Cave digging

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Looking up the entrance shaft of Committee Pot entrance to Notts II Cave on Leck Fell which was dug after divers had accessed an extensive cave system below Notts2up.jpg
Looking up the entrance shaft of Committee Pot entrance to Notts II Cave on Leck Fell which was dug after divers had accessed an extensive cave system below

Cave digging is the practice of enlarging openings of undiscovered caves to allow entry. Cave digging usually begins with a survey of mountains and valleys in karst topography searching for new caves, with the goal of creating accessible entrances. [1] Whether outside an inaccessible cave or inside an already accessible cave, when spaces are evident on the other side of blocked passages, many strategies can be used to widen entrances from rearranging rocks to using explosives. [2]

Contents

The area around digs may be unstable and often need to be shored up with scaffolding or concrete to prevent re-collapse. It can be a dangerous activity. [3]

Geological cave indicators

Most of the obvious caves in countries with a well-established caving community have already been discovered and explored, so cavers must search for new caves. This is most commonly accomplished by scouring the countryside in areas with cave potential for previously undiscovered openings to the underground. These may be found in sinkholes, in rock outcrops or anywhere the ground is underlain by limestone or other soluble rock. [4] Areas underlain by lava flows or where lava tubes are found may also contain new caves.[ citation needed ]

If the discovered feature is significantly draughting air either in or out, it is an encouraging indication that there is potential for a large or extensive cave beyond. [5]

Technique

On occasion, a newly discovered opening will be large enough for the average person to enter, but often they are too small and must be enlarged to allow entry. When the entrance is too small, it is enlarged using cave digging techniques.

Sometimes digging simply involves moving a few rocks and some soil. This can be accomplished with the bare hands or may involve the use of folding army shovels, root-pruning saws, hammer and chisels, buckets to move the material, and rope to haul the buckets if the opening is being enlarged in a downward direction. Large tamping tools and crowbars are also useful in dislodging the rocks and soil as the digging progresses. [6]

Sometimes, the use of equipment and brute force is not enough to gain entry into the cave. In cases such as these, serious diggers resort to more intensive means of opening the cave. Many "digs" become large group projects, involving backhoes, timber shoring, and even the use of large diameter well drilling methods. [7]

Where the main impediment is solid rock, entry may involve the practice of rock shaving. This method consists of drilling holes in the rock, filling them with a small amount of gunpowder, and then igniting it to fragment the rock in thin layers. [8] A similar technique, called plug and feather, involves driving wedges into lines of small diameter holes that have been drilled in the rock. As the wedges are driven into the holes, a crack forms along the line of holes and the rock is eventually broken. [9] A more recently developed technique is known as "capping", where a hole is drilled into the rock using a battery-powered drill, a small charge (commonly designed for use with a nail gun) is inserted, and tapped with a long steel rod in order to cleave off pieces of rock. [10] An environmental and safety assessment should be conducted before blasting to ensure minimal impact to the cave environment.

Impact

Cave digging can damage the cave by exposing it to the outside world or through the force needed to enter. This can harm the ecology within the cave. Careless cave digging can also lead to destruction or irresponsible removal of items with archeological significance. [11]

Related Research Articles

<span class="mw-page-title-main">Caving</span> Recreational pastime of exploring cave systems

Caving, also known as spelunking and potholing, is the recreational pastime of exploring wild cave systems. In contrast, speleology is the scientific study of caves and the cave environment.

<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">Karst</span> Topography from dissolved soluble rocks

Karst is a topography formed from the dissolution of soluble carbonate rocks such as limestone, dolomite, and gypsum. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. More weathering-resistant rocks, such as quartzite, can also occur, given the right conditions.

<span class="mw-page-title-main">Underground hard-rock mining</span> Mining techniques used to excavate hard minerals and gems

Underground hard-rock mining refers to various underground mining techniques used to excavate "hard" minerals, usually those containing metals, such as ore containing gold, silver, iron, copper, zinc, nickel, tin, and lead. It also involves the same techniques used to excavate ores of gems, such as diamonds and rubies. Soft-rock mining refers to the excavation of softer minerals, such as salt, coal, and oil sands.

