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19 results for “Caving rock”
Bhiwkund, Maharashtra, India. Main cave, rock inscription.
<p>Bhiwkund, Maharashtra, India. Main cave, rock inscription, documented 2018.</p>
Integrating ZooMS and zooarchaeology: new data from the Uluzzian levels of Uluzzo C Rock Shelter, Roccia San Sebastiano cave and Riparo del Broion
<p>ZooMS spectra of Riparo del Broion, Roccia San Sebastiano cave and Uluzzo C Rock Shelter.</p>
Early Buddhist rock-cut monasteries of the Western Ghats: Caves and Sculptures
<p>csv files containing basic information on early Buddhist rock-cut monasteries in the Western Ghats and Konkan coast regions of India. Only the caves cut between second century BCE and the early fifth century CE are included: from the earliest period of cutting up until just prior to the introduction of the Buddha image. Data featured are geographical groupings of caves alongside the number of caves and sculptures with descriptions. </p>
Bhiwkund, Maharashtra, India. Main cave, rock inscription.
<p>Bhiwkund, Maharashtra, India. Main cave, rock inscription, documented 03/2018.</p>
FIGURE. Four rupicolous taxa characteristic of the Sierra de las Nieves National Park: A. Centaurea clementei (vertical sunny cliffs in the Tajos de Añicle); B. Saxifraga globulifera (shady rocks in the Peñón de Ronda peak); C. Hieracium baeticum (rocky places in the Puerto de los Valientes mountain pass); D. Sarcocapnos baetica (overhanging cliffs in Cueva del Agua cave). (Photos by authors). in Vascular flora of the Sierra de las Nieves National Park and its surroundings (Andalusia, Spain)
FIGURE. Four rupicolous taxa characteristic of the Sierra de las Nieves National Park: A. Centaurea clementei (vertical sunny cliffs in the Tajos de Añicle); B. Saxifraga globulifera (shady rocks in the Peñón de Ronda peak); C. Hieracium baeticum (rocky places in the Puerto de los Valientes mountain pass); D. Sarcocapnos baetica (overhanging cliffs in Cueva del Agua cave). (Photos by authors).
Physical simulation of the influence of the original rock strength on the compaction characteristics of caving rock in longwall goaf
The compaction characteristics of broken rock in caving zone have a significant impact on the movement law of overburden and the prediction of surface subsidence. The mechanical properties of broken rock are clearly affected by the original rock strength of the roof. In this paper, the compaction mechanical behaviour of broken loose rock masses with different original rock strengths is studied by model testing. The results show that (1) the greater the original rock strength of broken rock is, the shorter the initial compaction stage, the earlier the transition compaction stage and stable compaction stage, and the lower the degree of compaction. (2) The initial deformation modulus and ultimate axial strain have a linear relationship with the original rock strength of broken rock. (3) Under different axial pressures, the deformation modulus increases with increasing original rock strength of the broken rock. The tangent modulus and axial stress change approximately linearly, the secant modulus and stress change linearly, and the tangent modulus and secant modulus have an exponential/hyperbolic relationship with strain.
Exterior Rock Art Panel, Escoural Cave, Portugal
On the fortified settlement of the Chalcolithic, above the Escoural cave, exists an outdoor rock art sanctuary. When, at the end of the Neolithic, the Cave was closed, its space began to be inhabited by communities of the Chalcolithic (2,000 BC), building a fortified settlement, as well as a megalithic dome of false dome, situated at a distance of about 600 meters, characterized by circular chamber, corridor and lobby for access to its interior. This is one of the panels of the rock art sanctuary. Source: Objaverse 1.0 / Sketchfab
Exterior Rock Art Panel, Escoural Cave, Portugal
On the fortified settlement of the Chalcolithic, above the Escoural cave, exists an outdoor rock art sanctuary. When, at the end of the Neolithic, the Cave was closed, its space began to be inhabited by communities of the Chalcolithic (2,000 BC), building a fortified settlement, as well as a megalithic dome of false dome, situated at a distance of about 600 meters, characterized by circular chamber, corridor and lobby for access to its interior. This is one of the panels of the rock art sanctuary. Source: Objaverse 1.0 / Sketchfab
Physical simulation of the influence of the original rock strength on the compaction characteristics of caving rock in longwall goaf
Open the record for dataset details and reuse information.
Data from: A multifactor coupling prediction model for the failure depth of floor rocks in fully mechanized caving mining: a numerical and in situ study
To study the mining-induced failure depth of floor rocks in a fully-mechanized mining caving field affected by different coal seam pitches, mining face lengths, burial depths and aquifer water pressures, multifactor coupled orthogonal numerical tests on the failure depth of floor rocks were conducted. The numerical results show that the failure depth of floor rocks increases with increasing mining face length, coal seam pitch and burial depth. According to the relationship between failure depth and these impact factors, a multifactor coupled prediction model for the failure depth of floor rocks was established. In addition, the in-situ measurement of the failure depth of floor rocks in the Yitang Coal Mine in Huoxi coal field in Shanxi Province, China, was performed, and the in-situ failure depths of floor rocks in the 100502 (80 m) and 100502 (180 m) mining faces were approximately 12.50~14.65 m and 17.50~19.20 m, in good agreement with the results of the multifactor prediction model. Furthermore, the sensitivity of each impact factor in the prediction model of the floor failure depth was further analysed by F-test and range analysis, and the impact order of studied factors on the floor failure depth is coal seam pitch>mining face length>burial depth>aquifer water pressure.
