New discovery of prehistoric archaeological remnants in volcanic caves in KrongNo, Dak Nong Province

Vietnam Journal of Earth Sciences, 39(2), 97-108, DOI: 10.15625/0866-7187/39/2/9186 97 (VAST) Vietnam Academy of Science and Technology Vietnam Journal of Earth Sciences New discovery of prehistoric archaeological remnants in volcanic caves in KrongNo, Dak Nong Province La The Phuc1*, Nguyen Khac Su2, Vu Tien Duc3, Luong Thi Tuat1, Phan Thanh Toan2, Nguyen Thanh Tung4, Nguyen Trung Minh1 1Vietnam National Museum of Nature, Vietnam Academy of Science and Technology 2Institute of Archaeology, Vietnam Academy of Social Science 3Institute of Social Sciences of Central Highlands, Vietnam Academy of Social Science 4Phu Gia Phat Company Received 24 January 2017. Accepted 21 February 2017 ABSTRACT The Krongno Volcanic Geopark in Dak Nong province with a unique and largest volcanic cave system in SE Asia discovered in 2007 occupies an area about 2,000 km2 in the Krong No, Cu Jut and Dak Mil districts and several neighboring communes in the Dak Song and Dak Glong districts. In 2016, Vietnamese archaeologists discovered a number of archaeological sites in hilly, farmland and riverine areas in the Krong-No Volcanic Geopark; however, none had been found in the volcanic caves. During the late December 2016 - early January 2017 field trip, a survey team led by Vietnam National Museum of Nature, VAST, discovered a series of archaeological sites and relics with a relatively high density in volcanic caves in the Krongno Volcanic Geopark. The discovered archaeological remnants include (1) stone materials and tools such as dish-shaped tools, short axes, blade-ground short axes, oval axes and blade-ground oval axes; flake tools, stone flakes, stone slabs; anvils, graters, pestles, etc., hand-fitting sharp quartzite stones and pieces of loess; (2) pottery, containing various ceramic tools with different thicknesses, mostly fired at low temperature, crumbly, made of fine sandy loam, hand-kneaded, simple forms, mainly pots and containers having rela- tively sharp sculptings of varied patterns on the pottery shards such as dot-dash, dotted line, dashed line, twisted rope, etc.; (3) animal and teeth bones, including fragments of animal bone, or bones of prehistoric human (?). The bones are mostly decayed and fragile when dry; the hollow portions of bones are filled with porous clay slurry. In addition to the bone fragments, there are cheek teeth of animals some are fossilized. Preliminary determination suggested the teeth are of herbivores. Most of the archaeological artifacts were found in caves with flat floors, having mouths fac- ing east, southeast or south heading to relatively wide areas to absorb the light, close to water sources and convenient to commute. These are the first prehistoric archaeological findings in volcanic caves in Vietnam, which will be stud- ied in more detail by Vietnam National Museum of Nature, VAST, and other authorized agencies to highlight a new type of settlement, a new adaptive trend of prehistoric dwellers in the Central Highlands and to open a new archaeo- logical study in the volcanic caves in Vietnam and Southeast Asia. ©2017 Vietnam Academy of Science and Technology 1. Introduction1 Krong No Volcanic Geopark (KVG) *Corresponding author, Email: laphuc@gmail.com contains not only important geological values but it also bears cultural, ecological and archaeological meaning, that meets some of the UNESCO criteria of an aspiring global geopark (UNESCO, 2009). The nominated La The Phuc, et al./Vietnam Journal of Earth Sciences 39 (2017) 98 KVG covers an area of about 2,000 km2 in Krong No, Cu Jut, Dak Mil districts and sev- eral neighboring communes in Dak Song and Dak Glong districts (Figure 1). While implementing the science and tech- nology project on “Investigation and assess- ment of geological heritage and establishment of Krong No Geopark, Dak Nong province”, several questions relative to the cultural herit- age were raised to what were the significant archaeological values in the KVG? How did prehistoric people live on and adapt to chang- es in the landscape and ecological environ- ment