Cave Diggers Simplified cave survey methods and mapping
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A survey is the only way you can find out how deep your cave is and where it is going. It is
a guide that indicates where to look for a continuation or passages that are likely to connect
with nearby caves. A high quality survey is ‘proof’ of a cave, indeed many cavers will not
even believe a cave exists until they have seen a good map of it!
Survey instruments
Vertical caves are typically steep, irregular and often confined, not to mention cold, wet
and dirty. Obtaining an accurate representation on paper is never simple. In all but the
easiest caves, hand-held instruments are the most suitable, if not the only alternative.
Sophisticated tripod mounted instruments such as theodolites and total stations are
impractical due to their inability to take steep sightings and setting up constraints.
The instruments must be light, compact and easy to carry. They must be fast to use and
allow you to take sights in any direction with minimal loss of accuracy. Even so, surveying is
painfully slow and takes five to ten times as long as a normal trip through the cave.
Tape and compass
A Suunto KB-14/360RT sighting compass and PM360PCT clinometer with a fibreglass tape are
the ‘International Standard’ for vertical caves. Both the compass and clinometer are neat
units in solid aluminium blocks and are robust enough to survive a considerable beating.
Contrary to their appearance though, Suuntos are far from waterproof and only a minor
dunking or even an unusually humid cave can cause the insides to mist up and render them
unreadable. An immediate solution that sometimes works is to warm them over a carbide
lamp flame. Careful, the plastic parts do burn and the mist usually reappears as the
instrument cools. You can reduce the risk of condensation by warming instruments to or
above the cave temperature before you use them – carry them in an inside pocket. Limited
waterproofing has been achieved by covering all joints in the instruments with epoxy resin.
They then leak more slowly.
After each day’s surveying, bring the Suuntos out of the cave and dry them in the sun, jar
of silica gel or carbide. At special request to the manufacturer it is possible to buy them
with small screw-in plugs in the side that you can remove to simplify drying. Other
compasses such as the Silva 54NL and a similar Suunto KB-77 model have a direct sighting
lens on top of the instrument that cannot mist up, making them far superior to the KB-14.
Complimentary clinometers are also available.
Suuntos are easy and fast to
read in the full light of day, but
once underground you need a
good light to see the face of the
dial clearly. In most cases it is
necessary to externally light the
face of the instrument. A
removable back-up or hand held
electric is ideal for this as it is
safer and easier than removing
your helmet for each reading.
Cavers often place a light hard
up against the instrument to
make the dial easier to read and
while this is fine for the
clinometer, the
electromagnetic effect and
steel components and magnetic
switches in the lamp will affect
the compass. Carbide lamps too,
may have enough steel pieces to
upset a compass. Keep any
lamps, battery packs or
generators a safe distance
away.
Always read the left side of a Suunto clinometer – the right is a percentage scale. Also
remember that the scale on the compass is backwards (right to left). Read sighting
compasses with one eye only to avoid the possibility of a 3° or more parallax error.
Suunto kit
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Most compasses only work well in a horizontal plane, or close to it. When you’re taking a
steep reading there is no option but to sight to an imaginary point above or below the
station. This is easier to do when sighting up rather than down and for the sake of accuracy,
avoid steep down-sights.
Use a 30 m PVC coated fibreglass tape in an open reel so that it will not clog with mud. Steel
tapes are heavy, break easily, difficult to use and may affect compass bearings.
Laser distance measurers
Tapes are rapidly being replaced by laser distance measurers. They
are very accurate, fast, sufficiently robust (although, clearly, not as
robust as a tape!), and very expensive. The original is the Leica
‘Disto’. As time goes on, more and more copies and new versions
with more features are appearing, such as the Hilti illustrated. It is
small, fast so that you don’t have to hold it on target for long and
has an excellent optical sight for use in sunlight where the laser spot
is often impossible to see. As I write, Leica has released the ‘A8’
with a built-in clinometer. It’s not cheap and still has no compass.
Like anything, you must use them correctly. You can measure a distance to almost anything,
so be careful that you are actually taking a distance to the station. The survey notebook
makes a good target. Lasers require extra care as they can damage your eyes. The target
holder should close their eyes or look away, while the instrument man should avoid shining
the laser at people’s faces. They are probably more dangerous while they are actually
measuring rather than when they are only ‘pointing’.
