Cave Diving
Cave diving is underwater diving in caves which are at least partially
filled with water. 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 specialized configurations. 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 decompression.
In the United Kingdom it is an extension of the more common sport of
caving, and in the United States an extension of the more common sport of scuba
diving. Compared to caving and scuba diving, there are relatively few
practitioners of cave diving. This is due in part to the specialized equipment
(such as rebreather diver propulsion vehicles and dry suits) and skill sets
required, and in part because of the high potential risks, including decompression
sickness and drowning.
Despite these risks, water-filled caves attract scuba divers, cavers,
and speleologists due to their often unexplored nature, and present divers with
a technical diving challenge. Underwater caves have a wide range of physical
features, and can contain fauna not found elsewhere.
History
Jacques-Yves Cousteau, co-inventor of the first commercially successful
open circuit scuba equipment, was the world's first scuba cave diver. However,
many cave divers’ penetrated caves prior to the advent of scuba with surface
supplied breathing apparatus through the use of umbilical hoses and
compressors. Scuba diving in all its forms, including cave diving, has advanced
in earnest since Cousteau introduced the Aqua-Lung in 1943.
There are three main classifications of diving: cave diving, open-water
diving and cavern diving. Open-water diving is where all divers start gaining
experience, and it's defined as a dive in which linear access to the surface is
directly available -- in other words, by swimming straight up, a diver should
be able to get a head above water, and sunlight is easily visible. In cavern
diving, on the other hand, a diver is exploring permanent, naturally occurring
caverns and has a ceiling overhead, but an entrance and visible light from the
sun are in sight. Both open-water diving and cavern diving are considered
recreational activities that require recreational-level certifications and
training, and divers usually limit descents to 130 feet.
Cave diving differs from the other two types of diving in that it's a
form of technical diving instead of a recreational one. It requires a much
different set of equipment and several years of training and certification, and
professionals constantly stress the need for top-notch fitness and gear. But
above all, they admire cave diving for its unique challenge and the potential
to discover the undiscovered -- scientific research gathered from cave dives
can lead to the study of rare organisms and even offer cures to diseases like
leukemia.
Cave
Diving Techniques
Moving around the
cave
Since cave diving is different from other recreational diving
activities, many of the techniques people use are also much different. Divers
are taught to swim in a prone, or face down, position, with the knees bent and
the fins elevated above the plane of the body. This is mainly a precaution
against kicking the bottom of a cave and stirring up sediment, but it also
offers a good streamline and creates little resistance to the water.
Cave divers move about a cave by using a simple technique called
"pull and glide" -- using the tips of their fingers, divers look for
crevices in rock for a place to hook onto. The rock is usually something hard
and porous like limestone, so it should have lots of pockets and places to
grab. After grabbing hold, divers pull and release, gliding through the cave
with relative ease.
Cave divers learn how to use mostly their feet for directional changes
along with short flutter kicks, and, in the case of solid limestone, some can
push off a cave ceiling with their feet to propel themselves along.
Divers can also take along battery-powered diver propulsion vehicles
(DPVs) to make swimming easier. Although there are many different types,
tow-behind DPVs are the most common, which pull divers through caves. DVPs help
divers use less oxygen since they're not exerting themselves as much, and they
can significantly increase the length of a dive.
Guidelines
Because there is little to no visibility in caves and cave divers must
use their own source of light, guidelines must be placed to ensure people can
find their way back to a cave's entrance.
Most caves already have guidelines in place from past explorers -- these
are called "gold lines" because of their yellowish color. They
consist of braided nylon string and are usually a bit smaller in diameter than
regular rope at about an eighth of an inch. These are placed throughout the
main tunnels of a cave. Labyrinthine caves also have smaller side tunnels, and
these are provided with smaller, white lines. They don't contact the main line;
instead, they usually end within 5 to 10 feet of the main line.
The main line of a cave does not extend to the exit -- this prevents
open-water divers or untrained or uncertified people from viewing it as an
invitation to enter the cave. Therefore, a main guideline typically starts 50
to 100 feet inside a cave.
Still, it's a cave diver's responsibility to run a temporary line, or
entry line, along a reel from the outside of the cave in order to maintain a
continuous guideline from open-water to the main line. This provides direct
access to a cave's exit. To make an entry line, divers make an initial tie-off
to something sturdy, like a big rock. A secondary tie-off is also made in case
the first one comes loose. The diver must be able to swim along the line with
his hand around it, making an "OK" sign, and with his eyes closed
make his way out of the cave. The line shouldn't be run near obstructions in
order to avoid snags and keep out of the way of other divers.
