Fox Glacier |
an idea of how quickly the glacier is melting |
foot of Fox Glacier |
vibrant algae in glacier pool |
edge of the glacial valley |
Franz Josef up close |
What makes NZ so famously beautiful is mainly due to the
work of glaciers. The impressive mountains that plunge into Sounds or Fiords
(deep, skinny, lake-esque bays) are the result of glaciers sliding past at the
incredible pace of 24 feet a day. The gorgeous meadows that stretch through the
valleys grow where glaciers once were. After shaping these two islands for thousands
of years, only two glaciers remain. We first visited Fox glacier, the smaller
of the two. After a 30-minute walk up the glacial valley we were at the foot
starring up at an alarmingly small patch of ice. In the glacial stream that
pours out from underneath the ice there were huge chunks of ice that have been
breaking off. We then drove 20K to the Franz Josef Glacier, which is
significantly larger. It stretches so far back into the mountain range that you
cannot see the end of it. The deep ice reflects a beautiful brilliant blue
light. The valleys are full of small rock that has been crushed off the
mountains by the glacier making it look more like a gravel yard than a natural
wonder. We feel lucky to have been able to see these before they are forever
gone. But I couldn’t help but feel a deep sadness as we passed the markers of
where the glacier used to be just a few decades ago.
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