Topofil
In its simplest form a topofil consists of a small
box that contains a roll of thread and distance
counter. A topofil offers some advantages
over a tape:
• It is lighter.
• No distance limit between stations, which is
ideal for big pitches.
• The thread is sighted along, increasing the
accuracy of high angle compass shots.
More advanced topofils use a compass and
clinometer adapted to read along the thread
laid from one station to the next. These are a
separate unit or mounted in the topofil box
provided it contains no magnetic components.
Commercially available topofils specifically
for caving use are restricted to the Vulcain.
The Vulcain model is a complete unit with
detachable compass, however they are only
sporadically available from the Club Vulcain in
Lyon, France and as such are hard to get. This
rarity and design limitations make
constructing one a reasonable alternative.
Unlike Suuntos, topofils have no optical
sighting, therefore there is never a problem
with them misting up or the need to put your
head in strange positions to read them. They
are fast to use, can be operated by a single caver and with practise offer a degree of
accuracy unequalled in other hand-held survey instruments.
Topofils have more working parts than tape and require a light touch to run well. If you use
it roughly the thread can break or snag as it pays out and you need to open the instrument
to insert a new roll of cotton when the old one runs out.
Topofils leave a thread line throughout the cave that you must collect on your way out. Use
cotton thread so that if you accidentally leave any behind it will eventually rot.
Hilti PD-32
Topofil kit
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Electronic instruments
As an experiment, I have mounted an
electronic clinometer and electronic
compass onto a Disto. The unit is
something like a ‘digital topofil’, without
the thread. Once calibrated, the clino
and compass ‘sight’ along the laser
beam. Shine the laser at the target, press
the hold button on the clino, then the
hold on the compass, then take the
distance. You can now read off the
instruments at your leisure rather than at
some awkward angle. The procedure is
simpler than Suuntos, and not as easy as
a topofil, but you don’t have to look after
a thread. You also still risk the possibility
of a transcribing error between the
instruments and the book. Hopefully
you’ll make fewer errors transcribing the
digital readouts than you would for
analogue instruments.
The ultimate cave surveying instrument
is the much more sophisticated and even
more experimental. ‘Toposcan’ is made
by a French/Quebec group. It combines
the three instruments into a single unit.
A single press of button sends the
distance-compass-clino reading directly
to your Palm PDA—no more transcribing
errors. With a Toposcan it should at last
be possible to survey at a reasonable
speed, if you can find one.
iDigital ‘topofil’
TopoScan
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Tactics and procedure
‘Survey what you explore’ is a good rule and one that has caused many an argument when
broken. A reasonable compromise is to have one or two cavers rigging and a survey team
following along behind them. On the next trip the two teams can swap places.
For ease of understanding the data and its later reduction, it is best to maintain the survey
direction. If you begin the survey at the entrance of a cave you should continue down the
cave, starting each new day’s surveying at the end point of the day before or some other
known point along the way. Surveying down one day then the next day going past the end
point and surveying back to it leads to confusion. Consistently surveying from a known point
keeps survey data as a continuous series instead of a collection of little pieces that you have
to tack together or reverse to calculate the total displacement from the starting point. It’s
not that the data is ‘wrong’, just that easier to understand data means fewer problems later
outside the cave.
The data you collect will be easier to understand and therefore mistakes are less likely if
you take all survey sights in the same sense; either all forward sights looking in the direction
of travel or a series of backsights looking back along the cave just traversed, but not a mix
of both. If you’re forced to take a sight in the opposite sense, note it well in the data and
avoid mentally reversing it in the cave. A mistake could well be undetectable except that
in the final map, when something looks wrong.
direction of travel
Foresights are taken in the direction of travel. From station 1 to
2, then 2 to 3, 3 to 4, etc. It is the simplest, least
confusing method of gathering data, especially when
using tape and compass.
Backsights are taken facing opposite to the direction of travel.
From station 2 to 1, then 3 to 2, 4 to 3, etc. This is the
preferred method for topofils.
Fore and Backsights are taken in both directions from each
station. From station 1 to 2, the 2 to 1, 2 to 3, 3 to 2, 3
to 4, 4 to 3, etc. For maximum accuracy.