<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">Cave diving</span> Diving in water-filled caves

Cave-diving is underwater diving in water-filled caves. It may be done as an extreme sport, a way of exploring flooded caves for scientific investigation, or for the search for and recovery of divers or, as in the 2018 Thai cave rescue, other cave users. The equipment used varies depending on the circumstances, and ranges from breath hold to surface supplied, but almost all cave-diving is done using scuba equipment, often in specialised configurations with redundancies such as sidemount or backmounted twinset. Recreational cave-diving is generally considered to be a type of technical diving due to the lack of a free surface during large parts of the dive, and often involves planned decompression stops. A distinction is made by recreational diver training agencies between cave-diving and cavern-diving, where cavern diving is deemed to be diving in those parts of a cave where the exit to open water can be seen by natural light. An arbitrary distance limit to the open water surface may also be specified.

<span class="mw-page-title-main">Jewel Cave National Monument</span> Cave in the Black Hills of South Dakota, USA

Jewel Cave National Monument contains Jewel Cave, currently the fifth longest cave in the world and second longest cave in the United States, with 219.77 miles (353.69 km) of mapped passageways as of March 2024. It is located approximately 13 miles (21 km) west of the town of Custer in Black Hills of South Dakota. It became a national monument in 1908.

<span class="mw-page-title-main">Blowhole (geology)</span> Hole at the top of a sea-cave which allows waves to force water or spray out of the hole

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<span class="mw-page-title-main">Cenote</span> Natural pit or sinkhole that exposes groundwater underneath

A cenote is a natural pit, or sinkhole, resulting when a collapse of limestone bedrock exposes groundwater. The term originated on the Yucatán Peninsula of Mexico, where the ancient Maya commonly used cenotes for water supplies, and occasionally for sacrificial offerings. The name derives from a word used by the lowland Yucatec Maya—tsʼonoʼot—to refer to any location with accessible groundwater.

<span class="mw-page-title-main">Ruby Falls</span> Underground waterfall in Tennessee, United States

Ruby Falls is a series of underground cascading waterfalls totaling 145 feet (44 m) in Lookout Mountain, near Chattanooga, Tennessee, in the United States.

Directional boring, also referred to as horizontal directional drilling (HDD), is a minimal impact trenchless method of installing underground utilities such as pipe, conduit, or cables in a relatively shallow arc or radius along a prescribed underground path using a surface-launched drilling rig. Directional boring offers significant environmental advantages over traditional cut and cover pipeline/utility installations. The technique is routinely used when conventional trenching or excavating is not practical or when minimal surface disturbance is required.

<span class="mw-page-title-main">British Cave Research Association</span>

The British Cave Research Association (BCRA) is a speleological organisation in the United Kingdom. Its object is to promote the study of caves and associated phenomena, and it attains this by supporting cave and karst research, encouraging original exploration, collecting and publishing speleological information, maintaining a library and organising educational and scientific conferences and meetings.

A silt out or silt-out is a situation when underwater visibility is rapidly reduced to functional zero by disturbing fine particulate deposits on the bottom or other solid surfaces. This can happen in scuba and surface supplied diving, or in ROV and submersible operations, and is a more serious hazard for scuba diving in penetration situations where the route to the surface may be obscured.

<span class="mw-page-title-main">Simpson Pot</span> Cave in North Yorkshire, England

Named after Eli Simpson, Simpson Pot is a limestone cave in West Kingsdale, North Yorkshire, England. It leads into Swinsto Cave and thence into Kingsdale Master Cave, and it is popular with cavers as it is possible to descend it by abseiling down the pitches, retrieving the rope each time, and exiting through Valley Entrance of Kingsdale Master Cave at the base of the hill. It is part of a 27-kilometre (17 mi) long cave system that drains both flanks of Kingsdale.

<span class="mw-page-title-main">Ponor</span> Natural opening where surface water enters caves

A ponor is a natural opening where surface water enters into underground passages; they may be found in karst landscapes where the geology and the geomorphology is typically dominated by porous limestone rock. Ponors can drain stream or lake water continuously or can at times work as springs, similar to estavelles. Morphologically, ponors come in forms of large pits and caves, large fissures and caverns, networks of smaller cracks, and sedimentary, alluvial drains.

