| "As a geochemist, volcanoes are excellent places to retrieve data
and learn about geological processes" claims Varekamp. "Volcanology is
one of the few areas in earth sciences where you can actually see things,
like the uplift of mountains, on a human time scale. In a lava flow, a
big eruption, or an acid river, you can really link the results you get
much easier in volcanology to a longer time scale." Varekamp explains how
this was particularly relevant to his most recent expedition in Argentina.
"We sampled a boiling lake, and everything that comes with it. We see that
the watery interface between the magma adapts with the outsides, because
it has a glacial top, which is melting. So, you are looking at this contact
with the exosphere and the interface with the magma just under that. This
is the area where most ore deposits form, so we are basically looking at
a natural laboratory of ore formation at a time scale which is of course
too slow to calculate day to day, but we can still calculate over the years
that we work there, how much of the volcano is being dissolved by the gaseous
waters, and how much metal is being taken up." The Earthís crust continually
recycles elements from the ocean and mantle. The volcanoes show these same
characteristics on a much shorter time scale. He claims that you can understand
the evolution of solid earth by scaling the processes of a volcano to a
larger time scale.
Studying volcanoes has taken Professor Varekamp to some very
special, extraordinary and often remote areas. He studied on a 70-person
crew boat in Indonesia for many years. There, he traveled to some islands
where the natives had not seen white people for decades. He later led an
exploration for three months back to Indonesia to work on a volcanic arc.
"It was the biggest thing I had ever done and I will probably never do
anything quite as big as that again." In Indonesia, he first got interested
in acidic lakes that sometimes accompany volcanoes. These lakes had a pH
level of about 0, the same as battery acid. Accompanied by several Wesleyan
students, Varekamp returned to Indonesia to further study these acidic
lakes. He discovered that by monitoring the local river system,you could
understand the volcano in terms of its lake water.
| Varekamp has recently traveled
to the Andes to study another almost boiling acidic lake. He understands
that doing research on these lakes may provide more reliable data on the
gases of a Volcano than actually sampling the gases. "In the old days,
I would take a sample with a vacuum bottle of volcanic gas, but it was
a 10 second sample of something that is streaming all the time. You always
wonder how representative that one sample was. However, crater lakes collect
and integrate the same elements over 50 years, which then start over after
further eruptions. In crater lakes, there is a much larger time signal.
That is a better way of looking at volcanic gases." |
| The Rio Agrio on the Copahue Volcano has a pH ~ 0.5. |
|
Although his studies in Argentina will probably end in 2 years, Varekamp
plans on returning. "I will probably keep working in the Andes because
Argentina is a great country to work in; I like it a lot. There are still
many unexplored areas and topics, so next time I go there, I will explore
a little more in the Patagonia region to see what I can find. I see myself
working in the Andes for some time to come."
Although Varekamp was experienced in volcanology, he teaches a wide
variety of courses in the E&ES Department. "When I got hired, they
said, "So, this volcanic stuff is nice, but you also got to do something
environmental because the Earth and Environmental Science program has got
to come off the ground." Johan then began to work on heavy metal pollution
in the wetlands and coastal marshes around Middletown. After conducting
detailed experiments on a wide array of variables, he realized that his
team could do more by studying sea level rise. Relative sea level rise
can be indicated by sampling sediments and may provide clues to the climate
at the time they were deposited. Johan commented, "Holland is flat, virtually
at sea level. So, basically sea level research would have been a lot more
appropriate than volcanology (in Holland), but I never studied sea level
rise until I came to the US." |