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English Crater

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Northern wall of English's Crater (~800 m across) seen from Perche's Mountain in November 2005. Newly growing (since August 2005) dome is enshrouded by steam to the left. Other features visible are remnants of the earlier dome and talus following the giant dome collapse of July 2003. These deposits were largely produced by the 1999–2003 period of dome growth. Boundary between core lava and talus on western side of this 1999–2003 dome is visible, emphasized by dashed yellow line. This trace is projected as black dashed line onto north crater wall in Figure 1. Inset map shows north and east flanks of Soufrière Hills volcano with the dome inside English's Crater. Contour interval is 100 m.
Published: 01 June 2009
Figure 2. Northern wall of English's Crater (~800 m across) seen from Perche's Mountain in November 2005. Newly growing (since August 2005) dome is enshrouded by steam to the left. Other features visible are remnants of the earlier dome and talus following the giant dome collapse of July 2003
Series: Geological Society, London, Memoirs
Published: 01 January 2002
DOI: 10.1144/GSL.MEM.2002.021.01.16
EISBN: 9781862393967
... Abstract During the 1995 to 1998 phase of dome growth at Soufrière Hills Volcano on Montserrat, we documented instability of the steep southern rim of English’s Crater, known as Galway’s Wall. The horseshoe-shaped English’s Crater provided good evidence for previous sector collapses...
Journal Article
Published: 01 August 2007
Quarterly Journal of Engineering Geology and Hydrogeology (2007) 40 (3): 267–292.
... being dormant for about 400 years. The most dramatic, distinct ‘landslides’ occur on the extrusive, expanding, andesitic lava dome within English Crater. Falls, topples and slides are caused by the over-steepening of the dome followed by its gravitational collapse. On occasions, these failures generate...
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First thumbnail for: Engineering geology of landslides on the volcanic ...
Second thumbnail for: Engineering geology of landslides on the volcanic ...
Third thumbnail for: Engineering geology of landslides on the volcanic ...
Journal Article
Published: 01 January 2004
Journal of the Geological Society (2004) 161 (1): 147–160.
... centre. During the current eruption of Soufrière Hills volcano (1995–2002) more than half of the lava erupted was transported into the sea. Flank collapses occurred several times during this stage, such as the English's Crater event ( c . 4000 years ago) or the Boxing Day event during the current...
FIGURES
First thumbnail for: Geomorphological evolution of Montserrat (West Ind...
Second thumbnail for: Geomorphological evolution of Montserrat (West Ind...
Third thumbnail for: Geomorphological evolution of Montserrat (West Ind...
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Propagators of Estonian crater theme in the English-language world. A. Ivan Reinwald (on the right) and Clyde Fisher, active educator and traveler from the American Museum of Natural History (https://en.wikipedia.org/wiki/George_Clyde_Fisher), on the floor of the Kaali crater no. 2 in 1936 (from Reinwald, 1938b). B. Leonard James Spencer (1870–1959), a renowned British mineralogist, Keeper of Minerals in the British Museum Natural History, and Reinwald’s collaborator (from Tilley, 1961).
Published: 29 August 2018
Fig. 8 Propagators of Estonian crater theme in the English-language world. A. Ivan Reinwald (on the right) and Clyde Fisher, active educator and traveler from the American Museum of Natural History ( https://en.wikipedia.org/wiki/George_Clyde_Fisher ), on the floor of the Kaali crater no. 2
Series: Geological Society, London, Special Publications
Published: 01 January 2006
DOI: 10.1144/GSL.SP.2006.256.01.12
EISBN: 9781862395046
... English mineralogist James Smithson, who collected meteorites. Early work included study of Smithson’s meteorites by American mineralogist J. Lawrence Smith and acquisition of the iconic Tucson Ring meteorite. The collection was shaped by geochemist F.W. Clarke and G.P. Merrill, its first meteorite...
Journal Article
Published: 01 August 1974
Journal of the Geological Society (1974) 130 (4): 341–366.
... of pyroclastics. The central nucleus consists of four hills (Gage's, Chance's, Galway's and Perche's) separated by deep valleys and truncated by a dome-filled crater, Volcanic geology and petrology of Montserrat 347 English's Crater. Exposures of solid lava are rare on the hills, but the hills are littered...