Leapfrog is taken in both directions alternately. From station 2
to 1, then 2 to 3, 4 to 3, then 4 to 5, etc It gives the
maximum survey speed for tape and compass and
minimises systematic errors.
direction of travel
direction of travel direction of travel
1
2
3
4
5
6 7
8
1
2
3
4
5
6 7
8
1
2
3
4
5
6 7
8
1
2
3
4
5
6 7
8
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Tape and compass
A team of three is the ideal for a tape and
compass survey: one to read the instruments,
one to manage the tape and a third to take the
notes and sketch the passage. If you use a Disto
instead of a tape, the instrument reader can also
use the Disto and the ideal team becomes two.
The note-taker is the ‘boss’ and in easy passage
the survey will move only as fast as the sketcher
can sketch, while in difficult passages the
instrument reader will be the rate determining
factor. When there are only two surveyors the
note-taker handles an end of the tape as well.
Tape and compass surveys are usually done as a
series of forward sights. In essentially ‘down’
caves however, it is far better to survey facing
uphill, taking ‘backsights’ so you can read the
compass more easily.
Begin the survey at a cave tag or marked point at
the entrance. The tape reader waits at the
entrance while the instrument reader runs the
tape down the cave and finds a ‘station’ from
which the tape reader is visible as well as
providing a good view toward the next station.
Measure the distance and perhaps move the
forward station a few centimetres so as to
coincide with a full decimetre on the tape. The
tape reader calls out the measurement to the
note-taker who repeats it.
The tape reader ‘lights’ the station by holding a
light on or behind it or by putting a finger on it
and lighting that. While lighting the station they
call out ‘left’, ‘right’, ‘up’ and ‘down’ estimates and rewinds the tape. Meanwhile, the
instrument reader sights the compass and calls the figure to the note-taker, who repeats it,
then the same for the clinometer. Before moving on they make sure that the note-taker
knows where the station is so that they can include it on the sketch. The instrument reader
then moves to the next station where the tape reader points out the station’s precise
location, leaves the end of the tape and moves down the cave in search of the next station.
The note-taker travels either between or behind the other two surveyors.
Reading a Suunto clinometer
Reading a Suunto compass
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Using a topofil
Topofil
A topofil survey is most efficient with two
surveyors: one to read the topofil and the other to
take notes. When a team is short-handed you can
do a topofil survey alone with no loss of accuracy
although it will be slower.
Topofil surveys run easily down a cave taking a
series of backsights and leaving a trail of thread
behind. If the thread breaks on a pitch or difficult
passage you can leave that one sight for the return
trip rather than having to do the pitch an extra
time.
The instrument reader begins by pulling out
enough thread to tie off to the entrance station
then calls out a ‘first topo’ to the note-taker, who
repeats it, then runs out a straight line of thread
to the next station. Preferably choose a small
projection you can later wrap the thread around,
that also has a view forward. After calling out the
distance, hold the topofil above the station or in
line between the stations and take a compass
reading and call it to the note-taker. Next, hold
the instrument beside or in line with the station
and take the inclination. The note-taker repeats
all readings. Be careful to ensure that the thread
is not snagged between stations and do not allow
it to sag while taking clinometer readings.
After you have taken the readings, wrap the
thread around the station two or three times by
pulling sufficient thread as stretch from the leg
that you’ve just measured.
Find the exact point on the thread by making a
mud mark on it at the correct point when the
distance is taken or by running the topofil past the
station until the thread begins to run and taking
the point on it where it passes the station. If there
are no projections to tie the thread to, anchor it
with a rock or ask the note-taker to hold it.
Clinometer reading
Finding the correct position on the thread
Taking the distance
Compass bearing
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New ways of surveying
New faster surveying instruments are shifting the balance so that the sketcher doesn’t have
a hope of keeping up. If you want a really detailed sketch you don’t have much choice but
to travel at the speed of your team artist. One option is to just neglect the sketch and use
the left, right, up and down data to computer generate the map. For large caves that will
be drawn at scales larger than 1:1000, this may well be adequate. Another approach is to
enter your data directly into a Palm PDA using Auriga software and plot as you go. All you
record on paper is the sketch and the Auriga plot helps a lot with that. With practise, this
could save you some time in the cave, and considerable time in the drawing up phase. If you
have time and resources you can take the data and mark the stations on one trip, then return
with a print of the line plot and sketch-in the details.
