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Underground sanctuaries

Many caves in Myanmar are sacred places. They probably have always been, but since the Buddhist religion spread in Southeast Asia, the caves of Burma have become places of refuge for monks and hermits, and places of worship for the entire population. Traces of attendance for religious purposes can be found in almost all the more accessible caves . Some of them, including the well-known Pindaya, and others less known, like Myin-Ma-Hti near the town of Kalaw , have been adapted for this purpose, with ceramic flooring and internal lighting, and are full of votive stupas and statues representing the Buddha. The Pindaya cave , in particular, is one of the most important holy places for the Buddhist religion all around Asia and receives several hundred thousand visitors every year.
Their impact on the conditions of the cave, from the environmental point of view, is considerable , but the richness and socio-cultural importance of these place, frequented from thousands of years, is huge and it deserves the greatest attention to be conserved.

Ponte Colossale

The paintings of Tepelmeme’s Puente Colosal JuquilaIn the course of the 2002 Juquila expedition, a particularly significant example of the recurring association between karst environments and ancient human activities was observed. Inside Tepelmeme’s Colossal Bridge there are numerous cave paintings which show how the spectacular tunnel had repeatedly kindled the interest of the indigenous groups which lived in the area in Pre-Hispanic times. The paintings are also of excellent technical and aesthetic quality, to the point of being among the best examples of Mexican cave painting.
Traditionally known of by the local inhabitants, the Tepelmeme paintings have been adequately described in scientific literature only in the last few years. In the mid 1960s, they were observed by Ross Parmenter, who was also given a feline bone decorated with complex engravings by a local man who had found it in the tunnel. However, Parmenter’s report remained unpublished and only in the mid 1980’s was a better description of the paintings published by the archaeologist Carlos Rincón Mautner. Finally, in 2004, Javier Urcid carried out a detailed research project during which the paintings were surveyed and many archaeological remains were found, both inside the Puente Colosal and in its surroundingsJuquila. The results of these researches indicate that the first ancient traces at the Puente probably date back to the Archaic period (7000-2000 B.C.). It was however during the Late Classic period (6th -9th Centuries) that the majority of the Puente’s paintings were painted by ñuiñe groups, belonging to a cultural tradition typical of the Lower Mixteca and whose exact linguistic affiliation is still unknown. The Puente Colosal’s ñuiñe paintings consist mainly of calendar glyphs accompanied by numbers. In all likelihood they are calendar names (that is, the names which Mesoamericans adopted based on their day of birth) and their placement suggests that the different glyph groups should be interpreted as genealogical records. That is, as genealogical sequences which attest to the noble pedigree of some individuals. The most spectacular glyph group, for example, could be read as “1 Grass is son of 11 Rain, in his turn son of 10 Owl”. The heterogeneous stylistic characteristics of the ñuiñe paintings, like the many instances of overlapping, indicate that the paintings were executed at different times, the majority of which at the end of the Classic period, a time during which several settlements near the Puente Colosal were thrivingJuquila. Among the paintings not having a genealogical nature, the figure of a naked prisoner with tied arms and losing blood from his penis, stands out and alludes to the ‘fertilizing’ characteristic of sacrificing war prisoners. The later and less striking paintings are instead dated to the Early Postclassic (900-1250 A.D.), the era to which the previously mentioned engraved bone also belongs. The last Pre-Hispanic evidences at the Puente Colosal (Late Postclassic, 1250-1500 A.D.) are not paintings but turquoise mosaics pieces, small jade beads, copal fragments, and the remains of offerings placed inside the tunnel. According to local testimonies collected by Urcid, in the past some wooden masks covered with turquoise mosaics were found in the tunnel, unfortunately they were burned as they were considered the work of the Devil. The Puente Colosal’s paintings and offering remains indicate that ancient indigenous groups perceived that spectacular karst environment as a place having a sacred nature and being associated with the underground world of fertility and ancestors. As they did with most caves, the natives interacted with these cosmic environments through ritual behaviour, whose material residues are those which we can still observe today within the Puente Colosal. Torna al progetto

Expedition “Palawan 2008”, Philippines

The "Palawan 2008" expedition, in the karst of St. Paul (Palawan, Philippines), was held from February 22 to March 12, 2008. The expedition was attended by 12 Italian cavers, two Mexicans and two English. The mission was part of a larger project of research and documentation, that La Venta Association is developing in collaboration with the authorities of the Puerto Princesa Subterranean River National Park and the capital of Puerto Princesa.