Journal Article
Journal: Geology
Published: 01 June 2009
Geology (2009) 37 (6): 551–554.
...Figure 2. Northern wall of English's Crater (~800 m across) seen from Perche's Mountain in November 2005. Newly growing (since August 2005) dome is enshrouded by steam to the left. Other features visible are remnants of the earlier dome and talus following the giant dome collapse of July 2003...
FIGURES
First thumbnail for: Clastic and core lava components of a silicic lava...
Second thumbnail for: Clastic and core lava components of a silicic lava...
Third thumbnail for: Clastic and core lava components of a silicic lava...
Image
Spines of extrusive viscous lava topple from the summit of the andesitic dome, before sliding or bouncing along the flanks of the dome and filling the inner walls of English Crater (photograph taken in 1996; the walls of the crater have now been breached). The former capital town, Plymouth, is at the top right of the photograph on the Caribbean (west) coastline. This has now been buried by flows that were generated from the lava dome.
Published: 01 August 2007
Fig. 5 Spines of extrusive viscous lava topple from the summit of the andesitic dome, before sliding or bouncing along the flanks of the dome and filling the inner walls of English Crater (photograph taken in 1996; the walls of the crater have now been breached). The former capital town, Plymouth
Journal Article
Published: 01 January 2007
The Journal of Geology (2007) 115 (1): 115–127.
... and southwest. A fifth dome—Castle Peak, which was contained in the steep-walled elliptical sector collapse scar of English’s Crater—has now been overtopped and buried by the new domes (1995–present; fig. 1 ). The stratigraphy of the SSH is dominated by the presence of scoriaceous lapilli and ash fall...
FIGURES
First thumbnail for: Prehistoric Stratigraphy of the Soufrière Hills–So...
Second thumbnail for: Prehistoric Stratigraphy of the Soufrière Hills–So...
Third thumbnail for: Prehistoric Stratigraphy of the Soufrière Hills–So...
Journal Article
Published: 01 August 1988
Journal of the Geological Society (1988) 145 (4): 541–551.
..., Perche's Mt and Castle Peak. The last of these occupies a crater, English's Crater, which is 1 km in diameter with walls 100-150m high but open to the ENE. These domes are from 800-1200m in diameter and up to 500 m high forming slopes of 32"-22". Surrounding them is an apron of fragmental deposits...
Image
Vertical air photograph showing different-shaped areas of subsidence on the outer wall of English Crater, accompanied by rock falls (large boulders), on the inner walls of the steep-sided subsidence depressions (these are now covered by ash-fall and pyroclastic deposits). The trees stumps provide some indication of the size of these features.
Published: 01 August 2007
Fig. 9 Vertical air photograph showing different-shaped areas of subsidence on the outer wall of English Crater, accompanied by rock falls (large boulders), on the inner walls of the steep-sided subsidence depressions (these are now covered by ash-fall and pyroclastic deposits). The trees stumps
Journal Article
Journal: AAPG Bulletin
Published: 15 October 2020
AAPG Bulletin (2020) 104 (10): 2099–2123.
... are mainly tectonic fractures, in addition to some shrinkage, dissolution, and cryptoexplosive fractures. Analyzing various sources of data revealed that fractures are generally better developed in the rhyolites and trachytes of the crater and near-crater group. Also, tectonic fractures are developed...
FIGURES
First thumbnail for: Natural fractures in tight gas volcanic reservoirs...
Second thumbnail for: Natural fractures in tight gas volcanic reservoirs...
Third thumbnail for: Natural fractures in tight gas volcanic reservoirs...
Journal Article
Published: 01 October 1998
Earth Sciences History (1998) 17 (2): 174–189.
... did not hesitate to do so.” As the work of another meteoritic pioneer, the English mineralogist Leonard James Spencer (1870–1959) shows, the legacy of the First World War similarly helped in the understanding of meteor craters. Spencer specifically compared his meteor craters with mine and shell...
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First thumbnail for: ‘NO IMPACT’: RENÉ GALLANT (1906–1985) AND HIS BOOK...
