Evaporite karst in Sicily
Abstract Karst areas are distributed over most of Sicily. The most widespread karst rocks are carbonates, particularly limestones, but karst phenomena can also be seen in evaporites and particularly in salt mines. This report provides an overview of evaporite karst in Sicily, along with a “case hist...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Liguori, V. [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2007 |
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| Systematik: |
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| Anmerkung: |
© Springer-Verlag 2007 |
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| Übergeordnetes Werk: |
Enthalten in: Environmental geology - Springer-Verlag, 1975, 53(2007), 5 vom: 14. Apr., Seite 975-980 |
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| Übergeordnetes Werk: |
volume:53 ; year:2007 ; number:5 ; day:14 ; month:04 ; pages:975-980 |
| Links: |
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| DOI / URN: |
10.1007/s00254-007-0723-9 |
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| Katalog-ID: |
OLC2074412479 |
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| 520 | |a Abstract Karst areas are distributed over most of Sicily. The most widespread karst rocks are carbonates, particularly limestones, but karst phenomena can also be seen in evaporites and particularly in salt mines. This report provides an overview of evaporite karst in Sicily, along with a “case history” that shows some of the evaporite karst risks to the environment. In the centre and south of Sicily, a thick sequence of Messinian evaporite rocks are subject to dissolution from meteoric and formation waters. In areas where potassium salts and rock salts are being mined, some geomorphologic changes result from the drilling of boreholes and the collapse of underground mines, thus lowering or collapsing the land surface. An example is the old salt mine “Muti-Coffari”, situated in the commune of Cammarata, where there is a modification of the surface flow of the River Platani. Meteoric waters and runoff flow down through a borehole, enter the underground mine cavity and dissolve the salts, and then the resulting brine flows into a branch of the river, making it salty. Field investigations showed the presence of salt along the edges and on the bed of the stream where it comes out of the cave. Therefore, interventions for risk mitigation are necessary since the old mine constitutes a serious danger for damage or collapse of nearby infrastructures, and can lead to degradation of the river ecosystem and the natural environment. | ||
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| 650 | 4 | |a Evaporite karst | |
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10.1007/s00254-007-0723-9 doi (DE-627)OLC2074412479 (DE-He213)s00254-007-0723-9-p DE-627 ger DE-627 rakwb eng 330 550 VZ 550 VZ 13 ssgn TE 3140 VZ rvk Liguori, V. verfasserin aut Evaporite karst in Sicily 2007 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2007 Abstract Karst areas are distributed over most of Sicily. The most widespread karst rocks are carbonates, particularly limestones, but karst phenomena can also be seen in evaporites and particularly in salt mines. This report provides an overview of evaporite karst in Sicily, along with a “case history” that shows some of the evaporite karst risks to the environment. In the centre and south of Sicily, a thick sequence of Messinian evaporite rocks are subject to dissolution from meteoric and formation waters. In areas where potassium salts and rock salts are being mined, some geomorphologic changes result from the drilling of boreholes and the collapse of underground mines, thus lowering or collapsing the land surface. An example is the old salt mine “Muti-Coffari”, situated in the commune of Cammarata, where there is a modification of the surface flow of the River Platani. Meteoric waters and runoff flow down through a borehole, enter the underground mine cavity and dissolve the salts, and then the resulting brine flows into a branch of the river, making it salty. Field investigations showed the presence of salt along the edges and on the bed of the stream where it comes out of the cave. Therefore, interventions for risk mitigation are necessary since the old mine constitutes a serious danger for damage or collapse of nearby infrastructures, and can lead to degradation of the river ecosystem and the natural environment. Karst phenomena Evaporite karst Salt mining Manno, G. aut Mortellaro, D. aut Enthalten in Environmental geology Springer-Verlag, 1975 53(2007), 5 vom: 14. Apr., Seite 975-980 (DE-627)129421634 (DE-600)190352-4 (DE-576)014797453 0943-0105 nnns volume:53 year:2007 number:5 day:14 month:04 pages:975-980 https://doi.org/10.1007/s00254-007-0723-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_267 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4277 GBV_ILN_4309 TE 3140 AR 53 2007 5 14 04 975-980 |
