Marvel Cave

Last updated
Marvel Cave
Marble Cave
Marvel Cave.JPG
Marvel Cave Cathedral Room
Location Silver Dollar City, Branson, Missouri,
United States
Coordinates 36°40′03″N93°20′23″W / 36.6675°N 93.3397°W / 36.6675; -93.3397
Depth500 ft (152 m)
Discovery16th century
Entrances2
AccessPrivate (Tours on park operating days)
Show cave opened1894
Show cave length60 minutes
LightingElectric
Features Flowstone, Stalagmites, Stalactites, Waterfall
Website http://www.silverdollarcity.com/theme-park/attractions/rides/Marvel-Cave.aspx

Marvel Cave is a privately owned cave located just west of Branson, Missouri, in Stone County. It is one of the main attractions of Silver Dollar City and is registered as a National Natural landmark. [1]

Contents

The first recorded expedition of the cave was in 1869, led by Henry T. Blow. Marvel Cave was originally called Marble Cave, after explorers in 1882 saw what they thought was marble on the cave's ceiling. This started the Marble Cave Mining Company, although later it was realized that there was never any marble in the cave. The Marble Cave Mining Company ceased all operations after only four and a half years. William Lynch purchased the cave in 1889, and soon after opened the cave to the public. In 1950, Hugo Herschend leased the cave for 99 years. The Herschends made renovations to the cave, and later opened the now popular theme park, Silver Dollar City, on the surface above the cave. [2] Marvel Cave is known for being one of the largest caves in Missouri, having one of the largest cave entry rooms (the Cathedral Room) of any cave in North America, and for being one of the longest running tourist attractions in the Ozarks.

History

The Bald Knobbers

According to Silver Dollar City park legend, a local group of vigilantes who later turned into outlaws called the Bald Knobbers were known for throwing people through the sinkhole into Devil's Den around the mid 19th century. Though it's possible that roving Bushwhackers and outlaws could have chosen to dispose of their victims through this sinkhole, the Bald Knobbers did not form until 1883 (starting-up in neighboring Taney County) and were replaced by an unofficial chapter in 1886 within nearby Christian County, with unofficial chapters in other counties (including Stone County, where the cave is located) later than that.

Despite there being no written evidence to substantiate it, it's possible that Stone County's unofficial Bald Knobbers used the cave for various uses sometime in 1889, between the time the mining operations ceased and late October of that year when it was purchased for sightseeing tours.

Early explorers

There is evidence that the Spanish explored the cave in 1541, hoping to uncover riches and possibly the fountain of youth. [3] There is a legend that the Spanish buried gold in the cave. The first known expedition was in 1869 and led by Henry T. Blow of St. Louis, a lead mining magnate. He explored the cave with six other miners. [3] One by one, the miners lowered themselves down into the sinkhole. They carried lanterns for light and spent hours studying the cave walls carefully searching for signs of mineral deposits. They went as far as the Shoe Room, because on one side was the Gulf of Doom, which they believed was the bottomless pit after throwing rocks down the Gulf of Doom and hearing no sound. On the other side was the Cloud Room, which was filled to the ceiling with bat guano. The miners returned to the surface late that evening having failed to discover the lead ore they sought, but were convinced that the flat ceiling of the Shoe Room contained marble. Their report gained the interest of area locals who decided to name the cave Marble Cave.

No more expeditions took place until 1882 when another group of entrepreneurs, led by Mr. T. Hodges Jones and Truman S. Powell of Barton County, entered the cave in hopes of finding lead. Jones and Powell found huge amounts of guano and the flat ceiling, which they also believed to be marble.

Marble Cave Mining and Manufacturing Company

In 1884, Mr. T. Hodge Jones bought the property and, with several of his friends, formed the Marble Cave Mining and Manufacturing Company to mine the marble from the cave. The company hired a geologist, and it was proved that what looked like marble on the ceiling of the Shoe Room was really limestone. To keep the company alive they mined out the guano and sold it for $700 a ton. The guano was used for gunpowder and fertilizer. The miners filled ore carts with guano, then the carts were pulled by donkeys to the Cathedral Room, and the carts were lifted out of the cave by a pulley system. In 1889, after four and a half years, all the guano was mined out. Marble Cave Mining, Co. closed all operations.

Marmaros

Marmaros (or Μαρμαρος, Greek for "Marble") was a small town that formed along with the Marble Cave Mining and Manufacturing Company in 1884. Originally called Marble City, it was located on the rough hilltop near the cave and recorded a plat map at the courthouse in Galena, Missouri. Marmaros contained a hotel, general store, pottery shop, white oak furniture factory, and was rumored to have a saloon. The town turned into a ghost town in 1889 after the Marble Cave Mining, Co. closed. When the Lynches bought the cave, the town was burned to the ground by the local group of vigilantes known as the Bald Knobbers.