Dorf markers, or small, plastic directional arrows, can be tied to
lines. These point toward exits, just in case a diver becomes disoriented.
Clips, markers that resemble clothespins, are also used at points for notation
reasons, including max penetration (the furthest point reached inside the cave)
and points of interest for other divers.
The average cave dive will last in excess of one hour, but some can last
for as long as 15 hours if the right equipment and gas supply is available.
Divers generally use what's called the "rule of thirds" -- when one
third of a diver's air supply is gone, he will stop the dive and begin moving
toward the cave's entrance.
Cave diving venues
Grand Bahamas Island
The caves and caverns of Grand Bahamas
contain an immense underwater cavern with a vast flooded labyrinth of caverns,
caves and submerged tunnels that honeycomb the entire island of Grand Bahamas and
the surrounding sea bed. The inland caves are not abundant with life, but do
contain creatures living in the caves other than the migrating gray snappers.
Residents of these caves include a type of blind cave fish and remipedia that
don't pose any threat to cave divers.
The caves in the Bahamas were
formed during the last ice age. With much of the Earth's water held in the form
of glacial ice, the sea level fell hundreds of feet, leaving most of the Bahamas
banks, which are now covered in water, high and dry. Rain falling on the most
porous limestone slowly filtered down to sea level forming a lens where it
contacted the denser salt water of the ocean permeating the spongy lime stone.
The water at the interface was acidic enough to dissolve away the limestone and
form the caves. Then, as more ice formed and the sea level dropped even
further, the caves became dry and rainwater dripping through the ceiling over
thousands of years created the incredible crystal forests of stalagmites which
now decorate the caves. Finally, when the ice melted and the sea level rose,
the caves were reclaimed by the sea.
Central and Northern Florida, U.S
The largest and most active cave
diving community in the United States is in north-central Florida. The North Floridan
Aquifer expels groundwater through numerous first-magnitude springs, each
providing an entrance to the aquifer's labyrinthine cave system. These
high-flow springs have resulted in Florida cave divers developing special
techniques for exploring them, since some have such strong currents that it is
impossible to swim against them.
The longest known underwater cave
system in the USA, The system, near Tallahassee, Florida, has
multiple interconnected sinks and springs spanning two counties (Leon &
Wakulla). One main resurgence of the system, Wakulla Springs, is explored
exclusively by a very successful and pioneering project called the Woodville
Karst Plain Project (WKPP), although other individuals and groups like the US
Deep Cave Diving Team, have explored portions of Wakulla Springs in the past.
One deep underwater cave in the
USA is Weeki Wachee Spring. Due to its strong outflow, divers have had limited
success penetrating this first magnitude spring until 2007, when drought
conditions eased the out-flowing water allowing team divers from Karst
Underwater Research to penetrate to depths of 400 ft (120 m) The current
deepest known underwater cave in the USA is Phantom Springs Cave located in
west Texas. Phantom Springs has been explored down to 462 feet in water filled
cave passages. This makes it the deepest underwater cave in the USA as of 2013.
The Florida caves are formed from
geologically young limestone with moderate porosity. The absence of speleothem
decorations which can only form in air filled caves, indicates that the flooded
Florida caves have a single genetic phase origin, having remained water filled
even during past low sea levels. In plan form, the caves are relatively linear
with a limited number of side passages allowing for most of the guidelines to
be simple paths with few permanent tees. It is common practice for cave divers
in Florida to join a main line with a secondary line using a jump reel when
exploring side passages, in order to maintain a continuous guideline to the
surface.
Yucatan Peninsula, Mexico
While there is great potential for
cave diving in the continental karst throughout Mexico, the vast majority of
cave diving in Mexico occurs in the Yucatán Peninsula. While there are
thousands of deep pit cenotes throughout the Yucatán Peninsula including in the
states of Yucatán and Campeche, the extensive sub-horizontal flooded cave
networks for which the peninsula is known are essentially limited to a 10 km
wide strip of the Caribbean coastline in the state of Quintana Roo extending
south from Cancun to the Tulum Municipality and the Sian Ka'an Biosphere
Reserve, although some short segments of underwater cave have been explored on
the north-west coast (Yucatán State).
