Lost River - Karst Information Portal

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2007 NSS Convention Guidebook 166 Figure 57. Tour map and topographic map showing the western edge of the Lost River basin and embayment transition from the sinkhole plain to the Crawford Upland, as well as the Orangeville Rise and the True Rise.
Travel from Wesley Chapel Gulf to Orangeville Rise Leave the Gulf driveway. Turn right (north) onto County Road 200W. Go north to Wesley Chapel. Turn left (west) onto Orangeville Road. Proceed west passing over a bridge over the dry bed of Lost River (Figure 57). At the bridge, downstream is to the southwest. The dry bed has eroded a long, meandering channel pathway far to the north of this point. Note the bedrock valley wall incised into the Ste. Genevieve on the south side of the road. Proceeding west, the road ascends a small toeslope spur of the Chester Escarpment which is on the north side of the Lost River basin. At this point, the Lost River embayment and basin is rapidly narrowing, and is in a 1-milewide transition zone between the Mitchell Plain and the Crawford Upland. The dry bed swings widely to the south around this upland spur and begins to adopt the morphology of an antecedent bedrock stream incised into an upland (here the Crawford Upland). Come to Intersection of County Roads 500W and 500N. Bear left (south). Drive to Orangeville (Figure 57). Note the Dry Branch channel, which is an upland stream, on the left side of the road. During times of excessive rainfall, surface waters overflowing from swallowholes in the karst valleys to the north rush down this surface channel and enter Lost River just below the Orangeville Rise. The karst valley of Dry Branch drains southward to the rise at Orangeville. Malott (1939, p 1984) described karst valleys as dismembered distal ends of the former surface systems (in which) the minor valleys have been cut through into the underlying limestones and karst features have developed in the valley floors. The change from surface to underground drainage is marked by dry beds and swallow-hole features, which receive and carry storm waters only. Some dismembered side valleys terminate in deep individual courses, producing blind valleys which end bluntly against higher land. More commonly the underground drainage is directed out from under the karst valley, but Lost River Field Trip occasionally the drainage is recovered in the lower section of the same valley, appearing as a rise or karst spring. Later stages of the karst valleys lead to the development of small karst plains hemmed in by clastic ridges or hills. The floors of these karst valleys are at grade with the upland surface of the Mitchell Plain within the Lost River basin to the east. During Pleistocene time, the Lost River became entrenched through the Tertiary-aged terra rosa and other soils into the limestone bedrock beneath the Mitchell Plain surface, and subsequently developed subterranean routes at grade [or slightly below (KS)] with the dry bed of Lost River, while the (karst) valleys in the Crawford Upland lost their surface drainage through subterranean stream piracy (Powell, 1964) The Dry Branch karst valley contains several sections of dry beds that empty into swallowholes. The subterranean drainage rises at the Orangeville Rise. This karst valley is unusual in that it carries water in its downstream part more often than most others in the Crawford Upland. Some karst valleys lack any significant dry bed and are more like a sinkhole plain. The diversion of surface drainage to the underground routes is favored by a lower base level of down cutting by the recipient stream. [Prior to Ruhe’s work (KS)], it was thought that most of the valleys may have been formed by antecedent surface streams during Tertiary time as a base-level counterpart of the Mitchell peneplain of Beede (1911, pp 95–97) prior to deep-stage channel development of subterranean drainage and karst features during Pleistocene time. Stop : Orangeville Rise (National Natural Landmark) The Orangeville Rise is an excellent example of a southern Indiana perennial vertical rise pool and spring. Figure 58 is a photo of the Orangeville Rise and Figure 59 is a sketch map and cross section. The Orangeville Rise is not the True Rise of the main Lost River but rather is the outlet for drainage captured in a Crawford Upland sub-basin of about 49 square 167
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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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Page 121 and 122: Geology Field Trip Figure 21. Trave
Page 123 and 124: Geology Field Trip Figure 22. Harri
Page 125 and 126: The Battle of Corydon, Indiana’s
Page 127 and 128: of rocks above the Ste. Genevieve i
Page 129 and 130: New Albany Shale Gas Wells: A natur
Page 131 and 132: Geology Field Trip Figure 29. Inter
Page 133 and 134: Preglacial Regional Drainage and Gl
Page 135 and 136: Stop 5: The Falls of the Ohio vicin
Page 137 and 138: Figure 35. Historic map of the Fall
Page 139 and 140: After experiencing a boat trip down
Page 141 and 142: Geology Field Trip Figure 36. Geolo
Page 143 and 144: that time. Locally, they are rarely
Page 145 and 146: Geology Field Trip Figure 38. U.S.