throughout thousands of years? How did they exploit the local natural resources to meet their needs? To answer these questions, in January 2017, a survey team including ge- ologists, culturologist, and archaeologists, led by Vietnam National Museum of Nature, VAST, re-examined the old relics, started the new survey and has discovered a number of archaeological sites in the volcanic caves in the Krong No district. The survey has shown some surprising results. The archaeological records show that be- fore 2017 archaeologists had discovered more than 30 archaeological sites in Dak Nong province (Nguyen Khac Su, 2007; Vu Tien Duc, 2015), none of this was in the volcanic cave. Archaeological remnants were collected at 12 sites in KVG, including Trung Son, Thac Lao, Suoi Tre, Thon Sau, Thon Bay and Thon Tam (Cu Jut district), Canh Nam, Nam Xuan (Krong No district), Truong Xuan, Dak Ton (Dak Song district), Dak R'la, Dak Lao (Dak Mil district). Among these, the archaeo- logical site at Thon Tam, Dak Wil commune, Cu Jut district, was excavated twice in 2006 and 2013. The initial research results of these sites indicated that the remnants belong to the Neolithic Age and Early Metal Age, about 6,000 to 3,000 years ago (Le Hai Dang et al., 2013; Nguyen Gia Doi, Le Hai Dang et al., 2006; Nguyen Khac Su, 2004, 2007; Truong Quang Quang et al., 2011; Vu Tien Duc, 2015). 2. Archaeological objects in volcanic caves in KVG 2.1. Geology of volcanic cave area The geological formations in the volcanic cave area are relatively simple, comprising only of La Nga, Xuan Loc and unconsolidated Quaternary formations (Figure 2). La Nga formation (J2ln) is widely distrib- uted in the west of cave area (Figure 2) and consisted mainly of terrigenous sediments which are divided into three sections. Section 1: weathered and cracked gray siltstone turned yellowish gray color; blackish gray claystone with the shiny surface with intercalation of thin layers of yellow sandstone; darkish gray sandy siltstone; the thickness being about 250- 300 m. Section 2: black siltstone thinly lay- ered, with idiomorphic pyrites scattered on the surface along with clayish shale fragments, and thin layers of sandstone containing white mica flakes; the estimated thickness about 100 m. Section 3: gray, light gray, yellowish gray medium-to-fine sandstone alternating with gray, yellowish gray sandy siltstone, silt- stone and thin layers of claystone; the thick- ness being about 350-400 m (Nguyen Duc Thang, 1989). Xuan Loc formation (β/Q12xl) is widely distributed in the central part shown in Figure 1, with basaltic rocks being the main compo- nent which is divided into three sections. Sec- tion 1: The brownish gray-to-black volcanic ash, sometimes tuff interbedded with layers of gray porous basalt; the thickness of about 35 m. Section 2: basaltic lavas including oli- vine basalt, darkish gray dolerite, plagiobasalt, having mostly massive structure; the thickness of about 45-50 m. Section 3: consisting of fis- sured lava flows along with explosive eruptive products with black, grayish green olivine basalts being the main rock type, some subor- dinate amount of volcanic bomb and breccia. The basalts are massive and a minor amount of porous type; the thickness is about 45-51 m (Nguyen Duc Thang, 1989). Vietnam Journal of Earth Sciences, 39(2), 97-108 99 Figure 1. Distribution map of Krongno volcanic geopark in related geological formations in Vietnam La The Phuc, et al./Vietnam Journal of Earth Sciences 39 (2017) 100 Figure 2. Distribution map of volcanic caves in Krong No Undivided unconsolidated Quaternary formations (Q) are widely distributed in the east of the cave area (Figure 2), comprising sandy clay, patchy-colored silty clay and lat- erite, occurred as unconsolidated accumula- tions in the lower session, forming the first- order terrace of the Srepok River, 3-6 m high; the total thickness is about 5-6 m (Nguyen Duc Thang, 1989). Mineral resources in the study area are mainly puzzolanas a weathered product from Xuan Loc basaltic formation in the Buon Choah commune, Krong No district. Besides, basaltic construction material and brick-made clay are found along the Srepok River valley (Nguyen Duc Thang, 1989). 