HSOC Corridor Information
From Missouri Outdoor
Rockwoods Reservation
By Conor Watkins
Rockwoods Reservation, a natural area administered
by the Missouri Department of Conservation (MDC),
is an enjoyable outdoor retreat for those looking
to escape the hurried life of St. Louis. Even
though Rockwoods Reservation is located near metropolitan
St. Louis, it is heavily wooded and home to a
variety of wildlife species including fox, bobcat,
squirrel, chipmunk, skunk, deer, raccoons, opossum,
wild turkey, bobcat, lizards, bats, salamanders,
frogs, birds, and snakes. As with much of Missouri,
Rockwoods is an excellent example of a karst terrain
where groundwater has dissolved some of the limestone
bedrock. The area is home to several small caves,
springs, a natural bridge, and losing streams
(streams that lose water into the groundwater).
The area also shows evidence of extensive lumbering
and mining/quarrying, which went on in the past.
New visitors to the area should start by investigating
the main office/museum provided by the MDC. This
building provides information on the history,
attractions, and wildlife of the area. Pictures
of the area during the mining days are on display
at the office. Young children will especially
enjoy the exhibits where one is allowed to touch
animal bones, skins, and other natural artifacts.
Some aquatic wildlife is on display in a tank
along with some stuffed mammals that inhabit the
park. No visit to the office building is complete
without a stop at the talking and moving Smokey
The Bear, which can be activated by the push of
a button. This attraction is viewable through
an outside window of the building and is located
on the on the south end of the office. Smokey
randomly tells stories, sings songs, and gives
advice on how to prevent forest fires and is usually
a hit with children. Feeders for songbirds and
hummingbirds are also present outside the office.
The area is planted with native flowers and vegetation.
If planning a hike, pick up a map of the area
at the main office. An intermittent spring (one
that flows in wet weather) is located behind the
office at the edge of the woods. It soon disappears
into a karst swallow hole. Picnic areas are provided
near the office and scattered throughout the rest
of Rockwoods along the main road.
Rockwoods provides six main trails ranging in
length from 300 yards to 3.25 miles. The shortest
trail is the Wildlife Habitat Trail. This trail
is flat and is an excellent choice for families
and the handicapped. The area near the trail is
complete with handicapped parking, picnic, restroom
facilities, and is wheelchair accessible. The
trail also features an interpretive brochure pointing
out around ten sites of interest along the trail.
The Prairie Trail is 500 yards long and passes
through a grassland prairie complete with native
prairie vegetation. Controlled burns help simulate
a natural environment back when man didn't put
out wildfires. This trail is also flat but not
suitable for wheelchairs.
The Trail Among The Trees is a hilly 1.5-mile
long trail complete with an interpretive brochure.
The trail takes the visitor through a rocky glade,
forested uplands and lowlands, through valleys,
quarried areas, and a small cave. The cave, known
as Bathtub Cave, is good for beginners. The cave
is small and it would be nearly impossible to
get lost. There is also minimal water and mud.
The cave's close proximity to the trail has made
it a target of vandals. Many formations have been
broken off and names have been spray painted on
the walls. Karsted rock along the trail is noticeable
because of its resemblance to Swiss Cheese. An
excellent view of the Rockwoods area can be seen
from an overlook at the rocky glade. This view
is good at sunset because of its west facing aspect
(exposure). Another interesting part of this trail
is the fact that this area was once quarried for
its limestone. Evidence of this appears in the
drill holes in the cliffs where dynamite was inserted
to blast the rock apart. An old rail bed, made
of piled up rocks, was once used to haul away
quarried rock and is still visible within the
valley. The beginning and end of the trail is
paved with asphalt and relatively flat but the
middle section of the trail is not paved and consists
of steep grades and stairs. A small spring is
present in Hamilton Creek directly across from
the office near the beginning of this trail.
The Rock Quarry Trail is two miles long and
has scenery very similar to the Trail Among The
Trees. It is paved with soft white gravel and
complete with an interpretive brochure. The trail
is very hilly and offers excellent views of the
old quarry remnants. The rail bed is still present
along with foundations of other structures. Two
small 'caves' are located near this trail. These
rock shelters are not natural caves, but remains
of the old quarry created by dynamite. Metal and
wooden parts such as rails, railroad ties, and
the associated hardware were haphazardly left
in these caves and are still present.
The Lime Kiln Trail is the longest and most
rugged looping trail in Rockwoods. It is hilly,
has a rough unpaved surface, and is around 3.25
miles in length. An old lime kiln is present at
the beginning of the trail. The trail also passes
by Hamilton Spring, a large spring also visible
from the main road through the area.
At ten miles in length, the Green Rock Trail
is Rockwood's longest trail and is the only trail
in the area that does not form a loop. This trail
is hilly, scenic, and ends up in the nearby Greensfelder
County Park. The trail has a small side loop within
Rockwoods.
