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Fig. 17 — The northern side of Nevis, looking east.

Fig. 49 — Diagram of a partly submerged cliff.

Fig. 20 — The southwestern coast of Dominica.

Fig. 10 — A rough outline of Statia, as seen through hazy air from the northwest end of St. Kitts: the huge inclined slabs of limestone, known as the “White Wall,” on the shore of the cone, appear to have been lifted up from a preëxistent submarine bank when the volcano was formed.

Fig. 63 — Rough plan of part of the west coast of Antigua, showing slightly cliffed headlands and beach-filled bays.

Fig. 61 — The subdued mountains of volcanic rocks in the southwestern quarter of Antigua. No shore cliffs are seen here.

Fig. 66 — The Island of St. Martin (from British Admiralty Chart No. 2038).

Fig. 48 — Cockroach Island, northwest of St. Thomas, looking north.

PL. II — The uplifted limestone island of Marie Galante.

PL. VIII — Isolated residual hills in the passage between St. Kitts and Nevis, looking east.

Fig. 31 — The low cliffs of the mid-west coast, St. Lucia.

Fig. 11 — The southeastern part of St. Kitts (from British Admiralty Chart No. 487).

Fig. 60 — Ideal section of the uptilted and down-worn half of the same atoll, drawn on twice the scale of Figure 59.

PL. VI — St. Kitts from Basseterre roadstead. Continuous with Pl. VII.

Fig. 2 — Saba Island (from U. S. Hydrogr. Office Chart No. 1011)

Fig. 45 — The embayed island of Virgin Gorda (from U. S. Hydrogr. Office Chart No. 3904).

Fig. 20 — The southwestern coast of Dominica.

Fig. 6 — Silver Hill, a maturely dissected volcanic mass at the northern angle of Montserrat. The cliff of the most exposed headland is about 450 feet high and is one of the highest cliffs seen on any island.

Fig. 43 — Norman and Peter islands (reproduced from British Admiralty Chart No. 2019). These skeleton islands lie southeast of St. Thomas, two miles back from the outer border of the great Virgin Island bank. The form of the islands suggests a long period of erosion without abrasion followed by a brief period of relatively strong submergence in association with which the headland cliffs were abraded.

Fig. 64 — Rough plan of the southwest coast of Antigua, showing slightly cliffed headlands and beach-filled bays.
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