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. · Recherche

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.

Identifiant: NAN130340148i1
Légende: 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.
Extrait de: The Lesser Antilles
Page: p. 116
Numéro: 116
Description: Carte topographique des 'îles Norman et Peter
Mot-clé Lieu: fr Îles Vierges britanniques
Mot-clé Siècle: 19
Type: fr Carte, plan
Format: image/jpeg
Conditions d'utilisation: fr Domaine public
Provenance: Service commun de la documentation de l’Université de Nantes
Plateforme source: Bibliothèque numérique Manioc
URI: http://www.manioc.org/images/NAN130340148i1

Collections: Images; Service commun de la documentation de l’Université de Nantes

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Contenus avec " Contient : 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. "
Titre	Classe
The Lesser Antilles	Texte