Page 147 and 148: depth of 12 feet. This became known
Page 149 and 150: Lost River Field Trip Figure 40. Ma
Page 151 and 152: Lost River Field Trip Figure 42 Phy
Page 153 and 154: Lost River Field Trip Figure 44. Co
Page 155 and 156: to Lick Creek to the southeast as p
Page 157 and 158: Lost River Field Trip Figure 46. To
Page 159 and 160: Figure 48A though D. Clyde Malott
Page 161 and 162: State Road 37 Corridor to Wesley Ch
Page 163 and 164: then proceed down hill to the north
Page 165 and 166: and is located 0.5 miles north. The
Page 167 and 168: Figure 54. A view of the rise pool
Page 169: Lost River Field Trip Figure 56. Ge
Page 173 and 174: miles (Bassett, 1976 and 2000) to t
Page 175 and 176: Crawford Upland morphology, and the
Page 177 and 178: historians and eyewitness accounts.
Page 179 and 180: Ash, Donald W., 1985: Geomorphology
Page 181 and 182: pany the geological map of the stat
Page 183 and 184: Mammoth Cave Region, Kentucky, and
Page 185 and 186: Little brown bat. The endangered In
Page 187 and 188: under flat stones or sticks. Its we
Page 189 and 190: Lewis, Julian J.; R. Burns; and S.L
Page 191 and 192: cave passages ranging in altitude f
Page 193 and 194: The Geology of Wyandotte Cave Monum
Page 195 and 196: The Geology of Wyandotte Cave Hall
Page 197 and 198: Cave fine-grained sediments were pr
Page 199 and 200: Projected Passage Profiles for the
Page 201 and 202: The History and Status of Karst Ver
Page 203 and 204: Karst Vertebrate Paleobiology in In
Page 205 and 206: Karst Vertebrate Paleobiology in In
Page 207 and 208: Leidy’s peccary (Platygonus vetus
Page 209 and 210: Figure 8. Skull of the dire wolf, C
Page 211 and 212: Figure 11. The Bat Room of Megenity
Page 213 and 214: Mammalian Faunas during the Last De
Page 215 and 216: cene Paleoecology and Archaeology o
Page 217 and 218: Harrison was by far the largest spr
Page 219 and 220: 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
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Bluespring Caverns “Myst’ry Riv
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Marengo Cave, located on the edge o
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of the cave, the scout program was
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avid spelunkers and loved the cave.
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Indiana Show Caves hire Richard L.
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Section VIII: Cave Descriptions 2 1
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Cave Maps and Descriptions The foll
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een made but a voice connection sho
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intersection. The left-hand passage
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enters from a too-low passage but a
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This pit is located on a heavily wo
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Main Passage in Erics River Cave. P
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drive road. There is a pull off on
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in 50 feet. This cave has pits and
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crawling, and very little belly cra
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Not to be confused with Harrison Co
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The Old Town Spring Entrance to Mar
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placed about 150 feet inside the en
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decorated grotto. In the south end
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Robinson Ladder Cave is an Indiana
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dates. Also, except for the entranc
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Saltpeter Cave Crawford County Cave
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This cave is located along the base
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of Texas Creek and is about half a
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water is from B-B Hole, a nearby ri
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Harrison County Caves 1915 Cave was
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meandering, narrow canyon. This pas
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was rigged in 1979 by Tom Fritsch a
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Jamie Winner at Big Mouth Spring Ca
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drop. At the bottom of this drop is
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Dave Stahl at the top of the first
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Nick Smith has arranged access to t
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he returned to remove this ledge, s
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on the left side of the main passag
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degree angle. At the bottom of the
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Ryan Moran climbing Gary Pit. Photo
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This cave is presently the main cav
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You can get to the pit in two diffe
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Willie Hunt at the entrance to Jays
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T he entrance to King Leo Cave is a
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The 40-foot-tall canyon. Photo by E
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way, flowstone and some gypsum flak
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Manhole Cave, Corydon West 7.5-minu
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CIG Cave Capers Guidebook: 1984, 19
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the 56-foot drop known as The Cathe
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Sharon McConnell in Rocky Hollow Ho
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Seitz Pit, also known as Fuzzys Pit
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Harrison County Caves 375
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with the sandy crawlways and contai
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it opens into Tourist Avenue. The l
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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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