Thirty minutes later, against the same wall, as the instrument man and I fade off into the
calm world of hypothermia-induced sleep, we begin to dream of rainbows, lollipops, and
the cave collapsing on the sketcher. When we finally awake, another 30 minutes has gone
by and the sketcher has at last caught up with the survey. Disappointed by the lack of
sweets, happiness, and dead sketchers, we carry on to the next station. —Brandon Kowallis,
NSS News, August 2006.
Survey stations
Choose stations that give as long a sight as possible in each direction as well as being easy
and comfortable to reach while taking the sight. Don’t, however, exceed 30 m and for
accuracy, try to stay below 20 m. Stations should always be a fixed point on the wall, roof
or floor. This minimises station error and makes it possible to accurately mark points for
future use.
In complex caves, cave systems or areas with several separate caves, systematise the station
labels or names so that each survey is readily identifiable. Do this by assigning a unique
alphanumeric label for each station.
Eg. N 2 7 0 6
where:
N = letter to indicate the cave or area
within a cave
2 7 = two digits to indicate the day of the
expedition or date and thus identify
each section of the N survey
0 6 = two digits to indicate the station
number within the N27 survey
When you survey more than 100 stations in one day change the date numerals. ie. The
station after N2799 could be NB700 or N2800. All this information is not needed for each
station in the field. What is required is that you mark each page of data clearly with the
appropriate letter and number. In simple or isolated caves it is sufficient to assign station
numbers only. Other labelling schemes that provide unique station numbers also work. One
thing to avoid is to split a series and use the same series of labels in two distinct sections of
caves. This easy leads to confusion as it is quite natural to assume that like numbered items
will be near each other.
Mark some stations such as those at junctions and the end of a day’s surveying. Do so in some
semi-permanent manner such as a strip of note paper or flagging tape tied to the station or
a cairn built with one of its rocks bearing the station number written in carbide. There is no
need to go through and label each station nor is it necessary to write station numbers on the
cave walls. When you label a station write the complete station number so as to make it
readily identifiable should another survey connect to it.
Before entering a cave to continue a survey, note down the tie-in station and the correct
series of station labels you will use that day.
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Surface surveys
At the cave entrance, ‘tie’ the survey to a permanent station whether it be a tag, painted
number or point chipped into the rock. Later you can locate the exact position of the cave
entrance by surveying to some known point such as another cave tag, local bench mark, trig
point, corner of a building marked on a topographic map of the area or fix the point using
GPS.
In some areas it is valuable to survey to the resurgence of the cave be it proved or only
suspected so as to give a more precise estimate of depth potential than is available from
some topographic maps.
Use Suuntos or more accurate instruments for surface survey and only use topofils to
measure the distance component. Even a light crosswind will displace a topofil thread
enough to give a compass error of several degrees.
In open country it may be difficult to use fixed stations that are not on the ground. Rather
than lay on the ground for each leg, sight to a vertical stick with a bright mark on it at the
same height off the ground as the instrument reader’s eye level. Take length measurements
with a tape, topofil or rangefinder. Laser distance measurers can be difficult to see in bright
sunshine. For accuracy avoid the temptation to use long sights—keep survey legs to a
maximum of 30 m.
Data collection
The notes and sketches that a surveyor makes should be of such a standard that someone
can draw up the map with no prior knowledge of the cave. To this end, note your data
systematically and consistently. A reliable method is to use a small pad with removable
sheets of waterproof paper printed with boxes to format the data on one side and a grid to
make sketching the passage shape easier on the other.
The minimum data you must collect in the cave is station number, distance, bearing and
inclination. To these, add estimates of left, right, up and down (LRUD) distances to the
walls, roof and floor. There is no recognised convention for these. However it is most
reasonable to take LRUD data while facing in the direction the survey is travelling.
Remember, they are estimates that reflect the general passage form and should be the
average distance to the walls, roof and floor from the station.
Another convention you must
decide on is the exact direction of
left and right. The option that
involves minimal notes and gives
a good representation is to take
the left and right data in the
direction that bisects the angle
between the two sights. Up and
down are best left as true
verticals.
LRUD data are essential for good
computer graphics and give scale
to the sketches, making drawing
up of the final map easier than
relying on sketches for
information that is difficult to
show. eg. If the surveyor is
sketching a plan as he goes, the
up and down data automatically
give a passage height.