In the Yucatán Peninsula, any
surface opening where groundwater can be reached is called cenote, which is a
Spanish form of the Maya word d’zonot. The cave systems formed as normal caves
underwater, but upper sections drained becoming air filled during past low sea
levels. During this vadose, or air filled state, abundant speleothem deposits
formed. The caves and the vadose speleothem were subsequently reflooded and
became hydraulically reactivated as rising sea levels also raised the water
table. These caves are therefore polygenetic, having experienced more than one
cycle of formation below the water table. Polygenetic coastal cave systems with
underwater speleothem are globally common, with notable examples being on the
Balearic Islands (Mallorca, Menorca) of Spain, the islands of the Bahamas,
Bermuda, Cuba, and many more.
As with all cave speleothems, the
underwater speleothems in the Yucatán Peninsula are fragile. If a diver
accidentally breaks off a stalactite from the ceiling or other speleothem
formation, it will not reform as long as the cave is underwater so active cave
conservation diving techniques are paramount.
In plan form, the Quintana Roo
caves are extremely complex with anastomotic interconnected passages. When cave
diving through the caves, the pathways then appear to have many offshoots and
junctions, requiring careful navigation with permanent tees or the implementation
of jumps in the guideline.
The beginning of the 1980s brought
the first cave divers from the U.S. to the Yucatán Peninsula, Quintana Roo to
explore cenotes such as , Naharon and Maya Blue, but also to central
Mexico where Resurgence Rivers such as Rio Mante, and sinkholes such as Zacaton
were documented.
In the Yucatán, the 1980s ended
with the discoveries of the Dos Ojos and Nohoch Nah Chich cave systems which
lead into a long ongoing competition of which exploration team had the longest
underwater cave system in the world at the time, with both teams vying for
first place.
The beginning of the 1990s led
into the discovery of underwater caves such as Aereolito on the island of
Cozumel, ultimately leading to the 5th biggest underwater cave in the world.
United Kingdom
UK requirements are generally that
all people wishing to take up cave diving must be competent cavers before they
start cave diving. This is primarily because most British cave dives are at the
far end of dry caves. There are individuals that begin cave diving directly
from the recreational diving, but they represent a minority in the UK, and
represent only a few percent of the Cave Diving Group (CDG).
Australia
Australia has many spectacular
water filled caves and sinkholes, but unlike the UK, most Australian cave
divers come from a general ocean-diving background.
The "air-clear" water
conditions experienced in the sinkholes and caves found in the Lower South East
(now called the Limestone Coast) of South Australia (SA) has attracted many
visiting divers with the first cave and sinkhole dives taking place in the very
late 1950s. Until the mid-1980s divers generally used single diving cylinders
and homemade torches, and reels, resulting in most of their explorations being
limited. Mixed-gas and rebreather technologies can now be used in many sites. The
area is usually known within the cave diving community as the Mount Gambier
region.
A series of incidents between 1969
and 1974 in the former Lower South East of SA in which 11 divers died
(including a triple and a quadruple fatality) in the following four karst
features - Kilsbys Hole, Piccaninnie Ponds, Death Cave (also known as Alleyns
Cave) and The Shaft - created much public comment and led to the formation of
the Cave Divers Association of Australia Inc. (CDAA) in September 1973. The
introduction of a testing program by the CDAA in 1974, which involved the
assessment of prospective cave divers' cave diving ability lead to a reduced
fatality rate. In 1989, this testing system was replaced by a training system
which currently consists of 3 levels of qualification - Deep Cavern, Cave and
Advanced Cave. Five further deaths have occurred since 1974; two died at
Piccaninnie Ponds in 1984, one person died at Kilsbys Hole in 2010, and two
people died in separate incidents at Tank Cave in 2011 including noted cave
diver Agnes Milowka.
During the 1980s, the Nullarbor
Plain was recognized as a major cave-diving area, with one cave, Cocklebiddy,
being explored for more than 6 kilometers, involving the use of large sleds to
which were attached numerous diving cylinders and other paraphernalia, and
which were then laboriously pushed through the cave by the divers. In more
recent years divers have been utilizing compact diver-towing powered scooters,
but the dive is still technically extremely challenging.
A number of other very significant
caves have also been discovered during the past 20 years or so; the 10+
(Lineal) kilometer long Tank Cave near Millicent in the Limestone Coast, other
very large features on the Nullarbor and the adjacent Roe Plain as well as a
number of specific sites elsewhere, and nowadays the cave diving community
utilizes many techniques, equipment and standards from the U.S. and elsewhere.
