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Boyce-Mayview Park
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Nature Journal: Hikes through the Old Mayview
Property
by Chuck Tague
October 23, 1998, 9:30 am. Tracey Buckman and I
scouted the Mayview property for a USC
Citizens for Land Stewardship outing the following day. Along the ridge
overlooking
Chartiers Creek I noticed a leaf on the ground that resembled an
american chestnut leaf. I
found several others including some attached to a twig. Several side
buds clustered around
the end bud on the twig indicating a species of oak. The leaves pointed
lobes, however,
disqualified my first guess -- the round-lobed chestnut oak. The field
guide identified it
as a chinquapin oak or yellow oak, Quercus muhlenbergii.
We located several chinquapin oaks, all along the
slope just above the flood plain. We
also found pignut hickory and a bitternut hickory growing on the base
of the slope. On the
flood plain we located some small papaws, several american basswood
trees, hackberry trees
and a large american elm. Tracey showed me an old sycamore with two
huge trunks. As we
left, a flock of at least nine wild turkeys scattered in all
directions. I had never
before come across chinquapin oak. To learn more about its occurrence
in Western
Pennsylvania I looked it up in Wild Flowers of
Western Pennsylvania and the Upper
Ohio Valley, (O. E. Jennings, University of
Pittsburgh Press, 1953) Jennings
wrote:
This is a large and abundant tree in the
Mississippi basin, but eastward more
largely confined to limestone soils . . . In our region this species is
rather rare and
local with usually only a few, often only a single tree, in any 1
locality, excepting the
limestone regions of Central Pennsylvania, where it is more common . .
..
Near Beadling, SW Allegheny County, in a broad
ravine below a limestone outcrop, Mr. and Mrs.
E. J. Mason discovered a number of large trees of this species with
widely ovate leaves
suggestive of q. Prinus (rock chestnut oak, now
considered Q. Montana.) I
checked with several naturalists from Mount Lebanon but no one was
familiar with the
Masons or the location of the ravine.
October 24, 1998, 7:30 am. Eighteen people joined
us for the walk through the Mayview
Property, including Mark Bowers from the Botanical Society of Western
Pennsylvania. The
weather was clear and crisp and the leaves still colorful. Along the
trail we found two
giant puffballs. These large white mushrooms resembled ostrich eggs and
measured nearly
nine inches long. On the flood plain Mark pointed out a yellow buckeye
tree, Aesculus
octandra. I had never seen a naturally growing buckeye in
Pennsylvania before. We
measured the largest of the twin sycamore trunks. It had a
circumference of 144 inches,
indicating it was around 183 years old, possibly older.
October 27, 1998, 8:30 am. I returned to the
Mayview property to explore the riparian
community along the flood plain. Riparian communities, or the
association of plants and
animals that live along the edge rivers and streams, are the most
diverse of the original
forest communities in western Pennsylvania. Because of the fertile,
level ground these
were the first forests cleared by the European settlers. No undisturbed
examples of this
community exist. We will never know what the land was like when the
settlers first
ventured up tributaries like Chartiers Creek, but possibly this small
neglected stretch
will give us a preview of what might develop in the future. In addition
to the buckeye,
chinquapin oaks, hickories, papaw, hackberries and basswoods, I found
red oak, sugar maple
and the invasive norway maple on the slope with box elder, elms and
sycamore dominating
the bottom land.
Upstream from the ravine, just before the flood
plain narrows and meets the steep
hillside, I found a dense thicket of papaws. The five inch long leaves
were still a deep
green and the arching trunks ranged from one to five inches in
diameter. According to
Jennings, papaws, Asimina Triloba, were once common
along the rich lower slopes and
flood plains in the southern part of western Pennsylvania and
considerable quantities of
the edible fruits reached Pittsburgh markets via packets from the upper
Monogahela Valley.
Tall american basswood trees, many with multiple trunks, created a
canopy over the papaws.
Some of the trunks had a diameter of over two feet. An abundance of
gray-brown nutlets
hung from the basswoods, each dangling from a stalk connected for half
of its length to a
long, curled bract. One of the seeds fell and spun off over the papaws,
the bract twirling
like a propeller.