Left and right data convention
direction of travel
L
R
L
R
L
R
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Survey data sheets
Table 10:1 Cave map symbols
marked survey station mud
change of survey grade flowstone
cross-section plane stalagmite
unsurveyed passage stalactite
abrupt change in floor flowing water
sloping floor standing water
boulders or blocks sump
rockfall airflow
crystals doline
gravel shaft
sand change in rock type
pitch (with height) climb (with height)
After Anderson, 1978. For official international symbols, see: www.carto.net/neumann/caving/cave-symbols/
Topofil Suunto Sketch
sketch
topofil
a al
old new
old new
marble
slate
10p 5c
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Draw sketches of the cave passage as a series of small plans or occasionally sections, with
all stations and pitches marked to simplify the drawing up. As a check, keep the plans to
scale and orientation so that you will notice a wrong figure from the instrument reader in
the first instance. Draw cross-sections, perhaps at a larger scale, to show passage shape or
help explain a complex piece of passage. Note a provisional tackle list along with the sketch.
Take down sketches and data with a soft mechanical or self-sharpening pencil. Carry the
pad, pencil, spare pencil, marking pen and flagging tape in a pouch that hangs around your
neck.
If you make a mistake during note taking, cross it out neatly and rewrite it. Never obliterate
an original, as it may useful in sorting out a more serious problem later. Sketches on the
other hand may become an unreadable mess if you do not erase errors.
At the end of each days surveying remove the used data pages from the pad so as not to risk
losing them in the cave on a later survey trip and transcribe the numerical data into a master
data book or computer so as to give a duplicate copy.
Be sure to include information such as members of the survey party, full name of the cave,
date and instruments used on the first page of any series of data or attached as a separate
title page.
Plot a traverse line as soon as possible and have the person who took the original notes draw
on the wall detail. Mark pitches, climbs and squeezes and write up an accompanying tackle
description or note the information beside each pitch. The original note taker should do as
much as possible so that the final drawing up will be as easy and accurate as possible.
Standard symbols
Only the neatest of note takers can use the full range of symbols in their original cave
sketches and have them correctly interpreted later. Use a few written words and an arrow
to indicate where and save the pretty symbols for the final drawing. Large caves are often
presented at scales of 1:1000 or more so it is impossible to note much more than the passage
outline, water, airflows and the occasional large block.
Survey accuracy
Precision is the reproducibility of data and is reflected by the fineness to which the
instruments can be read; theoretically half of the smallest unit marked on the scale.
Topofils should be readable to half a degree in compass and clinometer and half a
centimetre in distance. With Suuntos and tape this is a quarter of a degree for the compass
and half a degree for the clinometer and usually half a centimetre for the distance. In any
survey, the station error (distance the instrument actually is from the station) and
movement in the hand-held instrument is so great that anyone who reads to that precision
is fooling themselves. It is only reasonable to read to the nearest degree and nearest 5 cm
when you are surveying carefully.
Accuracy is the distance a surveyed point lies from the ‘truth’. It is largely affected by the
skill of the surveyors and the precision of the instruments.
Any survey point lies within an area of uncertainty, the size of which you can estimate. The
simplest means of checking the accuracy of a survey is to map a closed loop and calculate
the difference between the two end points that are supposed to be the same. This
difference is the ‘misclose’ and is rarely zero. A loop that closes within acceptable limits is
probably alright, one that is outside the limit suffers from one or more gross errors.
Estimating survey accuracy
You can estimate the theoretical accuracy of a survey using Random error curves for Suunto
and topofil surveys on page 181. These give an expression of the possible accuracy that the
instrument and survey can produce given certain parameters but cannot take into account
gross errors such as how well the instruments were really read, excessive station error, data
collecting errors, magnetic errors or systematic errors.
Use the curves to estimate the expected accuracy of an open survey as well as to check if
the misclose in a loop is within acceptable limits.
You can expect a perfectly executed survey to lie within the theoretical range and in
practice this is usually the case for the vertical while the plan is usually within twice this
value. Surveys lying up to twice the theoretical value for the elevation and three times for
the plan are still regarded as acceptable even though they are obviously affected by some
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gross error(s). This difference between the magnitude of the acceptable error in plan and
elevation is due to the comparative difficulty in getting accurate readings from a compass
as compared to a clinometer.