The CDAA is the major cave diving organization
in Australia and is responsible for the administration of cave diving at many
sites. All cave diving in the Limestone Coast as well as at some New South
Wales sites and the Nullarbor requires divers to be members of the CDAA,
whether in the capacity of a visitor or a trained and assessed member. A number
of other organizations participate in cave diving activities within Australia.
The Australian Speleological Federation Cave Diving Group which was formed in
2005 coordinates projects focused on exploration and mapping at sites throughout
Australia. The following diving training organizations offer courses in various
aspects of cave diving via instructors either resident in Australia or visiting
from overseas - Global Underwater Explorers, International Association of
Nitrox and Technical Divers and Technical Diving International.
Brazil
In Brazil there is cavern diving
in Chapada da Diamantina, in Bahia state; Bonito, in Mato Grosso do Sul state;
and Mariana, where there is also cave diving (visiting Mina da Passagem), in
Minas Gerais state. For cave diving in Mariana a cave diver certification will
be required.
Sardinia Italy
In the north west of Sardinia,
close to Porto Conte bay, Alghero territory, there is the most important cave
diving site in the Mediterranean Sea. Thanks to the huge limestone cliffs of
Capo Caccia and Punta Giglio there are more than 300 caves above and below
water, with about 30 large, and many smaller, underwater sea caves. The Nereo
Cave is the most important and it is considered also the largest in the
Mediterranean Sea. On the east side of Sardinia there are many underwater cave
systems starting from the Gennargentu Mountains, with underwater rivers which
arrive at the sea by different, lengthy routes. Here one of the deepest fresh
water caves exits at more than 110 m (360 ft) depth.
Cala Golone is a departure point
for cave diving in Sardinia's largest cave systems which are usually reached by
sea. Bue Marino is the longest known, and there are several others with various
lengths and depths.
West Timor, Indonesia
There are a number of freshwater
filled cave sites located near and within Kupang, the principal city in West
Timor and the provincial capital of East Nusa Tenggara. At least 2 sites have
been described: Gua Oehani (translates as the Oehani Cave) and Gua Kristal
(translates as the Crystal Cave).
As of 1999, there was no
requirement to hold cave diving certification to dive either of these sites.
However, competence equivalent to CDAA Advanced Cave and Cave/Advanced Cave
appears to be respectively appropriate for these sites.
Dominican Republic
There is a growing number of known
water filled caves in the Dominican Republic, spread all over the island.
Regions with underwater caves include Santo Domingo, Pedernales, Cabrera,
Bayahibe and others.
Active exploration is being
conducted by the Dominican Republic Speleological Society which is working
together with local institutions as well as international scientists to further
explore all the cave systems possibilities and focusing in the preservation.
The longest known cave in the
island is El Toro which is about6, 000 ft (1,800 m) in length.
The best known caves in the island
are Cueva Taina, El Tildo, El Chicho and El Dudu, which have easy access to the
water and with a good level of safety outside of the water as they are in
private properties or national parks.
Cave diving is playing a very
important role in science in the DR, {in the last 3 years the DRSS team
together with international scientists and "Museo del Hombre
Dominicano" has found a new species of cave bacteria, a number of new and
extinct bat species, the first evidence of extinct crocodiles in the DR, fossil
snakes, birds, sloths and remains of long extinct monkeys and other ancient
cave life. DRSS has cataloged over 120 new springs all over the island in which
many have caverns and cave systems attached.
Each diver carries a powerful primary light. The canister contains a lead-acid "gel cell" of 6.5 AH (shown left), 9AH or 14 AH capacity and is worn on the harness. The light head is a 10W High Intensity Discharge unit and is connected via a wet connector which can be plugged and unplugged under water.
Waterproof notebooks, or "Wet Notes" are used for a number of purposes. One use is for communication under water, and another is to record reference information during the dive, either to help with navigation inside the cave or for later analysis and planning of subsequent dives.
Cave
Diving Equipment
The best way to tell a cave diver apart from an
open-water diver or cavern diver is to look at the equipment in use. In this
section we'll look at the different kinds of gear a cave diver brings on a
dive.
