2. Location
• Ruiz is located in Calderas/Tolima, Columbia
• In the Cordillera Central, Andes Range
• Nevado del Ruiz lies within the Pacific Ring of Fire (convergent boundary)
• The composition of the magma has a high viscosity and silica content
• Like many other Andrean volcanoes, Nevado del Ruiz is a composite or
stratovolcano
• The summit of the volcano has steep slopes inclining from 20 to 30 degrees
• The summit is covered by glaciers, in fact Nevado means “snow covered”
• In the past when this volcano erupts it sends pyroclastic material out and creates a
lahar most of the time, (a possible reason for the amount of glacier at the summit
to decrease over time)
• The capital of Columbia: Bagota is relatively close to Ruiz
• Bagota has a population of 7,155,052
4. Type of Volcano
• Nevado del Ruiz is a composite volcano consisting
of hardened lava including volcanic ash
• Composite volcanoes are created by alternate
eruptions of pyroclastic material and lava flows
• At the summit of the volcano there are glaciers
covering 10 square kilometers of land
• Due to the glaciers a few lahars have been
created in the past
5. Self Created Image of Volcano
• Diagram of Nevado Diagram of
Nevado del Ruiz,
composite
volcano
(Scanned)
By Nic
6. Impact
• The benefits of the volcano include tourist
destination, provides a beautiful aspect to the
land, and it is home to the mountain tapir and
spectacled, both of which are ‘threatened’
• Some major dangers include another lahar,
pyroclastic material causing physical damage
to buildings, and the possibility of lowering
temperatures in a violent eruption
8. Monitoring the Volcano
• What is being used to monitor the volcano
cannot be found
• However a few methods that could be used to
monitor Ruiz would be a tiltmeter: to measure
the slope of the cone, or a seismograph
measuring the earthquakes created by volcanoes
• The steeper the measure of the slope the more
likely there is to be an eruption
• The more intense and the higher number of
earthquakes the more likely there is to be an
eruption
10. Eruptive History
• The first eruptions of Nevado del Ruiz occurred about 1.8 million years ago. Three
primary eruption periods in the history of the volcano have been identified:
ancestral, older and present. During the ancestral period between one million to
two million years ago, a complex of large stratovolcanoes was created. Between
1.0 million and 0.8 million years ago, they partially collapsed, forming large (5–
10 km wide) calderas. During the older period, which lasted from 0.8 million to 0.2
million years ago, a new complex of large stratovolcanoes developed (including
Older Ruiz, Tolima, Quindio, and Santa Isabel). Once again explosive summit
calderas formed from 0.2 million to 0.15 million years ago.
• On the morning of March 12, 1595, Nevado del Ruiz erupted. The volcano erupted
pyroclastic material including lapilli and pumice bombs. Additionally, the eruption
created a lahar was created killing more than 600 people
• The worst recorded quake as far as casualties was at Amero on November 13, 1985
killing 23,000 civilians and more than 10,000 animals
• The most recent eruption was in 2008, it was a minor one
