…..Posted
coordinates designate recommended parking. The Happel's Meadow
wetland, is located on both sides of PA Rt. 16 in Blue Ridge
Summit, PA. What is now Monterey golf course and the Pen Mar Little
League field were also once part of the
wetland.
A BRIEF
HISTORY
…....In the southeast corner of
Franklin County, Pennsylvania, one can locate the small town of
Blue Ridge Summit. Situated on the South Mountain Plateau in the
shadow of Mt. Dunlop, Blue Ridge Summit was once a thriving resort
community patronized by folks from Baltimore and Washington, DC who
chose to ride the railroad for a weekend retreat.
…....To
accommodate their guests, the lavish hotels of the period looked to
John and Albert Happel, whose farm on what is now known as
Happel’s Meadow supplied about 90% of the produce for the
resort. The Happels purchased the marshy area northwest of
Tracey’s Corner, set up a drainage system of terra cotta pipe
laid every 300 feet and began working the rich wetland soil.
Specialties included up to 300,000 celery plants annually, a
variety of herbs and green vegetables, cantaloupes and chickens.
Orders of 500 dozen ears of sweet corn on a weekend were not
uncommon. When John left the business in 1921, Albert farmed
timothy and sold wholesale feed, much of which was purchased by the
Washington Zoo. In 1937, the new PA Rt. 16 bisected the wetland,
but farming continued.
…....The Blue Ridge Summit resort
era gradually ended with the advent of the automobile and decreased
demand for train excursions. The Happel farm was passed on, and in
1990, Washington Township accepted from Charles Gardner and his
sister, Letitia, the donation of the 76 acre tract as a wetland
preserve.
AREA GEOLOGY
…....The
South Mountain Plateau and Happel’s Meadow are part of the
South Mountain geological formation which extends from Maryland
through the eastern part of Franklin County into Adams County and
ends near Dillsburg. The South Mountain fold is predominantly
Cambrian metamorphic rock (500-600 million years old) consisting of
limestone and dolomite with some sandstone and shale. A small
Precambrian intrusion in the Blue Ridge Summit area includes
gneiss, greenstone and serpentine.
WETLANDS
…....Happel’s Meadow has
officially been designated a wetland. To meet wetland criteria, an
area must:
……….1. be
saturated by surface or ground water such that the
.........] average annual
water level is at the surface
….……2.
demonstrate vegetation that is typical of wet marshy soils
……….3.
exhibit hydric soils
..…..Vegetation is a good
indicator of the water level and duration of saturation in a
wetland. Many wetland species are not commonly recognizable as
such. More familiar are sedges, cattails, rushes, skunk cabbage and
riparian hardwoods such as red maple and sycamore.
…....Hydric
soils are those which are saturated, flooded or ponded long enough
during the growing season to develop anaerobic conditions in the
surface horizon. Oxygen diffuses 10,000 times more slowly in
saturated soils than in unflooded soils. Microbes rapidly use the
little oxygen that does reach the soil, creating anoxic conditions.
The type of hydric soil depends upon both bedrock and vegetation.
…....Hydric soil is recognizable
by a rotten egg odor resulting from reduction of sulfur to hydrogen
sulfide under anaerobic conditions, deep organic content, and
gleying: bluish to greenish color resulting from reduction of iron
in the soil.
…....Happel’s Meadow is
drained by Red Run which follows Rt. 16 down the west side of the
mountain and joins the east branch of Antietam Creek not far from
Welty’s Mill. Wetlands provide not only a natural water
filtration system, but also offer species diversity rivaled only by
salt marshes, coral reefs and tropical rainforest canopies.
THE
CACHE
…....If you are arriving from the
west, carefully observe Happel’s Meadow as you drive through
on your way to the designated coordinates. Look for the sign to the
right about 0.6 mile from the posted latitude and longitude. If you
are arriving from the east, continue past Tracey's Corner and the
Pen Mar Little League field on the left, observe Happel’s
Meadow as you drive through it along Rt. 16, and then return to the
posted coordinates.
…....At the stated coordinates
you will be able to safely view a long section of the meadow
together with a sampling of the many plant varieties. Walk along
the edges but please do not enter the meadow, as
it is a fragile environment containing at least six species listed
in Maryland as being endangered.
……….To get credit
for this cache:
…....1.
Answer via E-mail to the cache owner the following:
……………A. What is the altitude at the listed coordinates?
……………B. How does altitude relate to the uniqueness of
Happel's Meadow?
……………….(Hint: When the Rt. 16 causeway was added, terra cotta pipes along the road were used to
..................help drain standing water).
……………C. Even if you can not see standing water now, list at
least 2
...............pieces of
visual evidence that Happel’s Meadow is a
.............. wetland.
……………D. Evaluate the surrounding area and in a sentence or
two,
………….….…formulate a hypothesis as to why or how a wetland can
be
……………..…sustained in this unique
location.
">….2.
Upload a photo of yourself or an item unique to you and your GPS with either Mt. Dunlop
.......... lookout tower
(to the west) or the Blue Ridge Summit post office (to your left as
you drive into
.......... the parking lot) in the background.
REFERENCES
“Recognizing Wetland Soils”. n.d. Available
Online: Sept. 30, 2007
..…..http://www.dnr.wa.gov/htdocs/lm/field_guides/recognizing/soils.html
Record Herald. 27
March, 1992. p. 6.
Record Herald. 24
May, 1975. p. 3.
Record Herald. vol.
142, no. 301 p. 1. 3 March, 1990.
U.S. Department of
Agriculture Soil Conservation Service. 1991. Hydric Soils of the
United States.
“What Is Wetland
Delineation?” Jan. 1997. Available Online: Sept. 30,
2007
…....http://www.epa.state.oh.us/pic/facts/wetdelin.html
Willard, Bradford. 1973. PA Geology Summarized.
Commonwealth of PA, D.E.R. Bureau
…....of Topography,
Geologic Survey.
Zephyr. 12
Septemper,
1902.