Sunday, February 17, 2013

Costa Rica's Volcanism





Hola Readers,

This is my view of the Poás Volcano from when I visited.
Welcome to San Jose! Today we are going to explore outside of the city in Poás National Park, this is the home of the Poás Volcano. The Poás Volcano is a stratovolcano also known as a composite volcano. It is made up of many layers. These layers or strata are composed of hardened lava, tephra, pumice and volcanic ash. The Poás Volcano is currently active and has erupted 39 times since 1828. The volcano was once very explosive and now has many craters. Near the summit of Poás there are two crater lakes the most famous lake is called Laguna Caliente (“Hot Lagoon”) it is known to be one of the most acidic lakes in the world.  The lake sometimes reaches a pH level of almost zero.
On Average this is the view of the Poás Volcano.

Next stop is the Arenal Volcano. The Arenal Volcano is an active andesitic stratovolcano. It is a mix of MAFIC/FELSIC the Arenal Volcano has the cinder cone shape but it also very explosive.  Andesite is an extrusive, igneous, volcanic rock and is a characteristic of subduction zones. The Arenal Volcano is famous for it’s nighttime show of spitting lava into the sky. Most volcanoes in Central America have very thick, viscous lava that is filled with gases and this causes the more violent explosions when they erupt. 

The Arenal Volcano from up close!
This is a picture of the Arenal Volcano that I took using binoculars.
 
The nighttime light show of the Arenal Volcano

So how are these volcanoes formed? The volcanoes in Costa Rica are formed by subduction. The western side of the Caribbean plate subducts the Cocos plate located in the Pacific Ocean.  The more dense Cocos plate currently moves about 10 centimeters per year. 

I hoped this gave you some information about two very interesting volcanoes in Costa Rica. Until next time!

Adios,

Danielle