The first part of the excursion is mainly concentrated on the western lava field of the 1914 eruption, which was the latest big eruption in historic time. The surface texture of the lava field is quite variable, from typical block lava to a broken pyroclastic flow. The route follows along the southern coast of Sakurajima to the second stop, which is a good vantage point from which to observe the lava flows of 1914 and 1946. Should our visit coincide with an active period, we will experience a shower of volcanic ash. upon passing through the road junction between Sakurajima and osumi Peninsula, the route turns northward. From stop 5-3 we can look at the different features of two volcanic edifices, Kitadake and Minamidake. At stop 5-4 we will see the buried “Torii,” a shrine “gate.” After that the route follows along the coast counterclockwise to the starting point. Along the way, we will be able to see new islands that appeared during An-ei eruption (1779-1781), the steep wall of Aira caldera, and Kirishima volcanoes far off to the north (see Day 5 route map).
Driving distance, 49.2 km; driving time, 3.0 hours (including stops); starting time, 8:00 am; assembly point, entrance of the hotel; leader, Tetsuo Kobayashi.
Figures & Tables
Epithermal Gold Mineralization and Modern Analogues, Kyushu, Japan
The late Cenozoic volcanic activity in Kyushu is characterized by large-scale volcano-tectonic depressions. The sites of these depressions together with associated volcanism and gold mineralization migrated southeastward in northern Kyushu and eastward in southern Kyushu. Thus, Quaternary gold deposits in Kyushu occur within 30 km west from the present volcanic front; the Pliocene gold deposits occur farther away from the active volcanoes.
Typical Quaternary gold mineralization in Kyushu is the quartz vein type with associated adularia and minor calcite. Although host rocks are predominantly andesitic volcanic rocks and sometimes rhyolite and lacustrine sediments, the major portion of high-grade quartz veins of the Hishikari deposit discussed here is hosted in basement sedimentary rocks close to the unconformity between the basement and overlying Quaternary andesites. Five distinct alteration types are recognizable on the basis of mineral assemblages for Quaternary gold deposits. Two are the deeper propylitic alteration and the shallower smectite-zeolite alteration of the widespread and temperature-controlled type; the rest are mica-chlorite alteration, argillic alteration, and silicification of the fracture-controlled type.
Most Quaternary and some Pliocene gold deposits in Kyushu are located near small Bouguer anomaly highs in areas of regional gravity anomaly lows. In the case of the youngest deposits the gravity anomaly highs are overlapped by low electrical resistivities. The small gravity anomaly highs have been ascribed to underlying uplifted blocks of basement. The low resistivity anomalies are caused by the presence of argillic alteration of the shallow portion of the mineralized systems.
The importance of circum-Pacific volcanic belts as a source of rich gold deposits has been highlighted by recent discoveries of deposits such as McLaughlin, California; El Indio, Chile; Lihir, Papua New Guinea; and Hishikari, Japan. In particular, epithermal gold deposits related to Quaternary volcanoes have become the focus of exploration in island-arc systems of the western Pacific rim, in which Kyushu lies. Kyushu is the principal gold-producing area in Japan. There are several important gold deposits which are related to waning or extinct geothermal systems of Quaternary age. The erosion level in the Quaternary volcanic areas is shallow so that some of the surface expressions are different from those of older deposits. The purpose of this paper is to outline the characteristics of gold mineralization of Quaternary volcanic areas in Kyushu on the basis of detailed geologic and geophysical investigations undertaken over the last ten years. Major epithermal gold deposits in Kyushu occur in late Cenozoic volcanic areas which were formed by the subduction of the Philippine Sea plate beneath the Eurasian plate.