With such fortifications, we headed for the mountains just
outside of town. The plan was to head to
the mountains and ridges to collect on bedrock surfaces. We first drove up
Muskeg Ridge, scanning the bedrock, which was a good sign. We drove up and down logging roads tramping
in logged areas as well as into the forests.
We were all armed with our bear spray, calling out periodically to
prevent a surprise arrival. There were
cobbles in the till but the sandstone bedrock had produced lots of fine
sediment, or the till. The layer of till
was thick, not providing the large boulders.
With no boulders in site we left for a ridge of Flood Mountain. As we were getting ready to checkout a
hillside rain struck. Time to don our
rain gear and head out across a bog and up a hillside. 
We found several boulders. While crossing a bog I saw more Linneas.
Such a treat.
Off next to Grande Mountain.
Hopes were high to find some good boulders. At this point we had five samples. Little did we anticipate the adventure that
awaited us. Last night as we watched the
sun set we had seen lights on the top of Grande Mountain. Today we were driving to its top on its back
side on a road now labeled for all terrain vehicles. It was washed out mountain surface road from
the start. One could only guess the last
time it was graded. The shoulders were
washed out with ditches and boulders and no place to pull over. The grade was steep with sharp switchbacks. The walls of the mountain were
crumbling. We saw an old mine shaft and
seams of coal. Bedrock cropped right
through the road surface and Berto had to carefully maneuver around these
outcrops. This road made the Cow dung
reservoir road to the Hanksville Burpee quarry look like a thoroughfare.
Finally we reached a point with the grade so
steep and the bedrock so prominent like steel ridges; we could go no further
and had to creep back down to a fortunate turn off of an old road long
abandoned. There we left the Ford
Explorer
and headed up the steep grade to walk the last two and a half miles to
the top on foot. The rain in the morning
had filled the ruts and potholes with water.
Fortunately it was sandier than clay, although it was quite greasy. Beds of lupines
flanked the shady side of the
road. Near the top, Alpine flowers now filled
the shoulders. Boulders were found
thickly covered with lichen. We sampled
boulders that were on top of the slope and not on the side where the mountain
would have sheltered.
We spread out,
some to the shoulders were and some to prospect. Jorie and I armed with our bear spray and
calling out announcing our arrival headed for the summit. Clouds were threatening rain and we all kept
our eye on the sky. This was not place
to be if rain were to come. The view was
spectacular as we proceeded up Grande.
The meadows spread to the side of the little road. Forget-me-nots in their rich, rich blue
spread across the wind swept Alpine meadows.
I took pictures of several plants I had not seen before for future
identification. At the top we only found
weathered sandstone bedrock. No
boulders. We returned to the others and
reported the lack of boulders on top. As
Heather finished her notes at the last site, Anders and Berto headed back up to
grab the 4 small cobbles of Gog, a Cambrian quartzite.
Time to head back to the Explorer.
Slowly slowly, Berto crept down the mountain in 4 low
dodging the outcrops and avoiding the washouts.
The 15% grade made it impossible for him to see the road immediately in
front. Anders stuck his head out of the
window to give him directions.
The lack of till or sediment on top was probably a result of
very thin ice flowing over the mountain top, thus hot being produced. The boulders were riding on thin ice
resulting in a localized distribution near the summit but not at the
summit. As we were on our way, Anders
asked, “What did we learn today?”
Heather responded, “Stick to the field plan. We went and did what we came to do and it
worked.”
Tonight Heather and Anders arranged the samples from the
last three days consecutively according to their sequential number of when
collected. The 39 samples were backed in
three Roughneck tubs. To keep the
specimens from slipping sheets are stuffed in the top. Britta will now drive these back to Edmonton
where they then will be shipped to Oregon State University. First load on their way.
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