How to Develop Good Practices Document Package from Different Type of References.How to Upload and Encode References to the Good Practices Database.Biodiversity Policies in the ASEAN region.How ASEAN is Faring in Biodiversity Conservation.90-Day Particle Dispersion Simulation for Vietnam-Philippines Sub-domain (Southwest Monsoon).90-Day Particle Dispersion Simulation for Vietnam-Philippines Sub-domain (Northeast Monsoon).90-Day Particle Dispersion Simulation for Indonesia-Philippines Sub-domain (Southwest Monsoon).90-Day Particle Dispersion Simulation for Indonesia-Philippines Sub-domain (Northeast Monsoon).90-Day Particle Dispersion Simulation for AMS (Southwest Monsoon).90-Day Particle Dispersion Simulation for AMS (Northeast Monsoon).Taxonomy: Key to the conservation puzzle.Invasive Alien Species: Keeping intruders out.Inland Waters: ASEAN’s most threatened ecosystems.Forest: Still an overdrawn natural resource.Cities and Biodiversity: Nature in tight spaces.ASEAN Heritage Parks and Protected Areas.The Post-2020 Global Biodiversity Framework.Support for Ratification and the Implementation of the Nagoya Protocol on Access and Benefit Sharing in ASEAN Countries.Institutional Strengthening of the Biodiversity Sector in the ASEAN (ISB).Institutional Strengthening of the Biodiversity Sector in the ASEAN (ISB II).Capacity Building Programme on Protected Area Management and Ecotourism: Experiential Learning Programme.Biodiversity Conservation and Management of Protected Areas in ASEAN (BCAMP).ASEAN-Korea Environmental Cooperation Project.ASEAN-China Environmental Cooperation Action Plan II.ASEAN Joint Statement to the CBD COP 15.The Richness of Biodiversity in the ASEAN Region.ASEAN Working Group on Nature Conservation and Biodiversity."The Formation of Large Chambers, With Examples from Laos and Other Countries" (PDF). ↑ Gunung Mulu World Heritage Area, Cave activities. The feeling of agoraphobia experienced by one of the discoverers is referenced in the novel House of Leaves by Mark Z. Its exceptional area is thought to be the result of the stability provided by the structure of the rocks in which it lies, dipping strata forming an anticline flank close to a syncline axis. It was formed by karstic solutional processes. Sarawak Chamber is formed in Melinau Limestone, a reef complex of Upper Eocene to Lower Miocene age. Accompanied visits can be arranged by the national Park. This long passage has a roof up to 60 metres (200 ft) high, and may require some swimming and a traverse along a ledge. To reach Sarawak Chamber, one must follow a river upstream from the cave entrance. Its volume and area were checked by laser scanning in 2011 and were found to be 9,579,205 cubic metres (338,286,400 cu ft) and 164,459 square metres (1,770,220 sq ft) respectively. Later named Sarawak Chamber, it measures 600 metres (2,000 ft) long, 435 metres (1,427 ft) wide and a maximum of 115 metres (377 ft) high, and was estimated as three times the size of the Big Room in Carlsbad Caverns National Park, New Mexico, then thought to be the largest underground chamber. The story of how it was discovered is told in the books Underground Worlds and Giant Caves of Borneo. The chamber was discovered by three British cavers, Andy Eavis, Dave Checkley and Tony White, in January 1981 during the Mulu'80 Expedition.
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