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10.1007/s00254-007-0723-9 doi (DE-627)OLC2074412479 (DE-He213)s00254-007-0723-9-p DE-627 ger DE-627 rakwb eng 330 550 VZ 550 VZ 13 ssgn TE 3140 VZ rvk Liguori, V. verfasserin aut Evaporite karst in Sicily 2007 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2007 Abstract Karst areas are distributed over most of Sicily. The most widespread karst rocks are carbonates, particularly limestones, but karst phenomena can also be seen in evaporites and particularly in salt mines. This report provides an overview of evaporite karst in Sicily, along with a “case history” that shows some of the evaporite karst risks to the environment. In the centre and south of Sicily, a thick sequence of Messinian evaporite rocks are subject to dissolution from meteoric and formation waters. In areas where potassium salts and rock salts are being mined, some geomorphologic changes result from the drilling of boreholes and the collapse of underground mines, thus lowering or collapsing the land surface. An example is the old salt mine “Muti-Coffari”, situated in the commune of Cammarata, where there is a modification of the surface flow of the River Platani. Meteoric waters and runoff flow down through a borehole, enter the underground mine cavity and dissolve the salts, and then the resulting brine flows into a branch of the river, making it salty. Field investigations showed the presence of salt along the edges and on the bed of the stream where it comes out of the cave. Therefore, interventions for risk mitigation are necessary since the old mine constitutes a serious danger for damage or collapse of nearby infrastructures, and can lead to degradation of the river ecosystem and the natural environment. Karst phenomena Evaporite karst Salt mining Manno, G. aut Mortellaro, D. aut Enthalten in Environmental geology Springer-Verlag, 1975 53(2007), 5 vom: 14. Apr., Seite 975-980 (DE-627)129421634 (DE-600)190352-4 (DE-576)014797453 0943-0105 nnns volume:53 year:2007 number:5 day:14 month:04 pages:975-980 https://doi.org/10.1007/s00254-007-0723-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_267 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4277 GBV_ILN_4309 TE 3140 AR 53 2007 5 14 04 975-980 |
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10.1007/s00254-007-0723-9 doi (DE-627)OLC2074412479 (DE-He213)s00254-007-0723-9-p DE-627 ger DE-627 rakwb eng 330 550 VZ 550 VZ 13 ssgn TE 3140 VZ rvk Liguori, V. verfasserin aut Evaporite karst in Sicily 2007 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2007 Abstract Karst areas are distributed over most of Sicily. The most widespread karst rocks are carbonates, particularly limestones, but karst phenomena can also be seen in evaporites and particularly in salt mines. This report provides an overview of evaporite karst in Sicily, along with a “case history” that shows some of the evaporite karst risks to the environment. In the centre and south of Sicily, a thick sequence of Messinian evaporite rocks are subject to dissolution from meteoric and formation waters. In areas where potassium salts and rock salts are being mined, some geomorphologic changes result from the drilling of boreholes and the collapse of underground mines, thus lowering or collapsing the land surface. An example is the old salt mine “Muti-Coffari”, situated in the commune of Cammarata, where there is a modification of the surface flow of the River Platani. Meteoric waters and runoff flow down through a borehole, enter the underground mine cavity and dissolve the salts, and then the resulting brine flows into a branch of the river, making it salty. Field investigations showed the presence of salt along the edges and on the bed of the stream where it comes out of the cave. Therefore, interventions for risk mitigation are necessary since the old mine constitutes a serious danger for damage or collapse of nearby infrastructures, and can lead to degradation of the river ecosystem and the natural environment. Karst phenomena Evaporite karst Salt mining Manno, G. aut Mortellaro, D. aut Enthalten in Environmental geology Springer-Verlag, 1975 53(2007), 5 vom: 14. Apr., Seite 975-980 (DE-627)129421634 (DE-600)190352-4 (DE-576)014797453 0943-0105 nnns volume:53 year:2007 number:5 day:14 month:04 pages:975-980 https://doi.org/10.1007/s00254-007-0723-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_267 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4277 GBV_ILN_4309 TE 3140 AR 53 2007 5 14 04 975-980 |
