Spatial and temporal variability of a coarse-sand anomaly on a sandy inner shelf, northeastern Gulf of Mexico
Abstract A 10-$ km^{2} $ area of anomalously uniform coarse sand and low relief, in 30 m water depth off Panama City, Florida, USA, exists as a palimpsest hardbottom within the prevailing sand-wave system. Side-scan sonar observations over a ten-year period document the morphologic response of the a...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Fleischer, Peter [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
1996 |
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| Schlagwörter: |
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| Anmerkung: |
© Springer-Verlag 1996 |
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| Übergeordnetes Werk: |
Enthalten in: Geo-marine letters - Springer-Verlag, 1981, 16(1996), 3 vom: Sept., Seite 266-272 |
|---|---|
| Übergeordnetes Werk: |
volume:16 ; year:1996 ; number:3 ; month:09 ; pages:266-272 |
| Links: |
|---|
| DOI / URN: |
10.1007/BF01204519 |
|---|
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OLC2036169023 |
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| 245 | 1 | 0 | |a Spatial and temporal variability of a coarse-sand anomaly on a sandy inner shelf, northeastern Gulf of Mexico |
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| 520 | |a Abstract A 10-$ km^{2} $ area of anomalously uniform coarse sand and low relief, in 30 m water depth off Panama City, Florida, USA, exists as a palimpsest hardbottom within the prevailing sand-wave system. Side-scan sonar observations over a ten-year period document the morphologic response of the anomaly to the bottom—wave—current interaction regime. The anomaly and surrounding sand waves remained fixed during this period. Ripples form within the anomaly in response to seasonal storms and decay during quiescent periods. Hurricane response includes minor realignment of sand waves, formation of megaripples, and deposition of a thin mud layer. | ||
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| 650 | 4 | |a Sonar | |
| 650 | 4 | |a Temporal Variability | |
| 650 | 4 | |a Coarse Sand | |
| 650 | 4 | |a Morphologic Response | |
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| 700 | 1 | |a Fiedler, Hannelore |4 aut | |
| 700 | 1 | |a Stender, Ingo H. |4 aut | |
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10.1007/BF01204519 doi (DE-627)OLC2036169023 (DE-He213)BF01204519-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Fleischer, Peter verfasserin aut Spatial and temporal variability of a coarse-sand anomaly on a sandy inner shelf, northeastern Gulf of Mexico 1996 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1996 Abstract A 10-$ km^{2} $ area of anomalously uniform coarse sand and low relief, in 30 m water depth off Panama City, Florida, USA, exists as a palimpsest hardbottom within the prevailing sand-wave system. Side-scan sonar observations over a ten-year period document the morphologic response of the anomaly to the bottom—wave—current interaction regime. The anomaly and surrounding sand waves remained fixed during this period. Ripples form within the anomaly in response to seasonal storms and decay during quiescent periods. Hurricane response includes minor realignment of sand waves, formation of megaripples, and deposition of a thin mud layer. Water Depth Sonar Temporal Variability Coarse Sand Morphologic Response Sawyer, William B. aut Fiedler, Hannelore aut Stender, Ingo H. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 16(1996), 3 vom: Sept., Seite 266-272 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:16 year:1996 number:3 month:09 pages:266-272 https://doi.org/10.1007/BF01204519 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_600 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4277 AR 16 1996 3 09 266-272 |
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10.1007/BF01204519 doi (DE-627)OLC2036169023 (DE-He213)BF01204519-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Fleischer, Peter verfasserin aut Spatial and temporal variability of a coarse-sand anomaly on a sandy inner shelf, northeastern Gulf of Mexico 1996 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1996 Abstract A 10-$ km^{2} $ area of anomalously uniform coarse sand and low relief, in 30 m water depth off Panama City, Florida, USA, exists as a palimpsest hardbottom within the prevailing sand-wave system. Side-scan sonar observations over a ten-year period document the morphologic response of the anomaly to the bottom—wave—current interaction regime. The anomaly and surrounding sand waves remained fixed during this period. Ripples form within the anomaly in response to seasonal storms and decay during quiescent periods. Hurricane response includes minor realignment of sand waves, formation of megaripples, and deposition of a thin mud layer. Water Depth Sonar Temporal Variability Coarse Sand Morphologic Response Sawyer, William B. aut Fiedler, Hannelore aut Stender, Ingo H. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 16(1996), 3 vom: Sept., Seite 266-272 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:16 year:1996 number:3 month:09 pages:266-272 https://doi.org/10.1007/BF01204519 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_600 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4277 AR 16 1996 3 09 266-272 |
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10.1007/BF01204519 doi (DE-627)OLC2036169023 (DE-He213)BF01204519-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Fleischer, Peter verfasserin aut Spatial and temporal variability of a coarse-sand anomaly on a sandy inner shelf, northeastern Gulf of Mexico 1996 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1996 Abstract A 10-$ km^{2} $ area of anomalously uniform coarse sand and low relief, in 30 m water depth off Panama City, Florida, USA, exists as a palimpsest hardbottom within the prevailing sand-wave system. Side-scan sonar observations over a ten-year period document the morphologic response of the anomaly to the bottom—wave—current interaction regime. The anomaly and surrounding sand waves remained fixed during this period. Ripples form within the anomaly in response to seasonal storms and decay during quiescent periods. Hurricane response includes minor realignment of sand waves, formation of megaripples, and deposition of a thin mud layer. Water Depth Sonar Temporal Variability Coarse Sand Morphologic Response Sawyer, William B. aut Fiedler, Hannelore aut Stender, Ingo H. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 16(1996), 3 vom: Sept., Seite 266-272 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:16 year:1996 number:3 month:09 pages:266-272 https://doi.org/10.1007/BF01204519 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_600 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4277 AR 16 1996 3 09 266-272 |
