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- KARST TOPOGRAPHY
• Cockpit Karst is a form of karst in which the residual hills are chiefly hemispheroidal and surround closed, lobed, depressions known as dolines or "cockpits" each of which is drained to the aquifer by one or more sinkholes Disappearing Streams
- Research on Fading Characteristics of Ultrahigh Frequency . . .
The results show that (1) the polarization type and signal frequency have a de nite in uence on the fading fi fl distribution types in the Karst landform; (2) Rice distribution is the optimal and
- Karst map of Southern Ontario, including Manitoulin Island . . .
Inferred Karst - regions of carbonate bedrock units highlighted counties, southwestern Ontario Sinkholes preferentially occur as above and within the Middle Devonian age high-purity dolostones most vulnerable or susceptible to karstification, where direct of the Lucas Formation and less commonly where fossiliferous field observations have not been made by OGS staff or other limestones of the
- PEER-REVIEW ARTICLE - North Carolina State University
Norway spruce (Picea abies Karst ) is one of 36 known spruce species It is one of the most widespread and economically valuable conifers in Europe The complex growth–environment–health status relationship is undergoing fundamental changes, especially in the mountain forests of Central Europe
- Benthic Macroinvertebrate Assemblages in Karst Springs . . .
Abstract: Ecosystems of karst springs are insuficiently studied in Bulgaria This study was focused on bottom macroinvertebrate assemblages from this river type Their taxonomic diversity
- Fungi from Asian Karst formations I. Pestalotiopsis . . .
Introduction Karst topography is a landscape formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum and is characterized by underground drainage systems with sinkholes, dolines and caves (Gorbushina et al 2003) Rainfall and temperatures vary greatly and the formations can be regarded as extreme habitats, especially when soils are sparse The south China Karst
- Primate sightings in Sangkulirang Mangkalihat Karst, East . . .
SUMMARY The Sangkulirang‐Mangkalihat Karst is an area in Kutai Timur and Berau regencies of East Kalimantan province, Indonesia, on the island of Borneo The peninsula is dominated by limestone geology, and it covers an area of over 18,000 square kilometres
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