The Lynches

On October 30, 1889, William Henry Lynch, a Canadian miner and dairyman, purchased the cave and the square mile of land around the cave where Marmaros was located for $10,000. [3] After coming to Marvel Cave, he found that Marmaros was burnt to the ground. Lynch, with the aid of his family, proposed to open the cave to sightseers. The Lynches began operation of the sightseeing venture in 1894 with a grand celebration and a few visitors. [3] The cave has remained open since, making it one of the oldest continuously running tourist attractions in the Ozarks.

When William Lynch died in 1927, ownership of the cave passed to his daughters. Shortly thereafter, the name of the cave was changed to Marvel Cave. [3] The Lynch family operated the cave for over fifty years.

The Herschends

A Chicago vacuum cleaner salesman, Hugo Herschend, purchased a 99-year lease on the cave in 1950, from The Lynch sisters. [3]

After Hugo Herschend's death in 1955, his wife Mary took over the day-to-day operations of the cave. With the aid of her two sons, Jack and Peter, Mary Herschend was able to make vast improvements to the cave. They added concrete paths and stairs to the cave, and a tower from the sinkhole to the top of the debris pile. Also, they added a narrow gauge funicular (cable-pulled) railway in 1957, whose trains pulled visitors a distance of 218 feet (66 m), [3] from the depths of the cave up to the surface. Before building the cable train, the Army Corps of Engineers said that it could not be built, because a cable train can not make a turn like the one the Herschends planned. The Herschends built it anyway, and it is still in operation to this day.

Once the cable train was in operation, the Herschends decided to recreate the mining village Marmaros, for tourists waiting to go on a tour. It opened in 1960, and grew into Silver Dollar City.

In 1972 Genevieve Lynch died and bequeathed the cave to the College of the Ozarks and the First Presbyterian Church of Branson. The Herschends continue to operate the property under lease. [4]

Tours

Currently there are two different tours offered: The Traditional Tour and The Lantern Tour.

Traditional tours

The first guided tours in the cave were in 1894 run by the Lynches. They lasted 8 hours and were by candle or lantern. Visitors climbed through the sink hole on a 100 feet (30 m) ladder down to the top of the pile. Then you were instructed to slide down the pile to the bottom. You received a candle to guide your way. The tours included the Egyptian Room (now the Shoe Room), the Lakes Passage, and you saw formations such as the Great White Throne (now the Liberty Bell), and the Spring Room Sentinel (now just the Sentinel). After the Hershends started tours in 1950, they removed the wooden stairs, and added concrete stairs and paths through the cave. Current tours last for about an hour, and are limited to 45 people.

Lantern tour

In 2006, Marvel Cave started offering The Lantern Light Tour. In this tour the electric lights are turned off in the cave and lanterns are given to each member of the tour. Unlike the regular tours which are free, this tour costs $16.12, and is limited to 20 people. The tour has been extended into the Mammoth Room, making it the first tour to incorporate this room in more than fifty years. One is also able to see both the summer and fall sections if the Waterfall Room is not flooded. The tour lasts about an hour and a half. The guide focuses on the history and folklore of the cave and is able to explain more information about the cave due to the small group setting of the tour.

Rooms and passages

Notable formations

Life in the cave

Gray bat in a hibernaculum. A colony of this species lives in Marvel Cave. Myotis grisescens hibernating.jpg
Gray bat in a hibernaculum. A colony of this species lives in Marvel Cave.

Marvel Cave is host to a variety of bats and salamanders. Marvel Cave has been recognized for its outstanding work in preserving its colony of endangered Gray Bats.

Bats
Salamanders

See also

Related Research Articles

<span class="mw-page-title-main">Cave</span> Natural underground space large enough for a human to enter

A cave or cavern is a natural void in the ground, specifically a space large enough for a human to enter. Caves often form by the weathering of rock and often extend deep underground. The word cave can refer to smaller openings such as sea caves, rock shelters, and grottos, that extend a relatively short distance into the rock and they are called exogene caves. Caves which extend further underground than the opening is wide are called endogene caves.

<span class="mw-page-title-main">Sinkhole</span> Geologically-formed topological depression

A sinkhole is a depression or hole in the ground caused by some form of collapse of the surface layer. The term is sometimes used to refer to doline, enclosed depressions that are also known as shakeholes, and to openings where surface water enters into underground passages known as ponor, swallow hole or swallet. A cenote is a type of sinkhole that exposes groundwater underneath. Sink and stream sink are more general terms for sites that drain surface water, possibly by infiltration into sediment or crumbled rock.