Across the small run that flows into Chartiers
Creek I identified a swamp white oak, Quercus
Bicolor. A large specimen with a thirty inch diameter trunk,
its leaves had a
wedge-shaped base with six pairs of round lobes. Beside it grew another
swamp white oak, a
foot in diameter with its trunk pressed tight against the trunk of a
pignut hickory about
the same size. American black walnut husks lay scattered across the
flood plain. These
soft round spheres the size and color of green tennis balls encased the
sweet walnut so
prized by cooks and squirrels. The husks had fallen from a gnarled old
tree almost three
feet in diameter. Walnut wood, with its rich dark color and the tight
twisting grain, is
very expensive and few trees are left to grow this thick. I approached
the small pool on
the flood plain where Tracey had spotted a great blue heron searching
for frogs and I had
watched an eastern phoebe snapping insects. Little more than a
depression at the base of
the slope, it is all that remains of an ancient bend in Chartiers.
In the soft soil beside the pool a neatly stacked
circle of mud pellets formed a
chimney around a crayfish tunnel. A fallen tree, with a diameter of
about fourteen inches
lay across one end of the depression. Long scaly ridges ran along the
gray bark; thick
branched thorns protruded from its side. I recognized it as a honey
locust. Across the
slope stood three more honey locusts of different sizes. I found none
of the long twisting
pods, but golden compound leaves covered the ground. According to
Jennings, honey locusts,
Gleditsia triacanthos, is a moderately
large tree and occurs chiefly on moist,
fertile bottom lands and slopes, particularly in limestone regions. Its
position on the
slope, level with the chinquapin oaks indicated a layer of limestone
ten feet of so above
the flood plain.
November 3, 1998, 8:45 am. The temperature fell
just below 40 degrees and a slight
breeze produced a typical November rustling. Most of the leaves had
fallen; only the dry,
brittle oaks remained. Some of the oak leaves fell. I could hear them
hit the litter. The
wind stopped but the dropping continued. The layer of dead leaves built
up, even in the
field, and I could not walk quietly. On the slopes in the ravine that
leads to the flood
plain few leaves lay on the ground in spite of the tall trees. Without
the herbaceous
layer, which was probably browsed off by deer, the leaf litter was very
vulnerable to wind
scouring. As I approach the ravine I stopped to admire a stand of at
least 3 chinquapin
oaks, a white oak and down slope, 2 red oaks, one nearly 2 feet in
diameter. Sunlight
shone through the leaves of the chinquapin oak, highlighting the rusty
outline on the
yellow leaves.
A Carolina Wren sang. The clear melodious notes
echoed through the ravine. I speculated
about the birds that breed along the flood plain. Of course, the common
residents,
Woodpeckers, Nuthatches, Tufted Titmice and Carolina Chickadees would
probably be well
represented because of the decaying trees with many cavities. I
remembered seeing a hole
excavated by a Belted Kingfisher in the steep earthen bank across
Chartiers Creek. I
imagine Spotted Sandpipers nest on the sandbars. Wild turkey would
surely breed here; also
tiny blue-gray Gnatcatchers and Ruby-throated Hummingbirds. Possibly
Yellow-throated
Warblers build tiny nests high in the sycamores. Yellow-throated Vireos
and Cerulean
Warblers would sing along the high slope. Singing Baltimore Orioles
should sparkle in the
sun shine through the sycamores. Louisiana Waterthrushes probably pass
through as they
move north in early April. Due to the drainage alterations in the
fields, the stream
through the ravine runs only intermittently and the waterthrushes do
not stay to breed.
What a shame we can no longer hear their cheerful Spring song. Maybe in
the future. . .
Mr. Tague is the founder/publisher of the
acclaimed “Nature Observer
News.” He also is the featured commentator on the Allegheny
Front on WYEP 91.3 FM. As
an educator/naturalist, he presents programs for schools and nature
centers throughout
Allegheny County. He is an adjunct professor for the Rachel Carson
Institute/Chatham
College. In addition to many other awards, Mr. Tague was a finalist for
the Three Rivers
Environmental Award in 1988. He can be reached by email at bluejay@city-net.com.
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