Casual vistors to present day Rockwoods Reservation
would find it hard to believe that the area was
a barren wasteland only fifty years ago. In the
past, the land was stripped of its trees, rock,
and soil. The first sustained human use of the
area was by the Hamiltons, a pioneer family who
settled there in 1800 when the land was still
under Spanish rule. Although they left little
or no evidence of their presence, a creek, spring,
and the valley containing the road through Rockwoods
bear their name. After the head of the household,
Ninian Hamilton died in 1828, the family moved
on and the area was sold to migrants who farmed
the valleys and low slopes. The steep slopes were
left forested. Farming changed the hydrology of
the area, which caused small springs and Hamilton
Creek to dry up. Much of the area remains this
way today. Nearby towns such as Pond and Glencoe
sprang up as distribution centers for the agricultural
goods from the Rockwoods area. Landmarks such
as the Pond Hotel still stand.
By 1854 the Woods-Christy Lumber Company from
St. Louis had bought up most of the land in Rockwoods.
In three years they stripped the area of its valuable
white oak timber and left it barren and eroding.
In 1857 the lumber company sold some of the land
back to farmers and attempted to sell the rest
of the area as a subdivision geared toward wealthy
businessmen from St. Louis. Due to the remote
location of the area and the barren landscape,
this business venture was a failure and was scrapped
in 1868.
Quarrying, which started in 1868 was the last
major industrial use of the Rockwoods area. The
Cobb-Wright-Case Mining Company (later known as
Glencoe Lime Company) had previously heard rumors
that the site held deposits of marble. This 'marble'
actually turned out to be a very high-grade limestone
from the Plattin Formation with far joint (fracture)
spacings. The company was able to sell the rock
as marble. Blasting was not used to remove the
rock at this site since the rock was used in construction
and was best used in large intact pieces. Steam
powered saws were used to cut ten foot cubes of
rock from the cliff face. These large cubes were
then cut into more manageable sizes and loaded
onto rail cars. The rock was then transported
to St. Louis on a spur line that connected to
the main Missouri-Pacific rail line in nearby
Glencoe. This high-grade limestone originated
mostly from the southern end of the current day
Rockwoods Reservation. As soon as quarrying started,
the valley near the present day office changed
into a company town.
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Once the remaining Plattin
Limestone was no longer profitable to mine,
the miners turned to quarrying the lesser
grade Kimmswick Limestone. This rock of
this formation was only suitable to make
lime, which is used in fertilizer or cement.
Blasting was the chosen method of removal.
Six locations were quarried. All that remains
of these quarries are sheer cliff faces
with vertical drill holes for sticks of
dynamite. In at least one location the miners
turned to underground room and pillar mining,
mainly to avoid having to remove overlying
'junk rock', which left the present day
Cobbs Cavern. The mine is large. It is around
two stories in height and larger than a
football field in area. It is unfortunate
that this impressive feature was recently
closed for fear that parts of the roof were
becoming unstable and might collapse. The
trail to this site is closed too, but the
mine can be viewed from the Rock Quarry
Trail at a distance. This is best done in
the winter when the leaves are down.
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All this quarried limestone
was kilned and reduced to lime on site. During
the early stages, this was done with four
large kilns built of local rock and lined with
high temperature firebrick. The kilns were loaded
with wood and coal (once all the locally available
trees had been cut). The high heat chemically
altered the limestone to lime, which is lighter
and easier to ship than an equivalent amount of
limestone. Six metal kilns, which are no longer
at the site, were added later on. Only one crumbling
rock lime kiln, now reinforced with metal rods,
still exists.
Gravel and clay/shale were mined from the northern
part of the area. The gravel was used in road
construction while the clay was used for clay
pipe and low-grade terra cotta. This site now
resembles a huge (800 feet across) sinkhole and
has strange eroding clay formations inside.
The Glencoe Lime Company went broke in 1938
after 70 years of mining in the area. In order
to recoup some of its costs, the mining company
sold its land to the state for $30 an acre. The
land was then placed under the jurisdiction of
the MDC, which has done an excellent job of reforesting
the area. Although evidence still exists, one
would find it hard to believe that the area was
once ravaged and barren. The area's return to
its current state proves that nature is very strong
and can recover from almost anything, given enough
time. To get to the area, take I-44 east from
Rolla to Eureka exit number 264. Turn left and
follow Hwy 109 3-4 miles north to Rockwoods, which
is located on the left. Visitors who enjoy the
area should also check out nearby Greensfelder
County Park, Rockwoods Range, or Babler State
Park.
Thanks to the Missouri Conservation Department
(http://www.mdc.mo.gov/),
MDC literature available at the site, "A Brief
History of Rockwoods Reservation" by Steve Wyatt,
and users of the MOCAVES listserve for some of
the information presented here.
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