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This volcanic explosion
was only 1300 years ago and The Flow comprised of black pumice, white pumice
and black obsidian (the difference between pumice and obsidian is basically the
amount of bubbles in the silicon). It
was fascinating to see the obsidian sparkling in the sunlight.
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Then we headed down to Crater Lake National Park about 50
miles further south. We found a nice
camp site in the Umpqua National Forest, right by Diamond Lake, looking up at
the snow covered Mt Bailey.
After lunch we drove into Crater Lake NP which, at 7000ft and above, was covered in snow. In fact there was so much snow we were unable to access half of the park as the roads were closed. What we did see looked beautiful in the sunshine.
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After a couple of hours in the park we headed home as the
weather was starting to close in and dark clouds blocked the sun.
28th September – Oregon Scenic Byway
It had rained most of the night and when we woke we could
barely see the lake due to the mist. Setting
off in the morning was hindered by the retractable steps up into the RV not
retracting! Paul’s skills with the
hammer came in handy once again! (Keeping
his hand in for the next Hammerslagen!).
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create a swirling pool.
From Glide we left the forested scenery and continued to
follow the Umpqua River via a rural road through pastoral country onto the
campground at Sutherlin. Here we met up
with our friends, Duane and Tami, who we had befriended in Tucson back in
March.
29th September – Sutherlin
We had planned to continue our journey west, to the coast,
but the weather forecast predicted the remains of a Tropical Storm bringing
torrential rain and high winds to the Oregon coast. So we decided to chill out at the
campground. It rained most of the day!
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