2.2. Geological characteristics of the ar- chaeological site-housing caves Cave systems discovered in the area are re- lated to the Xuan Loc basalt formation (Figure 2). So far Chu B'Luk volcano in the Buon Vietnam Journal of Earth Sciences, 39(2), 97-108 101 Choah commune, Krong No district (601m high relative to sea level, the crater is ~63m deep) is the only visible volcano in the area. Caves are found scattered around this volcanic area. Most of the current cave mouths are sec- ondary, formed following cave ceilings’ col- lapse; as a result, they are usually dome- shaped, and basaltic rock boulders are com- monly seen nearby. Some cave mouths are primary, formed following the emission of volcanic gas and the cooling of eruptive basal- tic lavas. These mouths are usually circular, steep to great depth (depth of C7 cave >10 m, “Python” cave ~25 m, P9 cave ~23 m). Cur- rently, only archaeological sites related to cave with secondary mouths have been dis- covered; especially, in caves with flat floors near wide, easily accessible, well-light mouths, and close to water sources. In con- trast, archaeological artifacts were not yet found in caves with narrow mouths, poorly light and stuffy. 2.3. The archaeological discovery in the Krong No Volcanic Geopark Thon Tam site: The archaeological site in Thon Tam (Dak Will commune, Chu Jut dis- trict) was excavated in 2006 with an area of 52 m2 and in 2013 with an area of 37.5 m2. The site is at altitude 382 m relative to the sea level and coordinates of 12042’31.3’’N and 107048’25.9’’E. The two excavation sites provide the same results. The cultural relics include stone tools, semi-finished tools, stone flakes, stone materials and pottery found in a red basaltic weathering bed with a thickness of 50cm. However, no traces of residential ar- chitecture, animal bones, charcoal ash were found. The discovery of the remnants suggests that Thon Tam was a stone ax ‘factory’, dated to the Middle Neolithic (about 5,000 years ago) (Le Hai Dang et al., 2013; Nguyen Gia Doi, Le Hai Dang et al., 2006; Vu Tien Duc, 2015). The survey around the excavation site in Thon Tam (Dak Will, Chu Jut district) at the altitude of 335m has found other 15 hills (now are black pepper plantations or industrial plants) surrounded by water pools. On the sur- face of these hills found were semi-finished stone axes, stone flakes, and stone materials. The discovery of oval axes, short axes, disc- shaped scrapers with one or both knapped sides and polished edge in this area bearing Early Neolithic making techniques of the Hoa Binh Culture, well-known in Vietnam and Southeast Asia, suggesting that the area is a concentration of remnants of prehistoric set- tlers in the Central Highlands. The survey of remnants in volcanic caves: C1 cave (Figure 3, Survey point: KVG107, GPS symbol: 083). The cave is about 300 m from a nearby pathway, easily accessible. Its mouth is nearly isosceles triangular (Figure 3), facing the east at 90°, the width of the base about 3.5-4 m, the ceiling about 3 m high, and >100 m long. The mouth of C1 cave was formed by thin and weak ceiling collapse. At the center of the floor closer to the mouth there is a narrow ba- saltic ridge with rough surface due to solid la- va ‘stalagmites’, all looks like a large croco- dile, heading to the cave mouth (Figure 4). Pieces of pottery, potsherds with dotted line pattern, red pottery broken pieces, made by fine sandy clay, low temperature fired, were collected on the floor. In addition, angular quartz fragments, 2 to 4 cm size were found in the cave. Whether these fragments were quartz tool-making wastes of prehistoric peo- ple or of shooting projectiles of homemade catapults of the local people remain unan- swered. Several pieces of ocher-stained limb bones were also recovered in the cave, possi- bly human bones (?). From the mouth of C1 cave to 100° east- ward is part of the same cave having ceiling collapse forming a double-mouth cave. There is a sunroof near the eastern mouth, with a di- ameter of about 1.7 m. This part of the cave is about 17-20 m long expanding in the sub- latitudinal