You can eliminate most of the potential gross errors in a survey by taking back-bearings on
each leg with a separate compass and clinometer as a check on misread instruments.
Altimeter
In most vertical caves it is not possible to survey a loop that takes in the extremities of the
cave, though minor loops will at least indicate if the surveying is generally up to standard.
Use an altimeter as a control to take a series of readings at known stations on the way down
and back up the cave and if possible leave a second altimeter on the surface to record
pressure variations caused by weather changes. A good altimeter ‘survey’ should give
readings that are within ±25 m of a good survey.
There are several variables to take into account when you do an altimeter survey. The
pressure difference either side of a strongly blowing squeeze can give altimeter errors up to
100 m. Fortunately, this is a local phenomenon and reading quickly return to normal as you
move away from the disturbance. One thing to specially take note of is the temperature
adjustment that any altimeter requires—even a temperature compensated altimeter. An
altimeter can only read the weight of air pushing on it. It ‘knows’ the altitude it is at based
on a standard column of air that has a standard temperature gradient. As you climb a
mountain the temperature often drops tens of degrees. As you climb up cave, it’s
temperature may drop two or three degrees.
If the sum of the temperature offsets from the normal temperatures (from Table 10:2) at
two different altitudes is 1 ˚C, the altitude difference calculated by your altimeter is 0.2%
off the real altitude difference (Suunto, 2003).
To temperature compensate altimeter depth readings:
• Calculate offset between the normal and measured temperature for each point
• Add the two differences
• Altitude error = sum of offsets x measured altitude difference x 0.002.
For example, the figures below are from a recent trip with a surface control:
entrance alt= 2232, temp = 20: offset = 19.5
camp 2a alt = 1377, temp = 13: offset = 6.9
so, 26.4 x 855 x 0.002 = 45
855 + 45 = 900 m (surveyed depth is 901 m)
While I can’t advocate mapping a cave with an altimeter alone, if you encounter a
discrepancy between the altimeter and traditional mapping, you can narrow down the
location of the problem and check the survey.
Table 10:2 Standard temperatures
Altitude
(m)
Temperature
(˚C)
0 15.0
200 13.7
400 12.4
600 11.1
800 9.8
1000 8.5
1200 7.2
1400 5.9
1600 4.6
1800 3.3
2000 2.0
2400 -0.6
2800 -3.2
3000 -4.5
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Random error curves for Suunto and topofil surveys
Systematic errors
Systematic errors are those inherent in the design or calibration of the instruments as well
as the way you read them. Systematic errors are not random but accumulate, making the
accuracy of the survey worse with increased length.
A wrongly calibrated tape for instance, adds to or subtracts from each measured distance,
making the cave bigger or smaller than it really is. A poorly calibrated compass will give a
constant error that has the effect of turning the north arrow on the finished map through
the number of degrees it is out of calibration. Similarly a maladjusted clinometer will affect
the overall angle of the map, reducing or increasing its depth and possibly ‘causing’ streams
to flow uphill. If you survey the entire cave with the same instruments it only requires a
minor adjustment in the final drawing up, but when several instruments are involved, all
with different calibrations, it can result in considerable confusion. Surveying a test loop will
not easily detect these systematic errors. Comparison with a standard is the best way.
Systematically misreading instruments can also accumulate errors. A surveyor sighting with
a Suunto to the light of an assistant of the same height adds 15 cm to the vertical difference
between the two stations and this accumulates for the length of the survey. A 200 m leg
survey would be 30 m out from this error alone!
Check your instruments before a surveying project and periodically during it to ensure that
they really do point north, horizontal and measure distance correctly. Test compasses
against each other. Check clinometers quickly by putting them on a flat surface, taking a
reading, turning them through 180° and taking a reciprocal reading. Test surveyors and
instruments by surveying a known non-horizontal test triangle in both directions.
Note any errors in the instruments and correct them if possible. Otherwise, clearly mark the
original notes and allow for the deviation by adding or subtracting it as a zero error when
you calculate the data.
0 1 2 4 5 6 7 8 9 10
3
1
2
4
5
6
7
8
9
3
traverse length (m x 100)
misclose
(m)
5 m*
10 m*
15 m*
20 m*
30 m*
5 m#
10 m#
average leg length
* Good survey:
station error ± 5 cm, distance error ± 5 cm,
compass/clinometer error ± 1˚.