Second thumbnail for: ‘NO IMPACT’: RENÉ GALLANT (1906–1985) AND HIS BOOK...
Third thumbnail for: ‘NO IMPACT’: RENÉ GALLANT (1906–1985) AND HIS BOOK...
Journal Article
Journal: Geology
Published: 11 July 2023
Geology (2023) 51 (9): 870–874.
... gravity and remote-sensing studies proposed that the porphyroclastic lava crater is located near the north of the Xiangshan peak ( Chen et al., 2012 ; Qiu et al., 2001 ). The rhyodacite crater is located near Shutang village, as conjectured based on magnetic susceptibility anisotropy measurements ( Li et...
FIGURES
First thumbnail for: Electrical image of magmatic system beneath the Xi...
Second thumbnail for: Electrical image of magmatic system beneath the Xi...
Third thumbnail for: Electrical image of magmatic system beneath the Xi...
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(Left) Map of Montserrat showing the approximate location of the Montserrat Volcano Observatory (MVO), Belham valley bridge and the Soufrière Hills volcano. Map also shows volcanic and volcaniclastic deposits (green, pyroclastic flow deposits; brown, pyroclastic surge deposits; blue, debris avalanche deposits; purple, lava dome). (Right) Example of Montserrat volcano risk map, for December 1999, showing the location of the active, expanding, extrusive, lava dome in English Crater (reproduced with kind permission of MVO/NERC, in Donnelly et al. 2006).
Published: 01 August 2007
, debris avalanche deposits; purple, lava dome). (Right) Example of Montserrat volcano risk map, for December 1999, showing the location of the active, expanding, extrusive, lava dome in English Crater (reproduced with kind permission of MVO/NERC, in Donnelly et al . 2006 ).
Journal Article
Published: 01 April 2020
Earth Sciences History (2020) 39 (1): 146–159.
... in leaves underground or above a steam crack at Sulphur Banks, Kīlauea Iki, and the Nāpau Crater Trail. Early Hawaiians bathed in the warm waters of Waiwelawela for health. To confirm the presence of volcanic heat, this study used geothermal resource maps by the Hawai‘i Play Fairway project. According...
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First thumbnail for: EARLY HAWAIIANS AND VOLCANIC HEAT
Second thumbnail for: EARLY HAWAIIANS AND VOLCANIC HEAT
Third thumbnail for: EARLY HAWAIIANS AND VOLCANIC HEAT
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 Maps showing spatial relationships between submarine deposits, submarine chutes and flank-collapse structures. Contour interval is 100 m down to 100 m below sea level for (a) and (c), and down to 600 m below sea level for (b), and 20 m below that. The 100 m isolines are annotated. (a) English's Crater flank-collapse structure; (b) submarine slope instabilities or flank-collapse structures of the South Soufrière Hills–Soufrière Hills volcano (see text for the discussion of the two models); (c) submarine slope instabilities off SW Montserrat.
Published: 01 January 2004
. ( a ) English's Crater flank-collapse structure; ( b ) submarine slope instabilities or flank-collapse structures of the South Soufrière Hills–Soufrière Hills volcano (see text for the discussion of the two models); ( c ) submarine slope instabilities off SW Montserrat.
Journal Article
Published: 01 October 2021
Earth Sciences History (2021) 40 (2): 625–628.
... on the German structures, with detailed references and quotes. She argues that the lack of peer review at the time was permissive of this co-existence. By the 1930s, there were published impact interpretations of lunar craters and of Arizona’s ‘Meteor Crater’ (which had other names), although alternative...
Journal Article
Published: 01 October 2024
American Mineralogist (2024) 109 (10): 1819–1833.
... in the submarine Wakamiko Crater (Ryukyu Volcanic Arc) as opposed to commonly observed accessory stibnite in the seafloor hydrothermal deposits. The stibnite dimorph, metastibnite, found here for the first time on the seafloor, appears to always form whenever stibnite is precipitated under submarine hydrothermal...
FIGURES
First thumbnail for: Mineralogical and geochemical facets of the massiv...
Second thumbnail for: Mineralogical and geochemical facets of the massiv...
Third thumbnail for: Mineralogical and geochemical facets of the massiv...