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10.1007/s00254-007-0723-9 doi (DE-627)OLC2074412479 (DE-He213)s00254-007-0723-9-p DE-627 ger DE-627 rakwb eng 330 550 VZ 550 VZ 13 ssgn TE 3140 VZ rvk Liguori, V. verfasserin aut Evaporite karst in Sicily 2007 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2007 Abstract Karst areas are distributed over most of Sicily. The most widespread karst rocks are carbonates, particularly limestones, but karst phenomena can also be seen in evaporites and particularly in salt mines. This report provides an overview of evaporite karst in Sicily, along with a “case history” that shows some of the evaporite karst risks to the environment. In the centre and south of Sicily, a thick sequence of Messinian evaporite rocks are subject to dissolution from meteoric and formation waters. In areas where potassium salts and rock salts are being mined, some geomorphologic changes result from the drilling of boreholes and the collapse of underground mines, thus lowering or collapsing the land surface. An example is the old salt mine “Muti-Coffari”, situated in the commune of Cammarata, where there is a modification of the surface flow of the River Platani. Meteoric waters and runoff flow down through a borehole, enter the underground mine cavity and dissolve the salts, and then the resulting brine flows into a branch of the river, making it salty. Field investigations showed the presence of salt along the edges and on the bed of the stream where it comes out of the cave. Therefore, interventions for risk mitigation are necessary since the old mine constitutes a serious danger for damage or collapse of nearby infrastructures, and can lead to degradation of the river ecosystem and the natural environment. Karst phenomena Evaporite karst Salt mining Manno, G. aut Mortellaro, D. aut Enthalten in Environmental geology Springer-Verlag, 1975 53(2007), 5 vom: 14. Apr., Seite 975-980 (DE-627)129421634 (DE-600)190352-4 (DE-576)014797453 0943-0105 nnns volume:53 year:2007 number:5 day:14 month:04 pages:975-980 https://doi.org/10.1007/s00254-007-0723-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_267 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4277 GBV_ILN_4309 TE 3140 AR 53 2007 5 14 04 975-980 |
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10.1007/s00254-007-0723-9 doi (DE-627)OLC2074412479 (DE-He213)s00254-007-0723-9-p DE-627 ger DE-627 rakwb eng 330 550 VZ 550 VZ 13 ssgn TE 3140 VZ rvk Liguori, V. verfasserin aut Evaporite karst in Sicily 2007 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 2007 Abstract Karst areas are distributed over most of Sicily. The most widespread karst rocks are carbonates, particularly limestones, but karst phenomena can also be seen in evaporites and particularly in salt mines. This report provides an overview of evaporite karst in Sicily, along with a “case history” that shows some of the evaporite karst risks to the environment. In the centre and south of Sicily, a thick sequence of Messinian evaporite rocks are subject to dissolution from meteoric and formation waters. In areas where potassium salts and rock salts are being mined, some geomorphologic changes result from the drilling of boreholes and the collapse of underground mines, thus lowering or collapsing the land surface. An example is the old salt mine “Muti-Coffari”, situated in the commune of Cammarata, where there is a modification of the surface flow of the River Platani. Meteoric waters and runoff flow down through a borehole, enter the underground mine cavity and dissolve the salts, and then the resulting brine flows into a branch of the river, making it salty. Field investigations showed the presence of salt along the edges and on the bed of the stream where it comes out of the cave. Therefore, interventions for risk mitigation are necessary since the old mine constitutes a serious danger for damage or collapse of nearby infrastructures, and can lead to degradation of the river ecosystem and the natural environment. Karst phenomena Evaporite karst Salt mining Manno, G. aut Mortellaro, D. aut Enthalten in Environmental geology Springer-Verlag, 1975 53(2007), 5 vom: 14. Apr., Seite 975-980 (DE-627)129421634 (DE-600)190352-4 (DE-576)014797453 0943-0105 nnns volume:53 year:2007 number:5 day:14 month:04 pages:975-980 https://doi.org/10.1007/s00254-007-0723-9 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_30 GBV_ILN_40 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_267 GBV_ILN_2006 GBV_ILN_2010 GBV_ILN_2014 GBV_ILN_2018 GBV_ILN_2027 GBV_ILN_4012 GBV_ILN_4277 GBV_ILN_4309 TE 3140 AR 53 2007 5 14 04 975-980 |
