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Speleogenesis and Karst in New Zealand
Kermode, L.O. The Speleological Society 1997 Journal of the speleological society of korea Vol.5 No.2
The cavernous rocks of New Zealand can be grouped broadly into two main geologic types-the massive, metamorphosed, Ordovician, Mt. Arthour Marble of north-west South Island, and the stratified, bioclastic, Tertiary Te Kuiti limestones of western regions of both islands. Although much cave exploration has been carried out in both these regions, the principal study so far has involved caves and karst in the central western portion of North Island near the well-known Waitomo Caves, where some 85km of caves have been surveyed during the past 12 years by members of New Zealand Speleolgical Society.
SPELEOLOGICAL POTENTIAL OF KAMCHATKA OBLAST
Ha, William R.lliday The Speleological Society 1997 Journal of the speleological society of korea Vol.5 No.2
In September 1996 I spent 8 days in Kamchatka Oblast of Silberia, speaking at the institute of Volcanic Geology and Geochemistry in Petropavlovsk and participating ina field excursion to the 1740 and 1975 lava beds of Tolbachik volcano. By international standards, the caves of these flows are small. But recently it has appeared that variations in chemistry and gas content of pahoehoe basalts makes profound variations in their lava tube caves. Thus it is important to look at as many speleoliferous regions as possible. This trend continued at Tolbachik.(omitted)
Cody, Ashley The Speleological Society 1998 Journal of the speleological society of korea Vol.7 No.2
This article is a brief study of some properties of Pupu Springs together with comparative comments on nearby rivers and resurgences. The information presented was collected by several people over the period from January 1970 until November 1971, and all analyses were made within a laboratory. “Waikoropupu” is a Maori name meaning “where water bubbles up through a throat.” However the name is more commonly simply 'Pupu Springs. Location is about 7km from Takaka; the outflow from the Springs flowing into the Takaka River at a point within 2km of the town. Grid reference for the Springs is: N.Z.M.S. I, Takaka, S8 (1968) 170819.(omitted)
Notes on the Volcanic of S. Miguel Island
Nnnes, J.C.,Braga, T.,Constancia, J.P. The Speleological Society 1997 Journal of the speleological society of korea Vol.5 No.2
The island of S.Miguel is part of the Azores, an archipelago composed of nine volcanic islands situated between the european and american continents. Aligned in a general WNW -ESE trend, between latitudes 37$^{\circ}$ -40$^{\circ}$ N and longitude 25$^{\circ}$ -31$^{\circ}$ W, the Azores islands show a very special geotectonic setting, at the triple junction of the Eurasian, African and North American lithospheric plates.(omitted)
Emberson, Rowan The Speleological Society 1998 Journal of the speleological society of korea Vol.7 No.2
The Bullock Creek Caves are located adjacent to the usually dry river bed of Bullock Creek, which reaches the sea about a kilometer north of Punakaiki. The caves have been comprehensively written up by Rodgers(l972). Under conditions of normal water flow Bullock Creek submerges where the stream meets limestone on the west side of thier Punakaiki syncline. In flood conditions it overflows the first submergence and progressively floods a series of smaller submergences down valley until it comes to the caves shown on the map. All these with the exception of Wazpretti Cave and Dry Valley Cave are probably more or less flooded during and after heavy rain.(omitted)
A Note on Biogenic Effects of Coralloid Speleothems in Round Mountain Lava Cave, Oregon, U.S.A.
Kashima, Naruhiko,Ogawa, Takanori The Speleological Society 1999 Journal of the speleological society of korea Vol.9 No.2
Corralloid speleothems from Round Mountain lave cave are are studied by scanning microscope and electron microprobe analyses. Scanning microscopy observation indicates that the diatom Melosira seems to contribute significantly to siliceous coralloid speleothems Electron microprobe confirms the presence of diatom and fragmental minerals(plagioclase and orthopyroxene) in coralloid speleothems. Chemical analysis of 3 diatom cells gives SiO2(74.8%), Al2O3(0.12%), FeO(0.11%), CaO(0.47%) and MgO(0.81%).
The Geographic Environment of Hwaam Cave Area
Hong, Chung-Ryol,Won, Pyong-Kwan The Speleological Society 1996 Journal of the speleological society of korea Vol.4 No.1
The geographic environment means the general state of the environment in the area. Especially, which means the generation cause, the development process of the cave, and the validity of cave development and conservation in the side of the place of the cave. This study put emphasis on lying in which place Hwaam cave in Tong-myon, Chong son-gun, Kangwondo is situated and having in which stand is in comparison with other districts, and how the geological structure which determine the cave forming cause is.(omitted)