcano, including damaging farmlands on the flanks of neighbouring volcanoes such as El Corazon, and thinly as far as Quito, affecting southern and central areas of the city.
Future Cotopaxi eruptions pose a high risk to the local population, their settlements and fields. The main danger of a significant eruption of Cotopaxi would be the flash-melting of its summit glacier, resulting in devastating lahars which would travel down the flanks of the volcano, guided by river valleys whose origins lie at the volcano. Danger from normal, explosive eruptive activity is limited to within Cotopaxi National Park. However, the great distances that lahars of the significant size that Cotopaxi's glacier produces could travel, greatly increase the hazard areas to include all river valleys leading from the volcano. If there were to be a very large explosion, it would destroy many of the settlements within the valley in the suburban area of Quito. Another city which would be in great danger is the regional capital Latacunga, which is located in the south valley, and has been destroyed at least twice in recent history by lahars caused by volcanic activity.

In art

, 1862.