Mars Analog

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RHEOGENIC CAVES AND CAVERNOUS STRUCTURES

OF KALAUPAPA PENINSULA, MOLOKAI ISLAND,HAWAII, USA: A MARS ANALOG REVISITED

� William R. Halliday

� Chris H. Okubo

� Stephan Kempe

� Michael and Sherry Garman� J. Judson Wynne

Figure 1.



Figure 2.Comparison of braided lava tube systems on Hualalai Volcano, Hawaii and Olympus Mons, Mars. At upper left is the Poikahe system of Hualalai volcano. Its

uppermost hundred meters has the form of a narrow braided complex. It is on private land and still is unmapped. Oblique aerial photo by W.H. At lower right isan unnamed lava tube system on Olympus Mons (NASA PIA06935) of about the same diameter. A short braid is present near the right end of the photographed

segment, and a longer, uncollapsed example may be present near its center. Image credit: NASA/JPL/Malin Space Science Systems.



Figure 3.

A terrestrial analog of use of Martian lava tube caves as habitations: car camping in Malheur Cave, a privately owned ³drive-in´lava tube cave in east-central Oregon. Unfortunately few such ³drive-in´ lava tube caves are known on Earth. Photo by W.H.



The

³Seven Sisters´

of Arsia Mons

Chloe

Wendy

AbbeyAnnie

Nikki

Dena

Jeanne

³THEMIS visual image,Cushing et al. (2007), GRL

L17201´

Figur e 4.Hi-RISE image of Arsia Mons, Mars, showing ³the Seven Sisters´. Image cr edit: NASA/JPL/University of Ar izona.



Jeanne, northern flank,

Arsia Mons Volcano,

Tharsis Region, Mars

Kau Desert Pit Crater,

Kilauea Volcano, Hawaii

Pit Crater Comparison

THEMIS visual image, Cushing

et al. (2007), GRL L17201

Figure 5.Low angle view of Kau Desert Pit Craters, Hawaii, with one of ³the Seven Sisters´ at approximately the same scale. Photo by Gerald Favre and image

credit NASA/JPL/University of Arizona.



Figure 6.Looking down one of the Kau Deserr Pit Craters, showing solid termination. Photo by Gerald Favre.



Figure 7.Looking up shaft of Wood Valley Pit Crater, Kilauea Volcano, Hawaii (inset). Its diameter is similar to those of ³the Seven Sisters´.

Photo by Gerald Favre.



Figure 8.Diagram of subterranean system of Wood Valley Pit Crater, Kilauea Volcano, Hawaii. This is the only recorded example of a pit crater as the orifice of

an extensive subterranean system on Earth. From Favre, 1993 (by permission).



Figure 9.Caver on rope in Hapai Mamo Pit, Mauna Loa Volcano, Hawaii, another pit crater with a diameter similar to those of ́ the Seven Sisters´.

Photo by W.H.



Parrot Pit

Figure 10.

Parrot Pit (upper) and Kaupulehu Crater (lower),northwest rift zone of Hualalai Volcano, Hawaii. Parrot Pit is a pit crater with a diameter similar tothose of ³the Seven Sisters´. Kaupulehu Crater contains a small example of an open vertical volcanic conduit somewhat comparable to that of

Kauhako Crater. Aerial photo by W.H.



Na One Pit,Hualalai Volcano, HI

Figure 11.Vertical aerial view of Na One Pit, a pit crater on the southeast rift zone of Hualalai Volcano, Hawaii, with a diameter comparable to those of ³the Seven

Sisters´. The localized elevation of the rim is an accumulation of tephra. Aerial photo by W.H.



Figure 12.Looking down into Na One Pit from the rim. The vertical orifice of the inner pit leading to a total depth of 263 meters below the spillover point of the rim

is on the left. Photo by W.H.



Figure 13.Caver on Tyrolean traverse, preparing to lower a 250 meter rope into the inner pit of Na One Pit for its first exploration. Photo by Carol Vesely.



Figure 14.Oblique aerial view of Kalaupapa Peninsula, showing Kauhako Crater and trench. Aerial phto by W.H.



Figure 15.Preliminary geological map of Kalaupapa Peninsula, by C.O.



Figure 16.View across Kauhako Crater, showing Kauhako Lake in center right. Photo by W.H.



Figure 17.Water level view of Kauhako Lake. Photo by W.H.



Figure 18.Vertical and horizontal diagrams of Kauhako Pit and Lake, f rom Maciolek, 1982.

Divers (M.G. and S.G.) have confirmed the sketched theoretical pattern of the pit to

a depth of 122 meters. Note that the vertical section shows the pit to have a levelbottom. This has not been confirmed.



Fe-S minerals at 12m Diatom in Fe-S matrix at 12m

Calcium carbonate precipitates at 24m Calcium carbonate precipitates at 40m

Figure 19.Photomicrographs of biogenic deposits at various depths on the walls of Kauhako Pit, behind bacterial mats and strands, by M.G. and S.G.



Figure 20.Upper end of the Kaupikiawa Cave System, Kalaupapa Peninsula, Hawaii. Photo by W.H.



Figure 21.Lower orifice of Old Ladies¶ Cave, on a sea cliff of Kalaupapa Peninsula upslope from the Kaupikiawa system. Note that the entire cross-section of the

lava tube can be observed here. Photo by W.H.



Figure 22.Kauhako Trench, downslope from Kauhako Crater. This structure previously has been described as a collapsed lava tube cave, but its diameter is

several orders of magnitude larger than the largest terrestrial lava tube cave on record and it instead appears to be an elevated primary lava trench.

Coombs et al identified it as an analog of lunar rilles. W.H. photo.



Figure 23.Extended longitudinal section of Ka Lua o Kahoalii. This structure previously has been described as a lava tube cave, but its parameters

are unlike those of any terrestrial lava tube cave on record and it appears instead to be a drained part of the feeder system for a lava lake.

Its orifice (upper right) is on the surface of this lava lake, about 3 meters from the edge of the inner pit of Kauhako Crater above Kauhako

Lake. Its course is immediately beneath the sloping, talus-covered slope of the inner pit above the lake (not shown in Figure 18).

Distances below surface in feet

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