It's important to remember that cave divers carry
redundant equipment -- this means that for every piece of equipment they carry,
an extra will come along for the dive. This is to make sure that if something
undergoes failure, there's a replacement to take over and allow a safe return
to the surface. It could be something seemingly unimportant like an extra mask,
or a piece of equipment that ensures a diver's survival, like an oxygen tank.
1. Masks
While open-water divers usually use snorkels because
they can easily reach the surface for air, cave divers could never afford to
bring one along and have no use for it. Cave divers stay submerged in the water
for long periods of time, and therefore bring along oxygen tanks for breathing
purposes -- a snorkel would only create excess weight and extra drag.
Cave divers usually keep masks simple, preferring
standard masks that are solid black. The reason dark masks are well suited for
cave diving is because of the light-absorbing qualities of the color black. Any
distracting light that might leak into the mask can be absorbed by the dark
material of the mask and prevent a diver from losing sight of entrances or
important spots. Cave divers also wear hoods made of nylon to protect their
heads from water leaks and damage during dives.
2. Fins
Cave divers typically prefer black rubber fins, and ones that aren't very flexible. Light, stiff fins work best because divers already so carry much mass with them into a cave. Moving through the water, they need to use short, controlled kicks to avoid stirring up any sediment on the floor of a cave.
Cave divers typically prefer black rubber fins, and ones that aren't very flexible. Light, stiff fins work best because divers already so carry much mass with them into a cave. Moving through the water, they need to use short, controlled kicks to avoid stirring up any sediment on the floor of a cave.
Stiff fins help cave divers move through the water
easier, while dry suits keep them warmer.
3. Suits
3. Suits
Cave divers use either dry suits or wet suits for
protection. The difference between the two kinds of suits is that dry suits are
designed to seal off water from entering and getting a diver's body wet. Made
of a synthetic rubber called neoprene, dry suits are the preferred choice for
cave divers because they allow much less heat loss. The material is
double-layered with a small space in between for insulating air, and divers
have the option of wearing extra undergarments. Wet suits will still suffice
for shorter dives and warmer waters, however.
Other equipment such as flashlights and small knives
to cut away snags come along on a dive. There are also several gadgets that
help divers during their ascent and descent. Different gauges give information
on air pressure and depth, and they may all be fitted onto one device along
with a compass for navigation.
Cave divers, of course, need to bring oxygen tanks,
or cylinders, with them while underwater. To learn about breathing in deep,
high-pressure water, read the next page.
4. Depth gauge and timer
Every diver carries at least one depth gauge and
timer. These allow the diver to calculate what decompression stops to make when
ascending at the end of the dive, using standard decompression tables.
Alternatively, all of these functions may be combined in a dive computer which
indicates depth, time and the required decompression stops.
5. Tanks, Back plate & Harness
The heart of a cave diver's equipment is the
"doubles". These are two tanks held securely together by steel bands,
and connected together by a manifold. The manifold has two outlets, each of
which can be turned on or off independently in case of problems. The center
knob allows the two tanks to be isolated if a problem cannot be solved by
turning off one outlet.
Two fully independent air regulator systems are
attached to the outlets of the manifold.
Each regulator system has a "first stage", which reduces the
pressure from approximately 200 atmospheres to about 10 atmospheres, and a
"second stage" (the mouthpiece) which supplies air on demand at
ambient pressure. A long hose on one
regulator allows divers to share air if necessary while swimming in line
through narrow caves.
A buoyancy compensation device, or "wing",
is attached to the tanks. This is essentially an airtight bag which can be
inflated to provide buoyancy. Valves allow air to be injected from the tanks or
from the diver's mouth to increase buoyancy, or to be released to reduce
buoyancy.
Valves allow air to be injected from the tanks or from
the diver's mouth to increase buoyancy, or to be released to reduce buoyancy.
The back plate and harness bolt onto the doubles and
holds the wing in position.
The harness is made from nylon webbing threaded
through the back plate and holds the equipment firmly in place on the diver.
6. Safety Equipment
Each diver carries a powerful primary light. The canister contains a lead-acid "gel cell" of 6.5 AH (shown left), 9AH or 14 AH capacity and is worn on the harness. The light head is a 10W High Intensity Discharge unit and is connected via a wet connector which can be plugged and unplugged under water.
Primary lights fail fairly
frequently, perhaps every 50 to 100 dives.
Each diver, therefore, also carries two backup lights. These are extremely reliable, and provide
sufficient light to exit the cave if all primary lights fail. The backup lights are clipped onto D-rings on
the diver's harness.
