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2007 NSS Convention Guidebook To the right of the entrance junction is a room. This room has large flowstone along the left wall. A muddy upper level continues off the room for 100 feet before becoming totally mud. filled with The drain off this room leads to a lower room and a yearround stream. The Terry Clark in Baker Hollow Cave. Photo by Dave Black. stream leaves the cave by way of a narrow, chert-lined crack that is too tight to follow. The up stream leads, in 500 feet at a flowstone mass. There are two in a short distance, to a small dome. At the top small in-feeding passages in this section of the of this 15-foot-high dome the stream passage cave that bring in water from the stream bed. continues for over 200 feet upstream as a 332
meandering, narrow canyon. This passage was not mapped. Reference: OVR <strong>Karst</strong> Encounters Guidebook: 1990,1991 D.Black CIG Cave Capers Guidebook: 1984, 1990 This cave is on public property. The old cave is a normal horizontal cave. The new cave is very tight and has three pits requiring vertical gear and 100-foot, 80-foot, and 60-foot ropes. The dig section has loose rocks and is subject to cave-ins. BBUB, short for “Bats Brought Us Back,” was discovered in 1982 as a result of digging in a breakdown-choked sinkhole that was blowing a plume of steam in the cold winter weather. After six digging trips the sink had been cleared to a depth of 6 feet with no cave in sight. At the point of calling off further digging, a bat emerged from the breakdown—the dig was on and the cave had found a name! The entrance is an enlarged crawlway for about 10 feet followed by a 7-foot drop into the cave passage. The cave is developed along bedding planes with minimal joint control. The passage is primarily crawlway, averaging 4 to 8 feet wide BBUB Harrison County Caves MVOR Guidebook, 1987 ISS Newsletter 1#1, 8/77 BIG Guide to the Caverns of Harrison- Crawford., 1963, R.Powell OVR <strong>Karst</strong> Encounters Guidebook, 1989 By Noel Sloan and 2 to 3 feet high. It appears to be developed in the Paoli and upper Ste. Genevieve limestones. Numerous chert nodules are evident in the upper levels. The cave has developed along two levels, a dry upper level with a sandy breakdown floor and an active, intermittently-wet lower level with either a cobblestone or clay floor. An active stream can be seen at several points in the lower level. The lowest point in the cave is at the bottom of a dome-pit about 50 feet inside the cave. Past this dome, the cave continues as a friendly crawl at about 30 feet below the entrance for some 450 feet until one encounters a small 4-foot climb-down. At this junction, one can continue in five directions either upper level upstream or downstream or lower level upstream or one of two downstream passages. A register has been placed at this junction. The upper level upstream cave continues as a 333
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Back Underground in Indiana A Guide
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Contents Welcome from the NSS Presi
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Welcome from the NSS President Welc
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Welcome from the Governor of Indian
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Color Photography Section We are mu
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Section I: The Harrison Crawford Ar
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The Convention Planning staff is pl
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The Harrison County Visitors’ Cen
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per day, which includes the right t
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A Short History of Early Crawford C
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Section II: Exploration 1
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Deep below the hills of Crawford Co
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Gypsum flowers and crusts. Beyond S
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top of Fools Dome began to take onl
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The Discovery and Exploration of th
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previous surface survey of the gulf
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The Survey Begins On Saturday, Janu
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through January as well as every we
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and another team went into the seco
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were surprised to learn that a tigh
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Other Exploration in the Lost River
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flood tube really played on our min
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efore splitting and ending in break
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Two Bit Pit Harrison County, Indian
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Two Bit Pit c l i m b - d o w n i s
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Two Bit Pit 4
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downstream passage is generally 6 t
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Trip #16 August 12, 1990 Greg McNam
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ing into established survey at the
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An Exploratory Trip to Gory Hole: J
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the right side. It was necessary to
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The Exploration of Harrison Spring
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guide line was no longer in the ent
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first that day and had already gone
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along his dive buddy, Ralph, for hi
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visibility out was normal, about 3
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Section III: Geology and Cave Scien
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Regional and Karst Geology of the O
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plains, swallowholes, storm water r
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Regional Physiography and Stratigra
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closely this apparent relationship
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Regional Physiography and Stratigra
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Figure 6. Geologic map of south-cen
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margin of the Mitchell Plain, chara
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cavern development. Somewhat more t
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Geomorphic History of the Mitchell
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idge summits in the Crawford Upland
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to produce such continuous surfaces
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Stratigraphy and Lithology of the O
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upward sequence. [This model shows
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County (Gray, Jenkins, and Weidman,
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He then casually and without explan
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outcrop is an overlooked and deserv
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Geology Field Trip Figure 13. Stop
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This five-stage model may have impl
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Figure 16. The Tower Quarry highwal
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River. Note that the valley is fill
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Smith and Tim Grisson of Ohio Caver
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of the Mitchell Plain were dissolve
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Geology Field Trip Figure 21. Trave
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Geology Field Trip Figure 22. Harri
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The Battle of Corydon, Indiana’s
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of rocks above the Ste. Genevieve i
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New Albany Shale Gas Wells: A natur
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Geology Field Trip Figure 29. Inter
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Preglacial Regional Drainage and Gl
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Stop 5: The Falls of the Ohio vicin
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Figure 35. Historic map of the Fall
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After experiencing a boat trip down
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Geology Field Trip Figure 36. Geolo
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that time. Locally, they are rarely
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Geology Field Trip Figure 38. U.S.
