WEBVTT

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Russia's Kola Peninsula, 1992.

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Geophysicist David Smythe takes a video camera onto the
rig floor of the Kola Superdeep Borehole.

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Workers handle pipe beneath a forest of steel.

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Smythe identifies the operation as an attempt to retrieve
dropped drill pipe.

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This is a hole that has already gone more than twelve
kilometres into the Earth.

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And the job in front of the crew is getting equipment
back.

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That is where the story of superdeep drilling gets
interesting.

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What did people go down there to find?

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What did the rock actually do?

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And what finally made the next metre too difficult, too
expensive, or no longer necessary?

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This is a tour of some of the major holes that tested
those limits, from scientific experiments to the search
for deep gas.

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First, one distinction.

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Measured depth follows the hole, including its bends.

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Vertical depth measures how far down you have gone.

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A long well can travel mostly sideways.

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At sea, the water above the seabed is another separate
measurement.

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We'll keep those quantities separate, and use reported
drilling depths without turning them into a misleading
league table.

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Before Kola, there was Project Mohole.

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American researchers wanted to drill through the oceanic
crust toward the mantle.

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The ocean offered a tempting advantage: the crust there is
much thinner than beneath the continents.

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It also put kilometres of moving water between the rig and
the rock.

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In 1961, a converted drilling barge worked near Guadalupe
Island, off Mexico.

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The deepest test penetrated about a hundred and
eighty-three metres beneath the seabed, below roughly
three and a half kilometres of water.

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It recovered basalt.

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The achievement was learning to drill from a floating
platform in deep water, with the much deeper scientific
objective still ahead.

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Holding position, losing equipment and keeping holes open
were difficult.

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Costs and management became problems too.

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Congress ended funding in 1966.

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Mohole never reached its intended boundary.

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Here, the stopping point was set above ground, before the
central geological question could be answered.

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Kola began in 1970, in the Soviet Union, with an ambitious
fifteen-kilometre design.

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The site put ancient crust within reach of the drill.

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Researchers wanted physical samples and measurements to
test their interpretation of the deep Earth.

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They also wanted to understand the mineral potential of
the nickel-bearing Pechenga region.

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The hole passed through a thick volcanic and sedimentary
sequence, then into older metamorphic basement below about
six point eight kilometres.

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Gneiss, amphibolite and other crystalline rocks
complicated the simple picture inferred from seismic
waves.

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A change in wave speed did not necessarily mark the neat
granite-to-basalt boundary that researchers had expected.

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That matters because a seismic section is an
interpretation.

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Drilling gives you a sample to test it against.

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Rock composition, deformation and fluids in fractures can
all affect the signal.

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Kola helped show how much information was hidden inside
what had looked like a straightforward boundary.

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The deeper crust contained a more complicated combination
of rocks and fluid-bearing structures.

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The engineering assumptions were being tested too.

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Temperatures rose more than expected.

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The deeper rock was difficult to keep open, and equipment
became stuck or broke.

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After one major accident in 1984, the researchers'
retrospective describes kilometres of drill string left in
the hole.

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Reaching a record once did not mean the crew could simply
continue downward from it.

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When equipment is lost downhole, drillers call it a fish.

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They try to catch it with another tool and pull it free.

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If that fails, they may plug back and steer a new branch
around the obstruction.

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The rig can spend days working without making the well any
deeper.

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A depth record hides all those metres drilled, abandoned
and drilled again.

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That brings us back to Smythe's camera in 1992, and the
attempt to retrieve dropped pipe.

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Here is David Smythe recalling the operation for BBC
Witness History in 2024.

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[David Smythe, recorded 2024] And before you can do any
more drilling, you had to recover that. They were doing
what they call a fishing expedition.

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Kola's famous reported depth is about twelve point two six
kilometres.

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It stopped short of the fifteen-kilometre design.

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The account written by Kola researchers places the end of
drilling in 1992, amid a drastic loss of funding.

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Heat, unstable ground and repeated recovery work had made
progress difficult; the financial collapse then removed
the ability to keep trying.

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But the end of deepening was not the end of every
investigation.

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German research records document a Kola hydraulic project
funded from 1998 to 2001.

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The site was later mothballed and its drilling
infrastructure dismantled.

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The end of drilling, the later research and the closure of
the working site were separate chapters.

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Now to Oklahoma's Anadarko Basin, where the objective was
commercial hydrocarbons.

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The Baden well passed thirty thousand feet in 1972.

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Its deep Hunton test did not establish the hoped-for
commercial result.

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Bertha Rogers followed, with the Hunton dolomite again a
major target.

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These were expensive attempts to find a working reservoir
beneath a very thick stack of sedimentary rock.

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The drilling fluid had a difficult job.

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It needed enough pressure to hold back deep gas, while
other formations could take that fluid away.