# Rough survey:
station error ± 20cm, distance error ± 20cm,
compass/clinometer error ± 2˚.
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Minimising errors
Random errors tend to compensate for each other as the number of survey stations
increases. Compensating errors may allow a rough survey to give a good closure even though
each individual point on the map is well displaced from where it should be. This is not to say
that you should ignore random errors. There are several procedures you can follow in order
to minimise both random and systematic errors.
Leg length
Long leg length magnifies compass
and clinometer errors and gives less
accurate final displacement than a
series of short sights. If you’re using a
topofil or rangefinder, avoid the
temptation to take sights longer than
30 m. The optimum leg length is a
compromise between station error
and instrument reading precision (see
Random error curves for Suunto and
topofil surveys on page 181). Roughly
located stations favour long survey
legs while low compass precision
favours short survey legs. On pitches
where the difficulty of getting any sight may outweigh the need for accuracy, try to keep
the pitch length as a true vertical.
High angle readings
Compasses become increasingly difficult
to read accurately as the angle of the
sight leaves the horizontal. On high angle
legs, improve accuracy by taking a
vertical then a low angle sight rather
than one high angle sight. On up sights
droop the tape between the stations
after you take the length and sight the
compass to the tape. Most topofils do this
automatically. Another possibility is to
dangle the clinometer from its string as a
plumbob at arm’s length to line up the
survey station with a spot on the wall at
the same level as the surveyor. Sight the
compass to the spot or the plumb line.
High angle compass error is mitigated by
the fact that as the angle of the sight
becomes steeper the possible
displacement error from a rough compass
reading decreases (a similar effect
applies to low angle clinometer
readings).
Comparative error in short and long survey legs
15 m leg
5 m leg
5˚
5˚
error = 0.44 m
error = 1.31 m
Reducing error on a steep sight
easy
easy
d
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&
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c
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compass
15. Surveying 183
Contents Index
Station error
Avoid ‘floating’ stations such as sighting
to the light of someone standing in
mid-passage. The person holding the
other end of the survey can never
faithfully relocate them. When sighting
it is often better to hold the instrument
in line between the two stations rather
than as close to the station as possible.
This is especially relevant to Suuntos
where the thickness of the surveyor’s
head can create a considerable station
error. Topofils are more naturally held
in line and their small size keeps the
station error small when this is not
possible.
The significance of the station error is
especially great for short survey legs
and diminishes with increasing leg
length.
Transcribing errors
Transcribing errors are common in cave surveying and once a reading is taken wrongly, it is
difficult to identify as wrong and in need of checking. At least one survey program (Compass)
attempts to find transcribing errors using statistical analysis of closed loops. Do not
remember readings, note them down as the instrument reader calls them out. A roughly
oriented sketch will help you pick up badly wrong compass readings. Have the note taker
call back all readings including the sign of clinometer angle for confirmation. Short leg
length aids communication. Do not mentally reverse readings while in the cave. Note the
reading as given and indicate beside it whether it is a back or fore sight if it is different from
the others. Direct entry into a PDA using Auriga reduces the problem. TopoScan will solve it.
Magnetic errors
Keep anything electrical or magnetic well away from compasses. Be especially careful of
holding a hand torch and anything with a magnetic switch too close when lighting the
compass dial. The bigger the piece of steel the worse the problem.
Rope lengths
Do not measure pitch length by using a ‘known’ rope length. The rope will almost certainly
have shrunk since it was last measured and knots, rebelays, deviations and non-vertical
hangs upset the calculation further. At worst, measure the rope length after derigging
provided it was rigged as a freehang.
Reducing station error - Suunto
Good
station
station
error
Poor
Good
station
Reducing station error - topofil
station
error
Poor
16. 184 VERTICAL
Contents Index
Training
Be sure all surveyors and assistants know what they are doing, have practised using the
instruments and understand the surveying style required.
Computing
Even in the most remote location it is possible to process raw survey data and have it back
as an on-screen plot within a few hours of exiting the cave.
It is easiest to calculate data on a purpose designed program such as Compass, Survex or
Walls. Most cave survey reduction software can be downloaded for free. Most have been
written to solve a specific cave surveying problem, then improved. Download a few, try
them out and see that one suits your needs. Whatever software you use, proof read the data
you enter as soon as possible in order to pick up any errors in both the data itself and its
organisation.
