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Trail Though Time Earthcache EarthCache

Hidden : 10/12/2004
Difficulty:
1 out of 5
Terrain:
3 out of 5

Size: Size:   not chosen (not chosen)

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Geocache Description:


The Missouri Department of Conservation’s Pickle Springs Natural Area is a special place with cool, moist canyons and spectacular views from tall sandstone bluffs. Several rare plants thrive here, including the beautiful wild azalea. But it is the geology, and its effect on the plants that live here, that makes the area truly unique.

Pickle Springs is a 180-acre area of rugged forested hills with several barren sandstone exposures, box canyons and waterfalls. Within a one-hour walk, there are many interesting geologic features to see, including natural arches, sandstone caves, chimneys, known locally as “hoodoos,” bluffs, box canyons and springs.

It is named after William Pickles, an early settler, who was killed by the notorious outlaw Sam Hildebrand and his gang during the Civil War. Pickle Springs was a favorite hideout for the many Confederate guerillas that roamed this area, attacking remote Union Army outposts and terrorizing local Union sympathizers. The guerillas were the remnants of General Sterling Price’s army of 12,000 men, who were so badly defeated when they attacked Fort Davidson, near Pilot Knob, On Sept. 26-27, 1864. Fort Davidson was defended by a garrison of 1,450 men led by General Thomas Ewing Jr., the brother-in-law of General William Tecumseh Sherman. The Confederates lost nearly 1,000 men in attacking the small earthen fort and its 11 cannons.

The rocks at Pickle Springs were formed nearly 500 million years ago when sand deposited in an extensive maze of braided river channels was cemented together to form sandstone. The sandstone became buried under younger layers of limestone, which were deposited on the floors of ancient seas. The area was then uplifted, as it is today, and erosion has worn away the overlying strata until the old sandstone is again exposed at the surface.

This sandstone, called the Lamotte Formation, outcrops in small portions of the St. Francois Mountains. Pickle Springs is the best known exposure of the Lamotte. Over millions of years, water, ice, rain, wind and plants have worn away softer parts of the sandstone, creating fantastic formations and deep canyons.

The weathered sandstone forms an acidic soil that supports many unique plants. During the time of the great glaciers (10,000 to 300,000 years ago), plants and animals moved south ahead of the advancing ice. Mammoths wandered in the cool canyons of Pickle Springs, grazing on the lush northern vegetation supported by the area’s acid soils. Today the Mammoths are gone, but many of the plants remain, relicts of that earlier climate. As you walk the trail through time you will see some of those relicts, along with the unique geologic features carved by nature.

Because of this unique concentration of rare plants and geologic features, this area has been designated a Missouri Natural Area and a National Natural Landmark. The two-mile loop trail takes you to a number of spectacular geologic features, including The Slot, Spirit Canyon, Dome Rock and Rockpile Canyon, among others. The walk is not particularly difficult, but the trail is narrow and steep in places. Sorry, but it is definitely NOT wheelchair accessible.

Please note:
· This is a state natural area and a national landmark. Please do not disturb animals, plants or rock formations.
· This area has dangerous cliffs and poison ivy. For your children’s safety, please keep them on the trail.
· Camping, rock climbing, fires, horses, motorized vehicles and littering are prohibited.
· Keep pets on leash.

Park at N 37°48.080, W 090° 18.090. Pick up a copy of the excellent “Trail Through Time” brochure at the trailhead. Bring a camera – you’ll definitely want photos of this unique and beautiful area.

To claim your find, send me an email (know_future@juno.com)) with the name of the feature located at:

N 37°48.072, W 90°17.564

This feature is on the trail and its name is on a small sign. [21 Jan 10: The sign is long gone, but if you can grab a map at the trailhead you won't have much trouble identifying the feature.] The heavy tree canopy may give you a different reading at this location. Just come as close as you can while staying on the trail and you will find it.

Additional Hints (Decrypt)

jngre eryngrq

Decryption Key

A|B|C|D|E|F|G|H|I|J|K|L|M
-------------------------
N|O|P|Q|R|S|T|U|V|W|X|Y|Z

(letter above equals below, and vice versa)