Park
Hours |
Apr 1 through Oct 30 |
|
7 am - 9 pm CST |
Oct 31 through Mar 31 |
|
7 am - 6 pm CST |
Logging Requirements - Updated June
5, 2007
To receive credit for
a find, please visit the spot at the listed coordinates. This spot
is located just above the fenceline on the southeast side, close to
the deepest, visible part of the Ensor Sink.
Take another
waypoint at the opposite fenceline on the northwest side across
the deepest part of the sink and measure the distance from
the original waypoint of the earthcache to this new waypoint on the
opposite side.
Email me or send me a
message via my profile with the following information:
- The waypoint coordinates you observed from a spot on northwest
fenceline just above the deepest part of the sink
- The measured distance from the original waypoint to the
observed waypoint
You can measure the
distance in the field or you can take the waypoint and use tools
such as online Coordinate Distance Calculator or
GeoCalc to find distances between
corrdinates later.
Reasonable answers
must received within 7 days of the find or else the log will be
removed.
Enjoy!
Ensor Sink Natural Area was established to preserve the natural
beauty of the land surrounding Ensor Sink, to provide recreational
opportunities for the community and to educate people about the
role of sinkholes and caves in the stormwater drainage for the city
of Cookeville.
Sinkholes are common in Tennessee where the rock below much of
the surface of the land is limestone. As rainwater seeps down into
the earth's surface and comes into contact with limestone, chemical
reactions cause the limestone to slowly dissolve. As water
continues to flow through holes that were created as the limestone
dissolved, the holes become larger. Some small holes eventually
become caves.
"Karst" refers to a geographic area with soluble rock, like
limestone, underneath it. Karst is characterized by sinkholes,
caves and an underground drainage system. Cookeville is built on
karst, and there are two, known, major cave systems beneath the
City of Cookeville. Ensor Sink is part of one of those systems, and
the other includes several caves in the Capshaw Cave system.
Sinkholes, also called "sinks" are the characteristic landform
of karst. Most sinks, known as "solution sinkholes," form as the
limestone dissolves, creating sunken areas in the land surface.
Other sinks, known as "collapse sinkholes," form when caves
collapse and suddenly drop a portion of the land surface above. The
outer edges of sinkholes are normally round or oval, and their
bottoms are either bowl or funnel shaped. When water drains into a
sinkhole, it works like a funnel to feed the water into caves and
underground streams below. Litter and pollutants that are in the
water are also carried underground.
DANGER: Beware of flooding! Ensor Sink and other
sinkholes can be dangerous when it rains. Flooding has been
forceful enough to take large, heavy trash items like grocery
carts, office chairs, bedsprings, bicycle frames and tires deep
into the underground cave system. That is why the channel and
sinkhole are enclosed by a fence. When flooding occurs, the strong,
flowing water can rise even higher than the fence. So, stay safe.
DO NOT ENTER FENCED-IN AREA AT ANY TIME. DO NOT STAY IN ENSOR
SINK NATURAL AREA DURING HEAVY RAINS.
}
This earthcache is approved by the
National
Speleological Society.