Also attached to the
harness is a short, sharp knife. This
allows the diver to cut himself free in the event of entanglement in the
guideline or other equipment. It is
common for cave divers to carry more than one knife--we normally attach another
knife to the handle of the light head.
Cave divers place
directional markers (arrows) and non-directional markers (circles) on the
guideline to record information.
Directional markers point to the nearest exit from the cave, and
non-directional markers are used for a number of purposes, including marking
the entrance route.
Each diver always carries a small reel or spool of nylon line known as a "safety reel". This is used when conducting a search for a lost guideline or fellow diver, and to repair any breaks in the guideline.
Each diver always carries a small reel or spool of nylon line known as a "safety reel". This is used when conducting a search for a lost guideline or fellow diver, and to repair any breaks in the guideline.
Waterproof notebooks, or "Wet Notes" are used for a number of purposes. One use is for communication under water, and another is to record reference information during the dive, either to help with navigation inside the cave or for later analysis and planning of subsequent dives.
7. Breathing Gasses
Air was the first gas used for scuba diving. It
consists of about 21% oxygen and 79% nitrogen. The high nitrogen component
limits the use of air. The reason is that the nitrogen is absorbed by the body
tissues while diving, and can cause bubbles to form when the diver surfaces. In
addition, the nitrogen acts as a narcotic at depths below about 30 meters,
affecting the diver's judgment and performance.
For most of our dives we, therefore, use a gas mixture
known as Nitrox 32%. This contains 32%
oxygen and only 68% nitrogen. The lower
nitrogen content reduces the amount of nitrogen which is absorbed by the body,
reducing the risk of bubble formation.
The mixture is still narcotic under pressure, and the high oxygen
content can be toxic at depth. This limits
the safe use of Nitrox 32% to depths of about 30 meters.
To help eliminate any bubbles during ascent, we make a
number of decompression stops at different depths during the ascent. For the final stop at six meters, we breathe
pure oxygen which rapidly eliminates bubbles.
Risks of oxygen toxicity limit the use of pure oxygen to a depth of six
meters.
For dives deeper than 30 meters, the narcotic effect
of the nitrogen can be avoided by replacing it with another inert gas: helium.
A typical mixture for depths up to 60 meters would be "20/50"
- this consists of 20% oxygen, 50% helium, and 30% nitrogen. Mixtures of oxygen, helium and nitrogen are
called Trimix.
Dives below 60 meters require special
considerations. The amount of nitrogen
must be reduced to a very low level in order to avoid narcosis. To prevent oxygen toxicity the amount of
oxygen must be reduced as well. A
typical mixture for dives up to 120 meters would be 10/70, containing 10%
oxygen, 70% helium and 20% nitrogen.
Breathing such a mixture at shallow depths would result in insufficient
oxygen supply for the body and must be avoided.
8. Stage Tanks
When the breathing gas requirement exceeds the
capacity of the doubles, extra gas can be carried in so-called stage tanks.
Stage tanks are fitted with clips to fasten the tank to the diver's harness.
Stage tanks can also be left clipped to the guideline - this is common on very
long dives, to provide an additional safety margin during the exit.
Stage tanks are also used when different gas mixtures
must be carried, most commonly for oxygen. When diving with several gases, it
is important that no gas is taken deeper than its maximum safe operating depth.
Each stage tank has a regulator system attached,
consisting of one first stage, one second stage, and a pressure gauge to show
the tank contents. When not in use, the second stage and hoses are secured
neatly in rubber tubes around the tank.
Normal swimming speed for a cave diver is 15-20 meters
per minute. We use diver propulsion vehicles (DPVs or "scooters")
when large distances must be covered, or when lots of equipment must be
carried. These are capable of pulling a fully equipped cave diver with several
stage tanks at speeds of 50-60 meters per minute. The small scooters have a
range of about three kilometers, and the larger scooters have a range of about
six kilometers. The scooters are powered by several large lead-acid get cells
housed in the tubes.
The photo to the right shows an exploration diver with
a scooter and one stage tank. This
equipment configuration is suitable for cave penetrations of up to about two
kilometers. For longer penetrations we
take two or three stage tanks and tow a second scooter behind us. This allows penetrations of up to about five
kilometers. Whenever we use scooters, we
allow sufficient reserve breathing gas to swim out from the furthest point if
all scooters fail.
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