Guil began the day by saying "The present is the key to
the past." With this in mind, we returned to the Farol de Santa Marta
mountainside to synthesize some of the concepts we had learned over the past
two days to understand the new topic of sedimentation.
Our steep trek up the mountainside included a
surprise: a friendly, 3-legged stray pooch from town followed us into the
field. The 3-legged hound (or Trooper, as we affectionately called him) seemed
to be out hiking all of us. Especially showing off to our 1-legged friend,
Andrew (who had injured his toe in a football match with some locals the night
before).
Our first stop of the hike took us to the high
altitude Sambaqui lookout where Guil gave us the basics. Sedimentation is a lot
like a bad relationship: complicated and lasts for way longer than it should.
It's a process that involves almost every part of the landscape and relies on
complex interactions between energy, distance, and density.
After bioturbating all over the place and coming to
a conclusion on the regulation grain size of sand (.6 - 2mm), the group
ascended one of the large dunes. Little did we know that climbing this dune
would result in one of the greatest geological showdowns this Maymester has
ever seen.

And thus began The Great Dune Debate of 2016. On
which side was the sediment being deposited? Were the deposits vertical, giving
rise to the sheer, cliff-like side? Or were the grains being deposited along
the horizontal, gradually sloped side? After a bloody battle of words and a
cracker-filled lunch, Guil revealed that in fact the women were correct.
Funny how two of those in the winning camp authored
this blog post. But we suppose it's the victors who get to write the history
books.
As our time comes to an end in Farol de Santa
Marta, we are looking forward to the countless adventures and fish dinners that
lie ahead.
ZLAM,
Ali and Carsen
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