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Fayetteville Green Lake, New York. 6. The role of turbidity currents in lake sedimentation1
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| Zeitschriftentitel: | Limnology and Oceanography |
|---|---|
| Personen und Körperschaften: | |
| In: | Limnology and Oceanography, 19, 1974, 4, S. 656-664 |
| Format: | E-Article |
| Sprache: | Englisch |
| veröffentlicht: |
Wiley
|
| Schlagwörter: |
| author_facet |
Ludlam, Stuart D. Ludlam, Stuart D. |
|---|---|
| author |
Ludlam, Stuart D. |
| spellingShingle |
Ludlam, Stuart D. Limnology and Oceanography Fayetteville Green Lake, New York. 6. The role of turbidity currents in lake sedimentation1 Aquatic Science Oceanography |
| author_sort |
ludlam, stuart d. |
| spelling |
Ludlam, Stuart D. 0024-3590 1939-5590 Wiley Aquatic Science Oceanography http://dx.doi.org/10.4319/lo.1974.19.4.0656 <jats:p>Turbidity currents are formed in Fayetteville Green Lake by sediment slumping on the sides of the lake basin. Deposition from these currents accounts for about 50% of all sediment accumulation on the floor of the main basin. Rate of sediment loss from the basin sides through the formation of turbidity currents approximately equals nonturbidite sedimentation rates on the gently sloping basin floor. Major turbidity currents arise most frequently where sources of terrestrial sediment are present. Major turbidity currents involve about 200–300 m<jats:sup>3</jats:sup> (dry volume) sediment and extend over about 6 × 10<jats:sup>4</jats:sup> m<jats:sup>2</jats:sup>.</jats:p> Fayetteville Green Lake, New York. 6. The role of turbidity currents in lake sedimentation1 Limnology and Oceanography |
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Fayetteville Green Lake, New York. 6. The role of turbidity currents in lake sedimentation1 |
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Fayetteville Green Lake, New York. 6. The role of turbidity currents in lake sedimentation1 |
| title_full |
Fayetteville Green Lake, New York. 6. The role of turbidity currents in lake sedimentation1 |
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Fayetteville Green Lake, New York. 6. The role of turbidity currents in lake sedimentation1 |
| title_full_unstemmed |
Fayetteville Green Lake, New York. 6. The role of turbidity currents in lake sedimentation1 |
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Fayetteville Green Lake, New York. 6. The role of turbidity currents in lake sedimentation1 |
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fayetteville green lake, new york. 6. the role of turbidity currents in lake sedimentation1 |
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Aquatic Science Oceanography |
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http://dx.doi.org/10.4319/lo.1974.19.4.0656 |
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1974 |
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656-664 |
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<jats:p>Turbidity currents are formed in Fayetteville Green Lake by sediment slumping on the sides of the lake basin. Deposition from these currents accounts for about 50% of all sediment accumulation on the floor of the main basin. Rate of sediment loss from the basin sides through the formation of turbidity currents approximately equals nonturbidite sedimentation rates on the gently sloping basin floor. Major turbidity currents arise most frequently where sources of terrestrial sediment are present. Major turbidity currents involve about 200–300 m<jats:sup>3</jats:sup> (dry volume) sediment and extend over about 6 × 10<jats:sup>4</jats:sup> m<jats:sup>2</jats:sup>.</jats:p> |
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| description | <jats:p>Turbidity currents are formed in Fayetteville Green Lake by sediment slumping on the sides of the lake basin. Deposition from these currents accounts for about 50% of all sediment accumulation on the floor of the main basin. Rate of sediment loss from the basin sides through the formation of turbidity currents approximately equals nonturbidite sedimentation rates on the gently sloping basin floor. Major turbidity currents arise most frequently where sources of terrestrial sediment are present. Major turbidity currents involve about 200–300 m<jats:sup>3</jats:sup> (dry volume) sediment and extend over about 6 × 10<jats:sup>4</jats:sup> m<jats:sup>2</jats:sup>.</jats:p> |
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| imprint | Wiley, 1974 |
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| institution | DE-D275, DE-Bn3, DE-Brt1, DE-Zwi2, DE-D161, DE-Gla1, DE-Zi4, DE-15, DE-Pl11, DE-Rs1, DE-105, DE-14, DE-Ch1, DE-L229 |
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| spelling | Ludlam, Stuart D. 0024-3590 1939-5590 Wiley Aquatic Science Oceanography http://dx.doi.org/10.4319/lo.1974.19.4.0656 <jats:p>Turbidity currents are formed in Fayetteville Green Lake by sediment slumping on the sides of the lake basin. Deposition from these currents accounts for about 50% of all sediment accumulation on the floor of the main basin. Rate of sediment loss from the basin sides through the formation of turbidity currents approximately equals nonturbidite sedimentation rates on the gently sloping basin floor. Major turbidity currents arise most frequently where sources of terrestrial sediment are present. Major turbidity currents involve about 200–300 m<jats:sup>3</jats:sup> (dry volume) sediment and extend over about 6 × 10<jats:sup>4</jats:sup> m<jats:sup>2</jats:sup>.</jats:p> Fayetteville Green Lake, New York. 6. The role of turbidity currents in lake sedimentation1 Limnology and Oceanography |
| spellingShingle | Ludlam, Stuart D., Limnology and Oceanography, Fayetteville Green Lake, New York. 6. The role of turbidity currents in lake sedimentation1, Aquatic Science, Oceanography |
| title | Fayetteville Green Lake, New York. 6. The role of turbidity currents in lake sedimentation1 |
| title_full | Fayetteville Green Lake, New York. 6. The role of turbidity currents in lake sedimentation1 |
| title_fullStr | Fayetteville Green Lake, New York. 6. The role of turbidity currents in lake sedimentation1 |
| title_full_unstemmed | Fayetteville Green Lake, New York. 6. The role of turbidity currents in lake sedimentation1 |
| title_short | Fayetteville Green Lake, New York. 6. The role of turbidity currents in lake sedimentation1 |
| title_sort | fayetteville green lake, new york. 6. the role of turbidity currents in lake sedimentation1 |
| title_unstemmed | Fayetteville Green Lake, New York. 6. The role of turbidity currents in lake sedimentation1 |
| topic | Aquatic Science, Oceanography |
| url | http://dx.doi.org/10.4319/lo.1974.19.4.0656 |