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Abstract Karst areas are distributed over most of Sicily. The most widespread karst rocks are carbonates, particularly limestones, but karst phenomena can also be seen in evaporites and particularly in salt mines. This report provides an overview of evaporite karst in Sicily, along with a “case history” that shows some of the evaporite karst risks to the environment. In the centre and south of Sicily, a thick sequence of Messinian evaporite rocks are subject to dissolution from meteoric and formation waters. In areas where potassium salts and rock salts are being mined, some geomorphologic changes result from the drilling of boreholes and the collapse of underground mines, thus lowering or collapsing the land surface. An example is the old salt mine “Muti-Coffari”, situated in the commune of Cammarata, where there is a modification of the surface flow of the River Platani. Meteoric waters and runoff flow down through a borehole, enter the underground mine cavity and dissolve the salts, and then the resulting brine flows into a branch of the river, making it salty. Field investigations showed the presence of salt along the edges and on the bed of the stream where it comes out of the cave. Therefore, interventions for risk mitigation are necessary since the old mine constitutes a serious danger for damage or collapse of nearby infrastructures, and can lead to degradation of the river ecosystem and the natural environment. © Springer-Verlag 2007 |
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Abstract Karst areas are distributed over most of Sicily. The most widespread karst rocks are carbonates, particularly limestones, but karst phenomena can also be seen in evaporites and particularly in salt mines. This report provides an overview of evaporite karst in Sicily, along with a “case history” that shows some of the evaporite karst risks to the environment. In the centre and south of Sicily, a thick sequence of Messinian evaporite rocks are subject to dissolution from meteoric and formation waters. In areas where potassium salts and rock salts are being mined, some geomorphologic changes result from the drilling of boreholes and the collapse of underground mines, thus lowering or collapsing the land surface. An example is the old salt mine “Muti-Coffari”, situated in the commune of Cammarata, where there is a modification of the surface flow of the River Platani. Meteoric waters and runoff flow down through a borehole, enter the underground mine cavity and dissolve the salts, and then the resulting brine flows into a branch of the river, making it salty. Field investigations showed the presence of salt along the edges and on the bed of the stream where it comes out of the cave. Therefore, interventions for risk mitigation are necessary since the old mine constitutes a serious danger for damage or collapse of nearby infrastructures, and can lead to degradation of the river ecosystem and the natural environment. © Springer-Verlag 2007 |
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Abstract Karst areas are distributed over most of Sicily. The most widespread karst rocks are carbonates, particularly limestones, but karst phenomena can also be seen in evaporites and particularly in salt mines. This report provides an overview of evaporite karst in Sicily, along with a “case history” that shows some of the evaporite karst risks to the environment. In the centre and south of Sicily, a thick sequence of Messinian evaporite rocks are subject to dissolution from meteoric and formation waters. In areas where potassium salts and rock salts are being mined, some geomorphologic changes result from the drilling of boreholes and the collapse of underground mines, thus lowering or collapsing the land surface. An example is the old salt mine “Muti-Coffari”, situated in the commune of Cammarata, where there is a modification of the surface flow of the River Platani. Meteoric waters and runoff flow down through a borehole, enter the underground mine cavity and dissolve the salts, and then the resulting brine flows into a branch of the river, making it salty. Field investigations showed the presence of salt along the edges and on the bed of the stream where it comes out of the cave. Therefore, interventions for risk mitigation are necessary since the old mine constitutes a serious danger for damage or collapse of nearby infrastructures, and can lead to degradation of the river ecosystem and the natural environment. © Springer-Verlag 2007 |
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