direction. Especially, a tree-shaped mold, more than 5m long and about 10cm in diameter, is seen on the south wall. La The Phuc, et al./Vietnam Journal of Earth Sciences 39 (2017) 102 Figure 3. Mouth of C1 cave Figure 4. C1 floor At the foot of the northern flank of C1-1 cave, a black soil trench was discovered con- taining many potsherds, pottery parts of 2-3 mm thick, some incised with dash patterns. Found also were a few shells of mountain snails, including Cyclophorus sp. - C3 cave (Survey point: KVG108, GPS symbol: C3): C3 cave is about 1 km west- northwest from C1 cave. The cave is 594.4 m long (La The Phuc et al., 2015) having mouth facing east at 110°. The mouth was collapsed, currently is about 4.5-5 m below the surround- ing relief, 20 m wide, 15m high, with basalts falling following the ceiling collapse piling up in front. The thickness of current ceiling cover is about 3-5 m. A tree-shaped mold is seen on the left wall of the mouth having a diameter of about 40 cm. Rock boulders up to several cu- bic meters are seen scatter on the floor. C3 cave at its current stage is not suitable for set- tlement, however, if it was a place of prehis- toric humans, any remnants left must be bur- ied under the falling rocks. No archaeological relics have been found in the cave. - C4 cave (Survey point: KVG109, GPS symbol: C4): C4 cave is 251 m long, about 300-400 m from C3 cave southeastward (La The Phuc et al., 2015). The mouth is in a 5-8 m deep depression, resulted from a ceiling collapse, half-round-shaped, facing south at 190°. The ceiling height 4.5-5 m high and the cave is 12-15 m wide. The floor is relatively flat, lower towards the mouth, covered with moist soil and basalt fragments with sizes of 10-40 cm. The floor is gradually higher as the cave becomes deeper, exposing solid basaltic bedrock (Figure 5). About 40 m from the mouth the cave turns left and extends deep in- side. A large basaltic boulder, about 1.5 m3, lies near the mouth also as a result of the ceil- ing collapse. Several archaeological artifacts were discovered near the mouth, including pebble materials, axes, stone flakes, anvils made from riverine pebbles, a piece of opal - chalcedony; animal teeth, loess with the trace of rodent teeth. Also found are crude potter- ies, small pottery pieces of 2-3 mm showing sculpting decoration similar to those observed on ceramics of the Neolithic Age in this area dated at 4,000-5,000 years ago (Figures 5, 6, 7, 8, 9, 10, 11). - Additional survey point in the area of C4-1(Survey point: KVG109/1): South- southeastward from C4 cave, across a lowland because of the ceiling collapse, there are two short cave branches lying parallel each other. Each cave is 100 m long with two mouths at both ends (due to ceiling collapse). Two northwestern mouths face 330° NW, towards the C4’s mouth. These two branch caves, hav- Vietnam Journal of Earth Sciences, 39(2), 97-108 103 ing similar sizes, were possibly separated from the main C4 cave. The sectional area of each branch is elliptical, about 12 m high and 15-20 m wide. A pile of basaltic rocks formed by ceiling collapse is seen near the southern mouth of the eastern cave. The wall in the northern mouth of the eastern cave is com- posed of porous basalt with large vesicles, coated with a thin layer of volcanic glass. Fragments of broken riverine pebbles and stones with hitting cracks (material stone) of prehistoric humans were found on the floor in the western branch cave. - C6 cave (Survey point: KVG117, GPS symbol: 091): C6 cave is 180.3 m long, about 200 m from C4 cave to the east, with the mouth facing southeast at 140° (La The Phuc et al., 2015). The cave spreads in the southeast - northwest direction from the mouth. A light well, about 2 m in diameter, is located at the end of the northwestern side. The ceiling coat- ing is fairly solid, 5-8 m thick above the mouth and gradually becoming thinner inside. From the light well, a branch expands to the northeast, then makes an elbow-sharp turn southward to join the major cave branch. The floor of the minor branch is higher than the main branch and is relatively flat. The place is good for living for privacy