Name: anomaly_Cretaceous_talus
Display Field: Feature
Type: Feature Layer
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Description: Areas along the lower Florida Escarpment with high-positive amplitude response concentrated in valleys between discrete ridges which appear to be slump deposits of carbonates, likely of Cretaceous age. Since the Cretaceous carbonates along the steep slopes of the Escarpment have been shown to be good substrates for coral communities, it is likely that these talus deposits would support coral communities as well. Though chemosynthetic organisms have been seen at the base of the Escarpment by ROV and submersible dives, none of the talus deposits have been visited to our knowledge and the Okeanos Explorer’s multibeam did not detect any active water column gas plumes in the mapped area.
Copyright Text: William Shedd (william.shedd@boem.gov), Jon Burrell (jon.burrell@boem.gov), Pierre Abadie (pierre.abadie@boem.gov) & Kody Kramer, Bureau of Ocean Energy Management, Office of Resource Evaluation, New Orleans, LA. & NOAA.
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Spatial Reference: 4267 (4267)
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Templates:
Name: anomaly_Cretaceous_talus
Description:
Drawing Tool: esriFeatureEditToolPolygon
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Last Edit Date: 12/17/2024 7:03:02 PM
Schema Last Edit Date: 12/17/2024 7:03:02 PM
Data Last Edit Date: 11/13/2024 6:20:35 PM
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