Very often we view the changing of a landscape in terms of a
great deal of time. Mountains for example are formed in seismic events and then
eroded and weathered with hundreds and thousands of years of Mother Nature
sculpting the meticulous details of one of these earthen wonders. One of the
greatest sculpting tools Mother Nature wields is water. This is why a river can
change much faster than a mountain.
Years ago I learned how a meadow is formed: Water picks up
minerals from the earth and deposits them on the sides and at the end of a
meandering river. Eventually it completely fills the river forming a meadow,
filling with local vegetation and ready for life to inhabit the area. I good way to
view this happening is our very own Provo Bay.
Satellite view of Hobble Creek and Mill Race
Years ago I grabbed this satellite image of this area to research
the possibility of a paddle down Hobble Creek and back up Mill Race. You can
see at the bottom how Hobble Creek feeds into Provo Bay and at the top you can
see a gaping wide opening to Mill Race. It was a successful paddle with the
help of a few Utah County Kayakers and their adventurous spirits, in spite of a
few scary lightning strikes. The water that year was even higher than this
image projected. In fact, I got a little lost looking for the mouth of Mill
Race in a confusing fragmite jungle.
Because of proximity to my home I frequently kayak Mill
Race. It very easy access for me and I don't have to plan a put in and take
out. It is a river that can be entered and exited at the same place. I can do
this solo or invite friends. A few weeks ago I took my friend Colton to the
mouth of Mill Race. The water was low that day and when we reached the end a
sand bar was blocking the entrance into Utah Lake. I thought to myself that
when the water gets higher I will be able to kayak into the lake once again.
Here is a picture comparison to the same spot:
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