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depth of 12 feet. This became known
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Lost River Field Trip Figure 40. Ma
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Lost River Field Trip Figure 42 Phy
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Lost River Field Trip Figure 44. Co
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to Lick Creek to the southeast as p
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Lost River Field Trip Figure 46. To
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Figure 48A though D. Clyde Malott
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State Road 37 Corridor to Wesley Ch
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then proceed down hill to the north
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and is located 0.5 miles north. The
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Figure 54. A view of the rise pool
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Lost River Field Trip Figure 56. Ge
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Travel from Wesley Chapel Gulf to O
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miles (Bassett, 1976 and 2000) to t
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Crawford Upland morphology, and the
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historians and eyewitness accounts.
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Ash, Donald W., 1985: Geomorphology
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pany the geological map of the stat
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Mammoth Cave Region, Kentucky, and
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Little brown bat. The endangered In
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under flat stones or sticks. Its we
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Lewis, Julian J.; R. Burns; and S.L
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cave passages ranging in altitude f
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The Geology of Wyandotte Cave Monum
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The Geology of Wyandotte Cave Hall
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Cave fine-grained sediments were pr
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Projected Passage Profiles for the
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The History and Status of Karst Ver
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Karst Vertebrate Paleobiology in In
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Karst Vertebrate Paleobiology in In
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Leidy’s peccary (Platygonus vetus
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Figure 8. Skull of the dire wolf, C
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Figure 11. The Bat Room of Megenity
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Mammalian Faunas during the Last De
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cene Paleoecology and Archaeology o
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Harrison was by far the largest spr
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drainage is north to Blue River. Th
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It may also be noted that Harrison
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Section IV: Indiana’s Cave Organi
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The Indiana Karst Conservancy, Inc.
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esource in cave and karst conservat
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Indiana Karst Conservancy daylight
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Indiana Karst Conservancy Heading f
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property. Meanwhile, Randy Jackson
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Number of Caves 1,000 Feet or Longe
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27. Warren 74 28. Miami 63 29. Foun
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Section V: History 235
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Lewis D. Lamon: Indiana’s Grand O
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will find a way in. Lewie’s softs
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George Jackson getting a drink at C
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Falls at the age of six, it was par
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weekends. Sometimes I would bring a
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Caves, Cave Rescue, and the Nationa
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lost or overdues or minor injuries:
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modular NCRC trainings have occurre
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A History of Indiana Caving We do k
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22 miles long. The addition of the
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Pace, Fort, Reeves, Sollman, Powell
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He formed a short-lived partnership
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manufactured history of Wyandotte C
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Section VI: Conservation 263
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The Richard Blenz Nature Conservanc
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The Richard Blenz Nature Conservanc
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pipe. Several dig trips subsequentl
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Lasiurus cinereus (horary bat), fem
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Myotis septentrionalis (northern my
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Cavers have already contributed lar
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ugs. • Pick up litter (use good j
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Section VII: Miscellaneous 27
Page 285 and 286: Bluespring Caverns “Myst’ry Riv
Page 287 and 288: Marengo Cave, located on the edge o
Page 289 and 290: of the cave, the scout program was
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Page 293 and 294: Indiana Show Caves hire Richard L.
