While staying in a small town called Oakley, Kansas,
which is located along I-70 in the northwestern part of the
State, I saw a sign indicating Monument Rocks 20 miles south of
the town on US 83. Having a picture of the land around our
campground, which was flat farmland, the sign piqued my
curiosity. So armed with camera in hand we jumped in our trusty
truck and went in search of the Monument Rocks. I pictured some
little rocks that someone had put there to amuse/entertain the
tourists. Well, I couldn't have been more mistaken. After
reaching a sign indicating Monument Rocks down a side dirt
road, we drove for about 4 miles and I got the surprise of my
life. There, in the middle of several corn fields, rose several
very large rocks as if pushed up out of the soil. I found out
that the Monument Rocks, as they are called, are really remnants
of layer after layer of Cretaceous seabed, the wind-carved,
water-eroded chalk pinnacles rise some 70 feet above the
plain. This natural formation served as a landmark for pioneers
and American Indians. Weathering has revealed a great
variety of
marine and reptilian fossils. Chalk bluffs and
similar formations are characteristic of the Smoky Hill River
Valley from this region east to Cedar Bluff Reservoir. As we
approached closer to the rocks (you can get right up to them, as
there are no barriers of any kind) I was able to see pieces of
sea life embedded in them. I found myself wondering if there were
other "Monument rocks" anywhere around. But you could
see no other large rocks anywhere on the horizon. The land had
again reverted back to miles and miles of farm land. As we drove
away my experience left me with several unanswered questions: Why
had these particular rocks remained? Had others been nearby and
had been removed hundreds of years ago? I guess only a geologist
could tell you for sure, but it certainly left me with a
different view of Kansas.
Laura