the cave. The spring was running strongly and some travertinepools that have been dry <strong>for</strong> five years are now full.+++Persons: Ed Alexander, Bob Burnett, John Fish, John Kreidler,Charlie Jennings, Tommy McGarrigle, Bill RussellDate: 31 May-IO June 1966Destination: Huautla de Jimenez, OaxacaReported by: John Fish Austin, TexasEd, Bob Charlie, and I left in my car late on Tuesdayafternoon, bound <strong>for</strong> the fabled Huautla plateau in northeasternOaxaca. Bill Russell, John Kreidler, and Tommy McGarrigle gota late start and joined us in Huautla. Despite the many traumasof our drive to Huautla (hole in the gas tank the size of anickel-repaired with a Tootsie Roll, fog along the mountain roads),we arrived there at last only to have to wait a day in Huautlawhile I recovered from a severe intestinal infection. BillRussell and group caught up with us and after puttin~ FelixSeiser,(visiting from Austria and had corne with Bill) on the busback to the U.S., we drove on to the cave area which starts aboutthree miles east of Huautla. On June fourth we got our firstlook at the cave country we were seeking.We had planned to drive to the end of the road and camp,but after passing several large sinkholes, everyone abandonedtheir cars and started checking the sinks near the road. Uponquestioning the local people, Bill was directed to the bottomof a large closed valley in which a small stream dropped intoa pit about 250 feet deep, later named S6tano de San A~ustin.The small town of San Agustin (hence the name of the sotano)lay 500 feet above the s6tano in a divide between two hugedolinas. The San Agustin dolina is approximately one mile longand up to a quarter of a mile wide. It consists of a largecentral dolina with several smaller dolinas or sinks at eachend below the towns of San Andres and San Agustin. The RioIglesia dolina appears to be larger, perhaps the same lengthbut considerably wider and deeper. In both dolinas water runsoff volcanic hills or ridges and sinks into the limestone dolinabottoms.Looking down from San Agustin we could see where the RioIglesia dropped into a fissure below a large opening in themountain. That afternoon Bob, Ed, and Charlie explored theentrance drop of s6tano del RIo Iglesia and found that the mainwater passage, which took several hundred gallons per minute,was impassable. An overflow passage was easily accessible,though, and led to a drop. Since it was virtually dark wedecided not to push the cave then.Meanwhile Tommy and Bill both spotted a large entrancenear San Agust!n on the hill ~bove. This was subsequently calledCueva de San Agustin and goes down a series of slopes and dropsto a deep pool of water. The cave appears to continue.57
After a perusal of our topo maps the next morning, wedecided to look over the area in general. (A section of thetopo map used is found on page 60.) In particular we wantedto go to Rancheria de Cameron, located along the southernflanks of the plateau, where a closed valley is shown. As therest of us began our hike, Bill, Tommy, and John Kreidler headedalong the NE trending closed valley to Tenango, several kilometersaway. We found immediately that our topographic mapswere incorrect in many details, especially relating to cUlture,so we made corrections as we went along. Many of the Indianswhich live in the isolated mountains speak only Mazatec, andat times communication was frequently a problem. We foundCameron that afternoon and discovered that the large valleybecame narrow and deep in a direction away from the plateau.It passed down a series of drops then between three hundredfoot high sheer limestone walls and finally emptied into abroad valley below. Greatly disappointed, we began the longeight kilometer hike back to camp. Except <strong>for</strong> the few cavesfound in the large San Miguel dolina (see cave descriptions),we found no pits or caves on the southern flanks of the plateau(this day) other than a few shallow, filled sinks. On the otherhand Bill Russell and crew found several small sotanos, most ofwhich were left unchecked, and a large cave with a stream enteringit. The cave, Cueva de Agua Carlata, was explored as faras the twilight penetrated, about 200 feet below the entrance.A large passage containing a good-sized stream led downwardinto darkness o They returned to camp having only partiallyobserved the large valley containing the village of Tenango.The morning of June sixth we decided to check out thesotano just below our camp, Sotano de San Agustin (see description).Although it was only a few hundred yards away,it took two to three hours to tie the rope off, and <strong>for</strong> Bob,Charlie, Ed, and Tommy to hack their way down the vegetationcovered entrance drop. The entrance is a pit as large as thatof Sotano de Huitzmolotitla, but not quite as deep. From thebottom a high fissure slopes steeply downward into a btg room,where another stream emerging from breakdown joins tha fromthe waterfall at the entrance, making it comparable to thestream of Rio Iglesia. Ed and Bob continued onward and foundthat after a series of short, closely-spaced drops, they hadused all of their rope and not yet reached the bottom. Fromthe top of the next drop water could be heard falling andsplashing far below.Since there already were enough people in Sotano de SanAgustin, Bill, John, and I decided to check out what from adistance looked like a very promising pit. Much to our surprise,it turned out to be a cave later named Millipede <strong>Cave</strong> (see description).From this cave we got our only good collection ofthe whole trip, then returned to the car.On June seventh, our last day at Huautla, we devoted theday to a reconnaissance of the nearby areas of the plateau.As it was about a ten kilometer hike one way, and we were attimes uncertain of the trails, we hiked only to the edge ofthe plateau. Among the features we saw were haystack hills,58
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de T1amaya the deepest surveyed cav
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and is about 200 feet long. It is p
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107NEWSNOTESTABLE OF CONTENTSTRIP R
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109CAVEMAPSDuring the past six year
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111CAVES OF GUERRERO AND MORELOSJOH
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113in the volcanic detrital deposit
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115CAVE DESCRIPTIONSGRUTA DE ACUITL
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117CUEVA DE CARLOS PACHECOcavecavec
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119CUEVA DEL DIABLOLocation:Descrip
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121References:levels. The entrance
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123decorated passage which extends
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125collections by Stanley Kiem (Loo
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1279.10.11.12.13.14.caves or cave-l
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131TABLE OF CONTENTSNEWS NOTES. ...
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NENCINO - JULILO ROADSSOTANO DE SAN
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FEETo100SOTANO DE LA JOYAJOYA DE SA
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137had not been checked was followe
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139a high mountain karst area with
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-SaltilloMonter..SKETCHMAPofCA~ON D
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143another 15 miles before we turne
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ENTRANCE Q~\\F~\~.~ ..~~-.~~~O~v'\.
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147S6tano de las Ra!ces lon the sam
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149and color motion pictures. The f
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151ground in the area. (See photogr
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ENTI'ANCEGRUTADENAVIDADMUNICIPIO DE
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155NOTES ON THE EXPLORATION OF SOTA
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157obtain a rough idea of how many
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159Grutas de Mogote, located one mi
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161Past the first large room (appro
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163-749 feet. The left-hand passage
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165it looked a good 300 feet deep.
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167was. Almost 2 hours were require
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Haarr, Allan P. 50 Clover Dr Delmon
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171Young, sam and Diane 474 lOth Av
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173RECENT ADDITIONS TO THE KNOWLEDG
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175large horizontal passage about 1
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177S6tano de Huitzmolotitla, with a
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AreaNorth ofMonterreySouth ofMonter
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182BIOLOGYSECTIONMEXICAN CAVE BEETL
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184from Canada to Oaxaca, but only
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INDEXVOLUME1966II
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187Cantabroniscus primitivus isopod
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189Hooton, Diana 6:149-154Hosley, B
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191pictographs 5:121Pinal de Amo1es
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193from La Si11eta looking eas~)f.