Aims of the expedition were: the completion of the photographic documentation of the underground river, especially about his extraordinary biological aspect, the exploration of some cavities in the NE sector of the massif seen during the expedition in 2007, the approach to the summit areas of St. Paul entering the karst area by SO and the completion of the exploration and survey of some cavities of the S area , in the village of Cabayugan. The expedition operated simultaneously in the three areas, unfortunately in conditions made difficult by bad weather characterized by strong afternoon thunderstorms that have made risky the exploration of the active cavity. The bad weather conditions have prevented then to reach the summit areas of the limestone ridge.

The group that has worked in the NE sector has completed the exploration of two important caves that act as sinkholes as well as many blind valleys that border the eastern edge of the karst. The two caves, called Nagbituka 1 and Nagbituka 2, develop along the contact between limestone and impermeable rocks and are characterized by short pits and long slides that are crossed climbing. The explorations have allowed us to ascertain that the two caves are parallel to the main systems of the Underground River, which runs from SW to NE along the ridge of St. Paul, and probably feeds the springs located along the limestone coast. So they are not connected with the main collector of the Underground River.

Nagbituka 1 was found to be 270 m deep, which makes it one of the deepest caves of the Philippines, for a development of 650 m. The second has a depth of 130 m for a development of 450 m. Both the caves have large areas of collapse and lateral galleries with concretions. At the moment it doesn't seem possible to make new significant developments in either of the two cavities. In the area there are in any other way active sinkholes yet to be explored.

In the south sector, the one in which were concentrated the efforts of the previous expedition, were not discovered any important caves. The summit area of the limestone plateau, where in the aerial photos were clearly visible large collapsed inlets, was unattainable on that side due to the presence of steep slopes of sharp limestone blades, very difficult, and very dangerous to cross. The teams, although expert have not been able to go more than a few hundred meters beyond the edge of the limestone relief, without reaching any of the entrances seen in the aerial photos. Have been discovered some rather modest cavities of contact at the base of the limestone buttresses, with limited development and closed by the alluvial deposits.

No significant new developments, however, inside o the underground river, where some branches, detected during the early stages of exploration ( 1990-1991), have been revised. Were, however, identified a number of promising windows that need specific equipment to be climbed. Inside the underground river was made a great job of photographic documentation of the hypogean fauna.

Myanmar 2012

In 2012 an international expedition led by Joerg Dreybrodt saw one of its members on the tracks left by the 2005 expedition. In that occasion were investigated different areas of the central regions of Shan. The return to the village of Pinh-ton to resume relations with the locals was an important part of the expedition and it was a pleasant surprise to see how much were impressed the memories of the Italian explorers after 7 years.

Only in the 2013 January expedition, organized by the Myanmar Caves Documentation project, the resurgence of Namun Spring was partially explored and topographed for a total development of about a kilometer.

4c_1998_1999

1998-1999: reconnaissances 4CDuring two investigations carried out in November 1998 and May 1999 two large caves located downhill, both near the dell and on the high surrounding mountains have been partially explored.
During these investigations we explored around 5km of underground tunnels, although most of these have not been fully explored. In some canyons we saw tens of caves with halls opening on vertical walls, thus we could only reach them through climbing techniques: free and aid climbing, fixed rope ascents. Torna al progetto

4c_2001_2002_2003

2001 - 2002 - 2003: expeditions 4CIn order to explore these caves and to discover new ones it will be necessary to equip advanced base camps in canyons and mountains, overcoming difficulties due to water transfer (there isn’t any known spring). As regards extremely deep and complex caves it will be necessary to equip base camps inside the caves.
4CDuring cave explorations we will carry out instrumental mapping, observations and geological sampling, surveys on physical data such as temperature, air flows, relative humidity, etc. As regards the spring lakes, research will be based on the underwater topography of the most significant pools and on the exploration of conduits that will be discovered. The goal is to produce the minimum impact on submerged ecosystems. Moreover we will try to describe through topographic mapping the morphology of inflow and outflow conduits in relation to the lithology of the explored sites.
 Specific hydro-geological studies will be carried out on water bodies: precise height measurements of each lake on the mean sea level and comparison of relative heights; measurements and comparison of temperatures; various types of chemical and physical analyses; measurements and monitoring of flow rates and levels, calculations of the speed of flow of intake conduits and drainage galleries. In the end a subaqueous photographic documentation will be realised, as it does not yet exist.
Some figures of the project that give an idea of the work performed: more than 70 researchers involved, 65 new caves explored, 8 km of underground topography, almost 200 geo-topographic observation points, tens of underwater immersions, thousands of metres of rope used within pools in mines and caves, thousands of kilometres walked, amongst all participants, on giant mountains without paths. Not to mention the numerous canyons descended for the first time by man. Torna al progetto

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