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Barra Honda
National Park
Although Barra Honda National Park covers 2,295 ha., its reason for being
is not what lies on the surface, but the geological treasure housed below.
This is the only park in the country designed to protect caves.
To date, 19 separate caves have been discovered in the limestone ridge that
makes up the Barra Honda formation. The entrances to these caves are all
vertical. Therefore, ropes and climbing equipment are necessary for those who
are interested in exploring this subterranean world. Cave depths vary from 21
to 240 meters.
In addition to stalactites and stalagmites, the wide variety of other curious
geological formations inside these caves have given rise to the following
descriptive names: soda straws, cave grapes, curtains, terraces, pearls,
flowers, needles, and even fried eggs! Compared to many other caves with
horizontal entrances, the geological features of Barra Honda are in excellent
condition owing to the difficulty of access.
The natural vegetation that once covered much of the park is sadly not in as
perfect a condition, due to deforestation and cattle ranching, nor is there a
well-marked system of trails to the few decent patches of forest in the park.
Admission policy: To go spelunking in Barra Honda requires previous permission
which can be arranged through the Park Service offices in San José (phone:
192).
Getting there: From San José, take the PanAmerican Highway north to just
beyond the entrance to Las Juntas de Abangares, look for the sign indicating
the left turn to the Tempisque Ferry. Once across the river, continue on for
about 12 km. before taking a right turn to the village of Barra Honda (also
known as Nacaome). Continue on towards the village of Santa Ana and follow
signs for the park entrance.
Climate: Hot and dry from December through April, and hot and humid during the
rainy season.
History: Over the course of the past 70 million years, nature has patiently
worked to create the remarkable system of caves at Barra Honda. First,
millions of years were necessary to form the marine limestone deposits derived
from ancient coral reefs. Then, seismic activity along local fault lines was
responsible for raising the ridge above sea level where rain water and
atmospheric gases could combine to dissolve away portions of the rock, while
also leaving calcium deposits in an endless pattern of strange shapes inside
the still-forming caves.
As recently as 1967, it was still a matter of debate whether or not Barra
Honda Mountain was a volcano. Credibility was given to this belief by the foul
odor and strange sounds -- likened to the roar of a steam engine -- that
emanated from one of the "craters" on top of the ridge. As
explorations of the caverns continued it became obvious that volcanism had
nothing to do with the formation of Barra Honda and the opening that produced
the smells and noise turned out to harbor a tremendous quantity of bats. The
odor came from the accumulated guano and the "roar" was the sound
made by the fluttering wings of tens of thousands of these creatures of the
night. Perhaps even more intriguing is the question, "Why are there so
few bats found in the other caves at Barra Honda?"
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