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We are now back in the lab analyzing the results. Please stay tuned!

 
 

 
 

 
 

 
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Introduction

Introduction

Introduction
Central America
A Collaborative Study
The Earth's surface comprises a number of tectonic plates that are in continuous motion relative to one another. The plates diverge or are pulled apart at spreading centers allowing new material to well up from the mantle
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and to form oceanic crust. Plates come together or converge at subduction zones which mark the locations where one plate plunges beneath another, returning crustal material to the mantle. The continuous movement of the plates therefore acts to recycle material between the Earth's crust and underlying mantle. This expedition is about volatile recycling along the Central American subduction zone and involves a number of scientists using different techniques in a collaborative approach. Read on!

Central America>>

 

 

 

 
  Daily Log  
 
January 2001
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