Page 295 and 296: Section VIII: Cave Descriptions 2 1
Page 297 and 298: Cave Maps and Descriptions The foll
Page 299 and 300: een made but a voice connection sho
Page 301 and 302: intersection. The left-hand passage
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Page 305 and 306: This pit is located on a heavily wo
Page 307 and 308: Main Passage in Erics River Cave. P
Page 309 and 310: drive road. There is a pull off on
Page 311 and 312: in 50 feet. This cave has pits and
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Page 315 and 316: Not to be confused with Harrison Co
Page 317 and 318: The Old Town Spring Entrance to Mar
Page 319 and 320: placed about 150 feet inside the en
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Page 323 and 324: Robinson Ladder Cave is an Indiana
Page 325 and 326: dates. Also, except for the entranc
Page 327 and 328: Saltpeter Cave Crawford County Cave
Page 329 and 330: This cave is located along the base
Page 331 and 332: of Texas Creek and is about half a
Page 333 and 334: water is from B-B Hole, a nearby ri
Page 335: Harrison County Caves 1915 Cave was
Page 339 and 340: was rigged in 1979 by Tom Fritsch a
Page 341 and 342: Jamie Winner at Big Mouth Spring Ca
Page 343 and 344: drop. At the bottom of this drop is
Page 345 and 346: Dave Stahl at the top of the first
Page 347 and 348: Nick Smith has arranged access to t
Page 349 and 350: he returned to remove this ledge, s
Page 351 and 352: on the left side of the main passag
Page 353 and 354: degree angle. At the bottom of the
Page 355 and 356: Ryan Moran climbing Gary Pit. Photo
Page 357 and 358: This cave is presently the main cav
Page 359 and 360: You can get to the pit in two diffe
Page 361 and 362: Willie Hunt at the entrance to Jays
Page 363 and 364: T he entrance to King Leo Cave is a
Page 365 and 366: The 40-foot-tall canyon. Photo by E
Page 367 and 368: way, flowstone and some gypsum flak
Page 369 and 370: Manhole Cave, Corydon West 7.5-minu
Page 371 and 372: CIG Cave Capers Guidebook: 1984, 19
Page 373 and 374: the 56-foot drop known as The Cathe
Page 375 and 376: Sharon McConnell in Rocky Hollow Ho
Page 377 and 378: Seitz Pit, also known as Fuzzys Pit
Page 379 and 380: Harrison County Caves 375
Page 381 and 382: with the sandy crawlways and contai
Page 383 and 384: it opens into Tourist Avenue. The l
Page 385 and 386: and connects back to the main strea
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to a small room with moss-covered f
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The Donaldson Cave entrance in 1938
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Dave Stahl in the lower level of Bu
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Dave Everton beginning the rappel i
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the owner, is quite friendly to res
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Roberts Cave was opened in 2001 by
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Mike Kennedy at the South Y in Sull
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Lawrence County Caves Sullivan Cave
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with breakdown. One passage to the
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Wayne Cave is the property of the I
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The natural bridge at Camp Two. Pho
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Dillon Cave is located in the Hoosi
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Lost River Cave should be considere
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Janie Atz preparing to cross the li
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Tom Duselis looking at cannonballs
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Owen County Caves 413
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Washington County Caves Cave River
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and continues as such to the Flowst
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een known as the Wet Clifty Cave an
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water depth, this passage eventuall
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After entering the gate at Henderso
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head of a dry ravine. The first 300
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at the Trinkle Cavern Entrance. Alt
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Section IX: Color Photography 42
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Bill Baus in the Formation Room in
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A cannonball in the Boone-Cannonbal
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John Harris in Binkleys Cave’s He
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Aaron Atz in CHUG Hall in Teds Dig.
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Cavers in the Wayne Cave crawlway.
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Willie Hunt in Jewel Box Cave. Phot
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Nate Newkirk in Lower Wild Turkey C
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Nate Newkirk in Redmond Cave. Photo
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A Abram, Jerry 400 Abram, Marie 400
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Cooper, James Fenimore 260 Cope, E.
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Elliot Stahl with the warning sign
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Hodges, Frank 393 Holiday World The
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McGowan, Dave 256 McGrain, Preston
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P.B.R. Plunge 369 Packard’s groun
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Spaulding, Greg 254, 255, 365 spide
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Dave Stahl ascending Fuzzy Hole. Ph
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