<span class="mw-page-title-main">Natural Bridge Caverns</span> United States historic place

The Natural Bridge Caverns are the largest commercial caverns in the US state of Texas. The name is derived from the 60-foot (18 m) natural limestone slab bridge that spans the amphitheater setting of the cavern's entrance. The span was left suspended when a sinkhole collapsed below it.

<span class="mw-page-title-main">Inner Space Cavern</span> Cave in Georgetown, Texas, United States

Inner Space Cavern is a karst cave located in Georgetown, Texas. The cavern was formed by water passing through Edwards limestone. The cavern is estimated to be around 20-25 million years old but were only open to the surface since the late Pleistocene period 14,000–45,000 years ago.

<span class="mw-page-title-main">Lechuguilla Cave</span> Cave in Eddy County, New Mexico, U.S.

At 150.4 miles (242.0 km), Lechuguilla Cave is the eighth-longest explored cave in the world and the second deepest in the continental United States. It is most famous for its unusual geology, rare formations, and pristine condition.

<span class="mw-page-title-main">Cathedral Caverns State Park</span> State park in Alabama, United States

Cathedral Caverns State Park is a public recreation area and natural history preserve located in Kennamer Cove, Alabama, approximately 5 miles (8.0 km) northeast of Grant and 7 miles (11 km) southeast of Woodville in Marshall County. The park, first known as Bats Cave, was developed as a tourist attraction in the 1950s. Cathedral Caverns was declared a National Natural Landmark in 1972 and opened as a state park in 2000.

<span class="mw-page-title-main">Craighead Caverns</span>

Craighead Caverns is an extensive cave system located in between Sweetwater and Madisonville, Tennessee. It is best known for containing the United States' largest and the world's second largest non-subglacial underground lake, The Lost Sea. In addition to the lake, the caverns contain an abundance of crystal clusters called anthodites, stalactites, stalagmites, and a waterfall.

<span class="mw-page-title-main">Silver Dollar City</span> Amusement park in Missouri, United States

Silver Dollar City is a 61-acre (25 ha) amusement park in Stone County, Missouri, near the cities of Branson and Branson West. The park is located off of Missouri Route 76 on the Indian Point peninsula of Table Rock Lake. Silver Dollar City opened on May 1, 1960. The park is an 1880s-themed experience. Silver Dollar City's operating season runs from March until December, with the park closed for two months. Silver Dollar City is owned by Herschend Family Entertainment.

<span class="mw-page-title-main">Wes Skiles Peacock Springs State Park</span> State park in Florida, United States

Wes Skiles Peacock Springs State Park is a 733-acre (297 ha) Florida State Park located on Peacock Springs Road, two miles (3 km) east of Luraville and on State Road 51, 16 miles (26 km) southwest of Live Oak, Florida. Activities include picnicking, swimming and diving, and wildlife viewing. Among the wildlife of the park are deer, bobcats, raccoon, squirrels, beaver and otters, as well as turkey, blue heron and barred owls. The park name commemorates the work of diver and explorer Wes Skiles. Prior to 2010 the park was known as Peacock Springs State Park. Amenities include a nature trail, six sinkholes, and Peacock and Bonnet Springs, with miles of underwater caves popular with cave divers. The two springs are tributaries of the Suwannee River. The park is open from 8:00 am till sundown year round.

<span class="mw-page-title-main">Abercrombie Caves</span> Protected area in New South Wales, Australia

The Abercrombie Caves, contained within the Abercrombie Karst Conservation Reserve, are a series of limestone arch caves that are located in the Central West region of New South Wales, Australia. The caves are renowned for their karst qualities, namely the formation that has been eroded by water action that has developed from a sinkhole to become a blind valley. Several good examples of crayback formations exist in both entrances.

<span class="mw-page-title-main">Fire in the Hole (1972)</span> Enclosed roller coaster

Fire in the Hole was an enclosed roller coaster located at Silver Dollar City in Branson, Missouri. The three-story steel coaster was built in-house by Silver Dollar City in 1972. The ride is often considered a cross between a dark ride and a roller coaster. A similar ride, "Blazing Fury", was built at Herschend Family Entertainment's Silver Dollar City Tennessee, now known as Dollywood, in 1978. On February 13, 2023, Silver Dollar City announced 2023 would be the last season for the ride before it is closed permanently. On August 14, 2023, Silver Dollar City announced the new Fire in the Hole to open in 2024 in the new "Fire District" section of the park.