and air circulation thank to the light well at the end of the cave. The floor of the major branch is relatively smooth, except for some basaltic rocks scat- tered on the floor. In general, the C6 cave is favorable for the residence of prehistoric peo- ple. Many archaeological artifacts were dis- covered in the cave such as semi-finished stone axes, basaltic stone flakes, loess, grav- els, and thick potsherds of 1.5-2 mm with plain surfaces or having twisted rope pattern (Figures 12, 13, 14). Figure 5. Mouth of C4 cave Figure 6. Stones and Potteries at C4 cave Figure 7. Disc-shaped tool, C4 cave Figure 8. Disc-shaped tool, C4 cave La The Phuc, et al./Vietnam Journal of Earth Sciences 39 (2017) 104 Figure 9. Short axe, C4 cave Figure 10. Anvil made from pebble, C4 cave Figure 11. Potteries, C4 cave Figure 12. Potteries, C6 cave. Figure 13. Fossil of pig teeth, C6 cave Figure 14. Human limb bones (?), C6 cave - C6’ cave (Survey point: KVG118, GPS symbol: 092): C6’ cave is approximately 200- 300 m from C6 cave south-southeastward, with a dome-shaped mouth >10 m high (Fig- ure 14). C6’ cave is ellipse- shaped, about 15 m wide and 13 m high. It is possible that C6 and C6’ caves were once a unity but divided following a ceiling collapse. The floor of C6’ cave is relatively flat, with basalt rocks protruding on both walls. There are grooves on the wall of C6’ cave, suggesting lava flow direction. The alignment of grooves is vertical or twisted, along with gravitationally oriented stalactites observed on the walls, suggesting Vietnam Journal of Earth Sciences, 39(2), 97-108 105 that the lava flows by were twisted, leaned along the cave walls due to gravitational ef- fect during the C6’ cave formation process. Inside the cave, nearby the mouth 13 stone ar- tifacts, 27 potsherds and several pieces of an- imal bones and teeth were discovered. The stone remnants include 3 pieces of material stone derived from riverine pebbles from Srepok River (?); claystone, quartz and clay siltstone slate; 6 pieces of primary and sec- ondary stone flakes, separated from claystone, fine-clay siltstone, with sizes shorter than 7cm; 4 stone axes with one knapped side, 2 made from basalt, others made from meta- morphosed siltstone to quartzite state (Figures 16, 17, 18, 19, 21). Pottery was made from coarse-grained sandy clay; ceramic coating of some pieces was peeled. The surface was in- cised with dash patterns or dash- circle-shaped patterns. There are two pieces with bulging mouth, bell-shaped, thick edge; and rounding- shaped, without mouth edge; one piece with mouth decorated with incised dash and circle- shaped patterns, having the thickness about 0.4-0.6 cm (Figure 19). - C6.1 cave (Survey point: KVG120): C6.1 cave is 293 m long, about 270 m from C6 cave south-southeastward (La The Phuc et al., 2015). This area is a largely subsided terrain containing 3 cave mouths: + Mouth 1: faces north at 10°; two potsherds were found here; + Mouth 2: faces east at 100°. Several archaeological artifacts were discovered by local people while exploiting bat droppings at this site. + Mouth 3: faces south at 160°. Like mouth 2, while digging the cave foundation for bat droppings local residents found many archaeological artifacts, including tools such as oval axes, blade-sharpened oval axes, blade-sharpened short axes (Figures 22, 23, 24), stone flakes and potteries similar to those in C4 cave. Figure 15. Mouth of C6 cave Figure 16. Relics on the floor of C6 cave Figure 17. Stone flake, C6 cave Figure 18. Stone flakes, C6 cave La The Phuc, et al./Vietnam Journal of Earth Sciences 39 (2017) 106 Figure 19. Quartz tool, C6 cave Figure 20. Potteries at C6 cave Figure 21. Ocher at C6 cave Figure 22. Oval axe at C6.1 cave Figure 23. Oval axe with polished edge C6.1 cave Figure 24. Short axe with polished edge, C6.1 cave 3. Initial Remarks - There are many archaeological sites in the Krong No Volcanic Geopark area, particu- larly in the volcanic caves. Preliminary sur- veys from cave C1 to cave C6.1, we have found prehistoric archaeological sites contain- ing pieces of evidence of early human settle- ment and tool making in the volcanic caves. These