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List of National Natural Landmarks in American Samoa - Wikipedia Jump to content

List of National Natural Landmarks in American Samoa

From Wikipedia, the free encyclopedia

This is a list of National Natural Landmarks (NNL) in American Samoa . All locations are on communally owned lands.

Name Designated District Coordinates Description Image
Cape Taputapu 1972 Western 14°19′17″S 170°50′36″W  /  14.3214°S 170.8432°W  / -14.3214; -170.8432  ( Cape Taputapu National Natural Landmark ) A natural exhibit of shoreline, offshore volcanic rocks, and blowholes sculpted by heavy sea-wave action
Fogama?a Crater 1972 Western 14°21′24″S 170°45′13″W  /  14.3568°S 170.7535°W  / -14.3568; -170.7535  ( Fogama'a Crater National Natural Landmark ) One of very few illustrations of the most recent episode of volcanism in American Samoa
Matafao Peak 1972 Eastern 14°17′38″S 170°42′16″W  /  14.2939°S 170.7045°W  / -14.2939; -170.7045  ( Matafao Peak National Natural Landmark ) One of five great masses of volcanic rocks that extruded as molten magma during the major episodes of volcanism that created Tutuila Island
Le?ala Shoreline 1972 Western 14°21′36″S 170°46′38″W  /  14.3600°S 170.7773°W  / -14.3600; -170.7773  ( Le'ala Shoreline National Natural Landmark ) A young flow of basalt, inter-bedded with layers of tuff , that illustrates erosion by wave action
Rainmaker Mountain
(Mount Pioa)
1972 Eastern 14°16′21″S 170°39′21″W  /  14.2725°S 170.6558°W  / -14.2725; -170.6558  ( Rainmaker Mountain (Mt. Pioa) National Natural Landmark ) An outstanding example of the gigantic plugs that created Tutuila Island
Vai'ava Strait 1972 Eastern 14°14′21″S 170°40′17″W  /  14.2393°S 170.6715°W  / -14.2393; -170.6715  ( Vai'ava Strait National Natural Landmark ) A classic illustration of steep cliffs and erosion-resistant outliers formed by wave action on a volcanic mass
Aunu'u Island 1972 Eastern 14°17′00″S 170°33′12″W  /  14.2833°S 170.5534°W  / -14.2833; -170.5534  ( Aunu'u Island National Natural Landmark ) The site of recent episodes of volcanism backed by a geologically recent tuff cone
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