If you’re forced to a more basic level by the lack of a computer, calculate X, Y, Z, D data
on any calculator that has trigonometric functions by using four simple formulae:
p = d cos c p=plan distance
∆X = p sin b c=compass
∆Y = p cos b d=distance
∆Z = d sin c b=bearing
D = sum of p ∆X=change in X
∆Y= change in Y
∆Z = change in Z
Table 10:3 Nada Cave coordinates
Carefully list the results, then make a cumulative list made of these relative coordinates (ie.
relative to the previous point) to give coordinates relative to the starting point.
Hand plot the X Y Z D data you’ve calculated in the field as a plan and projected or
developed section at a suitable scale (usually 1:1000) so that it can be used in further
exploration of the cave. Once you get the data home you can reprocess it using a more
sophisticated program on a bigger computer to get special features such as loop closures and
3-D graphics.
Station X Y Z D
N2701 0.0 0.0 0.0 0.0
2 5.0 1.8 -2.0 5.3
3 5.0 1.8 -11.8 5.3
4 8.1 -3.5 -10.2 11.5
5 9.8 -0.4 -13.3 15.1
6 11.3 -0.2 -13.0 16.6
7 12.6 -2.6 -16.6 19.4
8 16.9 -2.6 -15.0 23.7
9 16.9 -2.6 -27.0 23.7
10 19.5 5.1 -26.0 31.9
Traverse length = 57.5 m
17. Surveying 185
Contents Index
Plotting the survey
Before drawing up settle on a scale that either matches that of other caves in the area or
allows the cave to fill the page you are drawing it on. How much hand drawing you have to
do depends on the software that you choose. Chances are, you’ll have a line plot perhaps
with left and right (or up and down points), marked to match your sketch too.
For hand plotting, choose a zero point that allows the cave to fit on the page and draw scales
along the margins. Graph paper is better than trying to scale off distances with a ruler.
Traverse line
Plot the X (east) ordinate across the page against the Y (north) ordinate up the page.
Label each point with its station number and join the dots to produce the traverse.
Unless the cave is relatively straight it is easiest to plot a few stations at a time, join the
dots, then plot a few more so as not to become lost in a page of dots.
Mark left and right
Lightly mark left and right estimates from each station.
0 5 10 15 20
0
5
1
2/3
4
5
6
7
8/9
10
R
18. 186 VERTICAL
Contents Index
Sketch
Copy the sketch taken in the cave so that it fits the traverse, then fill in the details.
Draw sections (elevations, profiles) in the same manner as the plan but use different
coordinates, depending on the nature of the cave and the effect you desire.
Projected sections compress any part of the cave that does not run parallel to the projection
plane and make a vertical cave appear much steeper and shorter than it really is.
Plot X ordinates across the page
against Z down the page and add
the walls with the aid of LRUD data
and the plan.
Y
X
Projected Section, East-West plane
Z
X
19. Surveying 187
Contents Index
Plot Y ordinates across the page
against Z down the page.
Plot D across the page against Z down the page to give a right trending plot, that may indeed
be what the cave does. Often however caves zig-zag beneath themselves and by referring
to the plan you may wish to fold the developed section back on itself when the cave makes
a major change in direction. Once you plot the traverse, draw the floor and roof on as
before.
Projected Section, North-South plane
Z
Y
Z
D
Projected Section, East-West plane
20. 188 VERTICAL
Contents Index
‘3D’ view
Provided you supply LRUD data along with the
traverse data, some survey reduction
programs can plot a 3D representation of your
cave in seconds for on-screen viewing using
VRML. Unfortunately, this usually doesn’t
translate very well to printed images. Such
images usually work better for big, complex
systems by making the relationships between
the various passages more evident. Small
caves tend to look blocky and stylized, while
long, straight caves show most of the cave
‘too far away’ to be especially useful.
On a small scale (10 stations), Nada Cave on
the following page looks too stylised but you
could use it to provide the basis for a hand
drawn map. However on a larger scale—the 3D
of Dead Dog Cave has 700 stations —with
hidden lines removed, the plot gives a better
idea of what the cave is like than a
conventional map. By plotting the same data
twice, at viewing angles a few degrees apart,
you can generate stereo pairs of the cave.
VRML representation of Nada Cave
Ozto Ocotal/J2, Mexico. Photo: Enrique Ogando