are the first prehistoric archaeological findings in volcanic caves in Vietnam. - The volcanic caves in the Krong No vol- canic area, in particular, and the Central High- lands, in general, were very meaningful to the prehistoric dwellers, especially when their liv- ing techniques were low. The inspected caves in the KVG area are relatively wide, well- Vietnam Journal of Earth Sciences, 39(2), 97-108 107 ventilated, and easy to approach. With smooth floors, proximity to water resources, mouths facing east, southeast or south to receive the light, these caves appeared to meet ideal pre- requisites of “cavemen” to settle in. The sur- vey revealed that ancient people did reside in the volcanic caves and take shelter under ba- saltic roofs where they made their stone tools and potteries with relatively high skill; - In creating stone tools, they knew how to choose hard and ductile riverine pebbles such as silicic chert, silica-rich shale, quartzite or quartz, etc. They used stone knapping tech- niques directly on one or two sides to create the tool edges. Sometimes they used chopping techniques to separate stones into flakes for tool making. Beside major knapping tech- niques, they could also use sophisticated knapping techniques to improve and smooth- en blade edges. With regards to forms, the ancient people were able to make shaped tools, such as oval or sub-rectangular axes, sub-circular tools, stone flakes, stone slabs, anvils, pestles, etc. These tools were common in tribes during the Neolithic Age. By experiment, observation and ethnographic comparison, archaeologists suggested that these tools could be used to cut down trees, clear forests, butcher wild ani- mals, slice herbs, prepare food or work on bamboos or woods into tools and hunting weapons. Although only a few ceramic remnants have been discovered in the caves, but they indicate being produced with the ingenious techniques. They are potteries, made from fine sandy clay, manually molded, simple forms, mostly pots and containers with a thin ceramic frame, ce- ramic coating, square-shaped decoration with incised dash or dotted patterns. These are common ceramics in the archaeological rem- nant in the Late Neolithic and Early Metal Age. - With tools preserving the techniques of post - Hoa Binh culture and ceramic features, it can be suggested that there may be many generations resided successively in the caves and under rock shelters in the KVG, dated from the Middle Neolithic (6,000-7,000 years ago) to the Metal Age (2,000-3,000 years ago), even in the last several centuries. To clarify this prediction, it is necessary to carry out excavations, stratigraphic studies, chemi- cal analyses on the ceramic and rock samples chemical and petrological compositions and ages by spore and pollen tests and radiometric dating. - This is the first time the residential relics of prehistoric people have been discovered in volcanic caves and under basaltic rock shel- ters in Vietnam, highlighting a new type of settlement, a new adaptive trend of prehistoric dwellers in the Central Highlands and opening a new archaeological study in the volcanic caves in Vietnam and Southeast Asia. However, these are only the initial find- ings, the geologists in Vietnam National Mu- seum of Nature and the archaeologists of the Institute of Archeology should continue to discover new cave remnants, to carry out the excavations and systematic intensive studies on these remnants, contributing to the re- search on cultural-historical process of inhab- itants in Dak Nong and in Central Highlands, in general, adding a great valuable of culture- history of prehistoric humans in KVG. Aknowlegements The survey team gratefully thank Vietnam National Museum of Nature, VAST, Depart- ment of Science and Technology and leaders of Dak Nong for providing the most favorable conditions for the survey team to fulfill the scientific study and achieve the new findings. This report was completed during the imple- mentation of the project “Investigation and assessment of geological heritage and estab- lishment of Krong No Geopark, Dak Nong province”. 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