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Unstable shales could fall into the hole.

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Heat changed the mud's behaviour.

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The operational account describes constant testing and
adjustment.

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The challenge was managing the whole open hole, not just
cutting the rock at the bottom.

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In 1974, Bertha Rogers reached a reported total depth of
thirty-one thousand, four hundred and forty-one feet:
about nine point five eight kilometres.

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Near the bottom, high pressure and sulfur-bearing fluids
complicated the ending.

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The United States Geological Survey records sulfur
crystals coming to the surface after the overpressured
well was brought under control.

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The deepest rocks did not become Bertha's producing
reservoir.

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Gas production came from the much shallower Atokan granite
wash.

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Baden also had shallower completion work after reaching
total depth.

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Stopping the downward advance could be followed by another
phase of the well's life.

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A depth record, a successful geological test and a
productive completion are three different measures of
success.

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In Bavaria, Germany's Continental Deep Drilling Programme,
KTB, returned to the scientific questions.

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How hot is the crust?

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How much stress does it carry?

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Where can fluids move?

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The site lay in metamorphic rocks shaped by an ancient
continental collision.

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The team drilled a four-kilometre pilot hole before
starting the main borehole in 1990.

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The pilot supplied core and practical warnings.

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Steeply tilted rock fabric made a straight hole difficult
to maintain.

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Under stress, parts of the borehole wall broke away.

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In the main hole, deeper sections also narrowed with time.

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Researchers identified this convergence as a particularly
serious obstacle below about seven and a half kilometres.

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Think about the clearance around the drill pipe.

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It only has to disappear in one troublesome section to
trap the assembly.

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A harder bit cannot solve that.

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The crew needs a hole that stays open, drilling fluid that
works with the formation, and enough room to install
protective casing or a liner.

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Each recovery operation consumes time and money.

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At about seven and a half kilometres, temperature exceeded
the tolerance of the electronics in KTB's automatic
vertical-drilling system.

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The near-vertical path became harder to maintain.

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Stuck assemblies and unstable sections forced repeated
liners and sidetracks.

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The contemporary operational account describes the
remaining funds running low.

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In October 1994, deepening ended at a reported nine
thousand, one hundred and one metres.

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The well recorded more than two hundred and fifty degrees
Celsius near its bottom.

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But saying that heat alone stopped KTB leaves out the
failing hole and the budget.

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A drilling system has many limits.

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The first one you meet can make the others more expensive
to manage.

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KTB's afterlife is part of its achievement.

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The boreholes became a deep laboratory.

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The cores remained available for new questions, and
experiments could examine stresses and fluids in place.

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Ending the drilling phase preserved a scientific asset.

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A useful hole can keep producing knowledge long after it
stops producing new metres.

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The story continues in China.

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In the Tarim Basin, Shendi Taqe One combined scientific
exploration, oil and gas questions, and a test of
deep-drilling equipment.

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Drilling finished on January fifth, 2025, at a reported
ten thousand, nine hundred and ten metres.

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The rock was part of the problem.

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Hard dolomite with chert inclusions damaged the bits.

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Crews also battled drill-string fatigue, unstable
intervals and drilling fluid escaping into the rock.

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The operator's account says the last nine hundred and ten
metres took more than three hundred days.

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The deepest stretch consumed a disproportionate share of
the effort.

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Why stop there?

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The drill had reached ancient Cambrian source rocks.

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The operator said the required scientific information had
been gathered and hydrocarbon shows had been found.

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Going deeper added risk.

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The decision was to end deepening and move into testing
and further research.

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A hydrocarbon show still needs testing before anyone can
call it a commercial discovery.

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A newer research paper reports Xin'an One, in the Junggar
Basin, completed in October 2025 at eleven thousand, one
hundred and fifty-six metres total depth.

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It tested deeply buried clastic rocks.

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Reservoir quality was generally poor, although the team
identified more promising intervals and oil and gas shows.

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The gas analysis pointed to highly mature, coal-derived
gas.

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Testing was still being planned in 2026.

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And Shendi Chuanke One, in Sichuan, passed ten thousand
metres in October 2025.

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Its goals include deep petroleum geology and equipment
development.

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By our November 2026 cutoff, that is the latest confirmed
milestone in the operator's account.

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A final depth and outcome have yet to be established in
that record.

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This part of the story remains open.

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These projects did not encounter a single universal depth
limit.

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Mohole lost its funding.

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Kola combined difficult drilling with the loss of
financial support.

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Oklahoma's wells could seek production higher in the
section.

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KTB stopped amid hole instability and dwindling funds,
then continued as a laboratory.

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Taqe's team judged that the next stage should be testing
what the well had already reached.

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The useful question is what we need from the next metre,
whether we can keep the hole usable, and whether the
answer is worth the work.

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This is GeoNavigate Industry Chatter.