The West Virginia Speleological Survey (WVaSS) is a speleological organization and ongoing cave survey program that has gathered information and published about West Virginia caves and karst since 1967.

There are a number of terms that are used in connection with caves, caving and speleology. The following is an incomplete list.

<span class="mw-page-title-main">Digging</span> Removal of material from a solid surface

Digging, also referred to as excavation, is the process of using some implement such as claws, hands, manual tools or heavy equipment, to remove material from a solid surface, usually soil, sand or rock on the surface of Earth. Digging is actually the combination of two processes, the first being the breaking or cutting of the surface, and the second being the removal and relocation of the material found there. In a simple digging situation, this may be accomplished in a single motion, with the digging implement being used to break the surface and immediately fling the material away from the hole or other structure being dug.

<span class="mw-page-title-main">Amatérská Cave</span> Cave and archaeological site in the Czech Republic

Amatérská Cave is part of longest cave system in the Moravia, Czech Republic. It is also famous for archaeological discoveries. Except for the entrance, the cave is not accessible to the public, although occasionally it is opened for visitors.

<span class="mw-page-title-main">Cave diving regions of the world</span> Regions of the world where known cave diving venues exist

Cave diving is underwater diving in water-filled caves. The equipment used varies depending on the circumstances, and ranges from breath hold to surface supplied, but almost all cave diving is done using scuba equipment, often in specialised configurations with redundancies such as sidemount or backmounted twinset. Recreational cave diving is generally considered to be a type of technical diving due to the lack of a free surface during large parts of the dive, and often involves planned decompression stops. A distinction is made by recreational diver training agencies between cave diving and cavern diving, where cavern diving is deemed to be diving in those parts of a cave where the exit to open water can be seen by natural light. An arbitrary distance limit to the open water surface may also be specified. Despite the risks, water-filled caves attract scuba divers, cavers, and speleologists due to their often unexplored nature, and present divers with a technical diving challenge.

References

  1. "Chapter 1 - Searching". Virginia Speleological Survey. Retrieved 29 April 2024.
  2. Jones, William K. (31 October 2005). DIGGING: GUIDELINES FOR CAVERS AND RESOURCE MANAGERS (DOC). National Cave and Karst Management Symposium. Albany. pp. 88–91. Retrieved 27 April 2024.
  3. "Chapter 2 - Digging". Virginia Speleological Survey. Retrieved 29 April 2024.
  4. "Chapter 1 - Searching". Virginia Speleological Survey. Retrieved 29 April 2024.
  5. Gabrovšek, Franci (3 April 2023). "How do caves breathe: The airflow patterns in karst underground". PLOS ONE. 21 (3). Bibcode:2023PLoSO..1883767G. doi: 10.1371/journal.pone.0283767 . PMC   10069778 . PMID   37011070.
  6. Jones, William K. (31 October 2005). DIGGING: GUIDELINES FOR CAVERS AND RESOURCE MANAGERS (DOC). National Cave and Karst Management Symposium. Albany. pp. 88–91. Retrieved 27 April 2024.
  7. Jones, William K. (31 October 2005). DIGGING: GUIDELINES FOR CAVERS AND RESOURCE MANAGERS (DOC). National Cave and Karst Management Symposium. Albany. pp. 88–91. Retrieved 27 April 2024.
  8. Jones, William K. (31 October 2005). DIGGING: GUIDELINES FOR CAVERS AND RESOURCE MANAGERS (DOC). National Cave and Karst Management Symposium. Albany. pp. 88–91. Retrieved 27 April 2024.
  9. Roberts, Liz (3 January 2013). "Cave team details nine-hour rescue of man stuck in Ogof Ffynon Ddu". grough. grough. Retrieved 14 May 2024.
  10. Gardner, John. "Best Practice Capping Techniques". Braemoor. Retrieved 17 December 2015.
  11. Ronquillo, Wilfredo P. (June 1995). "Anthropological and Cultural Values of Caves". Philippine Quarterly of Culture and Society. 23 (2): 138–150. JSTOR   29792183 . Retrieved 28 April 2024.