<span class="mw-page-title-main">Carlsbad Caverns National Park</span> National Park in New Mexico, United States

Carlsbad Caverns National Park is an American national park in the Guadalupe Mountains of southeastern New Mexico. The primary attraction of the park is the show cave Carlsbad Cavern. Visitors to the cave can hike in on their own via the natural entrance or take an elevator from the visitor center.

<span class="mw-page-title-main">Bat Cave mine</span> Former mining operation in Mohave County, Arizona

The Bat Cave mine was a bat guano mine in a natural cave located in the western Grand Canyon of Arizona at river mile 266, 800 feet (240 m) above Lake Mead.

<span class="mw-page-title-main">Blue Hole (New Mexico)</span> Sinkhole used for scubadiving in New Mexico, United States

The Blue Hole of Santa Rosa, or simply the Blue Hole, is a circular, bell-shaped pool or small lake located along Route 66 east of Santa Rosa, New Mexico that is a tourist attraction and swimming venue, and one of the most popular dive destinations in the US for scuba diving and training. The Blue Hole is an artesian well and cenote that was once used as a fish hatchery.

The Caves of the Tullybrack and Belmore hills are a collection of caves in southwest County Fermanagh, Northern Ireland. The region is also described as the West Fermanagh Scarplands by environmental agencies and shares many similar karst features with the nearby Marble Arch Caves Global Geopark.

<span class="mw-page-title-main">Cheese Cave</span> Lava tube in Washington, United States

Cheese Cave is a lava tube located in Gifford Pinchot National Forest just southwest of Trout Lake, Washington. It is approximately 2,060 feet (628 m) in length, with a mostly flat floor 25 feet (8 m) wide and a 45 feet (14 m) to 60 feet (18 m) high ceiling.

<span class="mw-page-title-main">Cherney Maribel Caves County Park</span> County park in Wisconsin (US)

Cherney Maribel Caves County Park is a county park located near Maribel in Manitowoc County, Wisconsin. The park occupies 75 acres along the West Twin River. Cherney Maribel Caves consists of eleven caves along a rugged cliff line that runs parallel with the West Twin River. Maribel New Hope Cave, Tartarus Cave, Sinkhole Cave and Split Rock Cave are all established gated caves that need guides to visit the entire caves, they are gated due to past vandalism to the Speleothems and protect the current Speleothems.

<span class="mw-page-title-main">Cedar Sink</span> Landform in Edmonson County, Kentucky, United States

Cedar Sink is a vertical-walled large depression, or sinkhole, in the ground, that is located in Edmonson County, Kentucky and contained within and managed by Mammoth Cave National Park. The sinkhole measures 300 feet (91.4 m) from the top sandstone plateau to the bottom of the sink and was caused by collapse of the surface soil. The landscape is karst topography, which means the region is influenced by the dissolution of soluble rocks. Sinkholes, caves, and dolines typically characterize these underground drainage systems. Cedar Sink has a bottom area of about 7 acres (2.8 ha) and has more fertile soil compared to the ridgetops.

<span class="mw-page-title-main">Mystic River Falls</span> Water ride at Silver Dollar City

Mystic River Falls is a river raft ride located at Silver Dollar City in Branson, Missouri. The ride is an upgraded installation and direct replacement of the former Lost River of the Ozarks attraction, which was removed following the 2018 season, as well as an investment to celebrate the park's 60th anniversary. As of its construction in 2020, Mystic River Falls holds the record for the Western Hemisphere's highest drop on a raft slide at 45 feet (14 m) tall, as well as a total linear length of 2,100 feet (640 m) and a unique elevator lift. Mystic River Falls soft opened for members on July 5, 2020 and officially opened to the public on July 21, 2020.

The 1973 Mount Gambier cave diving accident was a scuba diving incident on 28 May 1973 at a flooded sinkhole known as "The Shaft" near Mount Gambier in South Australia. The incident claimed the lives of four recreational scuba divers: siblings Stephen and Christine M. Millott, Gordon G. Roberts, and John H. Bockerman. The four divers explored beyond their own planned limits, without the use of a guideline, and subsequently became lost, eventually exhausting their breathing air and drowning, with their bodies all recovered over the next year. To date, they are the only known fatalities at the site. Four other divers from the same group survived.

References

  1. "National Natural Landmarks - National Natural Landmarks (U.S. National Park Service)". www.nps.gov. Retrieved 2023-04-18.
  2. "Marvel Cave". www.silverdollarcity.com. Retrieved 2023-04-18.
  3. 1 2 3 4 5 6 7 Show Caves of the United States of America: Marvel Cave
  4. Missouri Roadsides: The Traveler's Companion - Bill Earngey - University of Missouri Press (October 1995) - ISBN   0-8262-1021-X