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Table 3 Sedimentological characteristics of marine submersions deposits along the TAH17–1 core

From: A late Holocene record of marine high-energy events along the Atlantic coast of Morocco: new evidences from the Tahaddart estuary

Events Position in the core (cm) Thickness (cm) Grading Sorting Upper Contact Basal contact Other sedimentological characteristics
E1 87–92
125–140
20 No (chaotic structure) Very poorly sorted Relatively sharp Sharp (erosional) Angular gravels and Mud-clasts
E2 148–149 1 No Very poorly sorted Sharp Sharp No
E3 150–151 1 No Very poorly sorted Sharp Sharp No
E4 152–153 1 No Very poorly sorted Sharp Sharp No
E5 154–155 < 1 No Very poorly sorted Sharp Sharp No
E6 154–155 < 1 No Very poorly sorted Sharp Sharp No
E7 155–156 < 1 No Very poorly sorted Sharp Sharp No
E8 155–156 < 1 No Very poorly sorted Sharp Sharp No
E9 156–157 1 No Very poorly sorted Sharp Sharp No
E10 159–160 1 No Very poorly sorted Slightly Sharp Slightly Sharp No
E11 163.5–165 1,5 No Very poorly sorted Slightly Sharp Slightly Sharp No
E12 172–175 3 No Very poorly sorted Slightly Sharp Slightly Sharp No
E13 190–230 40 Unclear Very poorly sorted Sharp Gradational No
E14 248–270 22 Normal grading Poorly sorted Gradational Not found Mud-clasts