Effect of Earth-Air Movement on Water Transport in the Rock Surrounding Cave B113 in the Mogao Grottoes
<p>data</p>
Data from: A multifactor coupling prediction model for the failure depth of floor rocks in fully mechanized caving mining: a numerical and in situ study
Open the record for dataset details and reuse information.
Escoural Cave Rock Art Painting Panel 23 to 26
Discovered on an April afternoon in 1963, after an explosion of a quarry, the Escoural Cave proved to be an unavoidable site for the history of archeology in Portugal. What the cavel represents today transcends its tourist value, and assumes itself as an international reference for Paleolithic art as the westernmost point of Europe with such artistic representations of Prehistory. The cave art of the Escoural Cave fits in chronologically between 20,000 and 18,000 years a. C. In addition to the engravings, paintings depicting various figures from aurochs to equines as well as geometrical are also known. This is the 3D model of motifs 23 to 26, depicting several bovines, a hybrid figure as well as several undetermined strokes. This is one of the main panels in the Escoural Cave, occupying a central spot inside this natural cavity. Source: Objaverse 1.0 / Sketchfab
Escoural Cave Rock Art Engraving 1 and 2
Discovered on an April afternoon in 1963, after an explosion of a quarry, the Escoural Cave proved to be an unavoidable site for the history of archeology in Portugal. What the cavel represents today transcends its tourist value, and assumes itself as an international reference for Paleolithic art as the westernmost point of Europe with such artistic representations of Prehistory. The cave art of the Escoural Cave fits in chronologically between 20,000 and 18,000 years a. C. In addition to the engravings, paintings depicting various figures from aurochs to equines as well as geometrical are also known. This is the 3D of motifs 1 and 2. Both are engravings: the first is a non figurative engraving; the second is a schematic representation of a bovine. Source: Objaverse 1.0 / Sketchfab
Escoural Cave Rock Art Engraving 21
Discovered on an April afternoon in 1963, after an explosion of a quarry, the Escoural Cave proved to be an unavoidable site for the history of archeology in Portugal. What the cavel represents today transcends its tourist value, and assumes itself as an international reference for Paleolithic art as the westernmost point of Europe with such artistic representations of Prehistory. The cave art of the Escoural Cave fits in chronologically between 20,000 and 18,000 years a. C. In addition to the engravings, paintings depicting various figures from aurochs to equines as well as geometrical are also known. This is the 3D model of the engraving number 21, representing a hut with several strokes converging on top. Source: Objaverse 1.0 / Sketchfab
Escoural Cave Rock Art Engraving number 63
Discovered on an April afternoon in 1963, after an explosion of a quarry, the Escoural Cave proved to be an unavoidable site for the history of archeology in Portugal. What the cavel represents today transcends its tourist value, and assumes itself as an international reference for Paleolithic art as the westernmost point of Europe with such artistic representations of Prehistory. The cave art of the Escoural Cave fits in chronologically between 20,000 and 18,000 years a. C. In addition to the engravings, paintings depicting various figures from aurochs to equines as well as geometrical are also known. This is the 3D model of engraving number 63, representing a large set of geometrical crosslinked lines or reticular motifs. Source: Objaverse 1.0 / Sketchfab
Exterior Rock Art Panel, Escoural Cave, Portugal
On the fortified settlement of the Chalcolithic, above the Escoural cave, exists an outdoor rock art sanctuary. When, at the end of the Neolithic, the Cave was closed, its space began to be inhabited by communities of the Chalcolithic (2,000 BC), building a fortified settlement, as well as a megalithic dome of false dome, situated at a distance of about 600 meters, characterized by circular chamber, corridor and lobby for access to its interior. This is one of the panels of the rock art sanctuary. Source: Objaverse 1.0 / Sketchfab
Low Poly Rock Cave
Low poly rock cave made with 3dMax Source: Objaverse 1.0 / Sketchfab
Exterior Rock Art Panel, Escoural Cave, Portugal
On the fortified settlement of the Chalcolithic, above the Escoural cave, exists an outdoor rock art sanctuary. When, at the end of the Neolithic, the Cave was closed, its space began to be inhabited by communities of the Chalcolithic (2,000 BC), building a fortified settlement, as well as a megalithic dome of false dome, situated at a distance of about 600 meters, characterized by circular chamber, corridor and lobby for access to its interior. This is one of the panels of the rock art sanctuary. Source: Objaverse 1.0 / Sketchfab
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