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10.1007/BF01204519 doi (DE-627)OLC2036169023 (DE-He213)BF01204519-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Fleischer, Peter verfasserin aut Spatial and temporal variability of a coarse-sand anomaly on a sandy inner shelf, northeastern Gulf of Mexico 1996 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1996 Abstract A 10-$ km^{2} $ area of anomalously uniform coarse sand and low relief, in 30 m water depth off Panama City, Florida, USA, exists as a palimpsest hardbottom within the prevailing sand-wave system. Side-scan sonar observations over a ten-year period document the morphologic response of the anomaly to the bottom—wave—current interaction regime. The anomaly and surrounding sand waves remained fixed during this period. Ripples form within the anomaly in response to seasonal storms and decay during quiescent periods. Hurricane response includes minor realignment of sand waves, formation of megaripples, and deposition of a thin mud layer. Water Depth Sonar Temporal Variability Coarse Sand Morphologic Response Sawyer, William B. aut Fiedler, Hannelore aut Stender, Ingo H. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 16(1996), 3 vom: Sept., Seite 266-272 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:16 year:1996 number:3 month:09 pages:266-272 https://doi.org/10.1007/BF01204519 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_600 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4277 AR 16 1996 3 09 266-272 |
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10.1007/BF01204519 doi (DE-627)OLC2036169023 (DE-He213)BF01204519-p DE-627 ger DE-627 rakwb eng 550 VZ 550 VZ 13 ssgn Fleischer, Peter verfasserin aut Spatial and temporal variability of a coarse-sand anomaly on a sandy inner shelf, northeastern Gulf of Mexico 1996 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © Springer-Verlag 1996 Abstract A 10-$ km^{2} $ area of anomalously uniform coarse sand and low relief, in 30 m water depth off Panama City, Florida, USA, exists as a palimpsest hardbottom within the prevailing sand-wave system. Side-scan sonar observations over a ten-year period document the morphologic response of the anomaly to the bottom—wave—current interaction regime. The anomaly and surrounding sand waves remained fixed during this period. Ripples form within the anomaly in response to seasonal storms and decay during quiescent periods. Hurricane response includes minor realignment of sand waves, formation of megaripples, and deposition of a thin mud layer. Water Depth Sonar Temporal Variability Coarse Sand Morphologic Response Sawyer, William B. aut Fiedler, Hannelore aut Stender, Ingo H. aut Enthalten in Geo-marine letters Springer-Verlag, 1981 16(1996), 3 vom: Sept., Seite 266-272 (DE-627)129932140 (DE-600)381526-2 (DE-576)015466973 0276-0460 nnns volume:16 year:1996 number:3 month:09 pages:266-272 https://doi.org/10.1007/BF01204519 lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_11 GBV_ILN_21 GBV_ILN_40 GBV_ILN_62 GBV_ILN_70 GBV_ILN_600 GBV_ILN_612 GBV_ILN_2018 GBV_ILN_4012 GBV_ILN_4277 AR 16 1996 3 09 266-272 |
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spatial and temporal variability of a coarse-sand anomaly on a sandy inner shelf, northeastern gulf of mexico |
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Spatial and temporal variability of a coarse-sand anomaly on a sandy inner shelf, northeastern Gulf of Mexico |
| abstract |
Abstract A 10-$ km^{2} $ area of anomalously uniform coarse sand and low relief, in 30 m water depth off Panama City, Florida, USA, exists as a palimpsest hardbottom within the prevailing sand-wave system. Side-scan sonar observations over a ten-year period document the morphologic response of the anomaly to the bottom—wave—current interaction regime. The anomaly and surrounding sand waves remained fixed during this period. Ripples form within the anomaly in response to seasonal storms and decay during quiescent periods. Hurricane response includes minor realignment of sand waves, formation of megaripples, and deposition of a thin mud layer. © Springer-Verlag 1996 |
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Abstract A 10-$ km^{2} $ area of anomalously uniform coarse sand and low relief, in 30 m water depth off Panama City, Florida, USA, exists as a palimpsest hardbottom within the prevailing sand-wave system. Side-scan sonar observations over a ten-year period document the morphologic response of the anomaly to the bottom—wave—current interaction regime. The anomaly and surrounding sand waves remained fixed during this period. Ripples form within the anomaly in response to seasonal storms and decay during quiescent periods. Hurricane response includes minor realignment of sand waves, formation of megaripples, and deposition of a thin mud layer. © Springer-Verlag 1996 |
| abstract_unstemmed |
Abstract A 10-$ km^{2} $ area of anomalously uniform coarse sand and low relief, in 30 m water depth off Panama City, Florida, USA, exists as a palimpsest hardbottom within the prevailing sand-wave system. Side-scan sonar observations over a ten-year period document the morphologic response of the anomaly to the bottom—wave—current interaction regime. The anomaly and surrounding sand waves remained fixed during this period. Ripples form within the anomaly in response to seasonal storms and decay during quiescent periods. Hurricane response includes minor realignment of sand waves, formation of megaripples, and deposition of a thin mud layer. © Springer-Verlag 1996 |
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Spatial and temporal variability of a coarse-sand anomaly on a sandy inner shelf, northeastern Gulf of Mexico |
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Sawyer, William B. Fiedler, Hannelore Stender, Ingo H. |
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