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Geology of the United States Virgin Islands

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may explain north-plunging late folds, due to eastward movement of the Caribbean plate. The formation of the Cayman Trough produced the last significant tectonic feature on the islands after 39 million years ago, with sinistral strike-slip faults. A structural block produced as a result creates a 5.7
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basalt. Silt or sand-sized material is most common unlike the Louisenhoj Formation boulders, suggesting a more distant volcanic source. In fact, sediments become finer, ascending upward into the Picara Member and Mandal Member. Striking slump folds and deformation of limestone and conglomerate beds
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deposited along with the submarine volcanic activity, accompanied by dikes and small plutons in the Careen Hill Intrusive Suite. An extensional environment is inferred by the presence of sheeted dikes. Geologists have debated the origins of keratophyres, suggesting a back-arc basin environment,
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more typical of island arcs, above the Water Island Formation. Except as pillow basalt on Ramgoat Cay, primary volcanic units are scarce from this time period. Given the boulder-sized clasts and different mineralogy, geologists have inferred that these clasts must have originated from several
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One of the most in-depth studies of groundwater in the U.S. Virgin Islands was conducted by the U.S. Geological Survey in 1995, focused on Saint Croix. The south-central part of the island is underlain by alluvium and carbonate rocks, including lenses of silt and clay. The
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Kingshill Limestone and Pliocene Post-Kingshill Limestone are all a single hydrological unit. The water-table aquifer ranges between five and 68 feet below the grounds surface and overall groundwater in the area contained comparatively high sodium chloride concentrations.
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although this is challenged by high-levels of silica in the rocks. Local hydrothermal alteration was proposed as a reason for metal anomalies in the Lameshur Volcanic-Intrusive Complex.
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Unlike Saint John, on Saint Thomas, radiolarian chert exists but is much rarer. Pyroclastic flows are preserved on Saint Thomas, together with limited fossil-bearing
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followed the episode of compression, forming around 39 million years ago in the Eocene. East-west compression brought brittle fractures filled with veins of
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On Saint John, the Tutu Formation is the youngest stratified unit, although volcanism continued on the neighboring
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cement in upper rock units. The Outer Brass Limestone deposited during a lull in volcanic activity in the
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kilometer sinistrally offset contact between the Water Island and Louisenhoj formations.
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The 1.5 kilometer thick Louisenhoj Formation contains clasts which record a shift toward
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includes mafic volcanic rocks, with complex mineralogy that first began to erupt in the
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bound together with calcareous cement and including both marble and andesite clasts.
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below water, creating the two kilometer thick Water Island Formation in the
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The Narrows pluton and Virgin Gorda batholith, which are dominated by
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overlain and interspersed with carbonate and conglomerate units.
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Salt River Bay National Historical Park and Ecological Preserve
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Unsourced material may be challenged and removed. 154:The island began to form with keratophyre and 1100:Geography of the United States Virgin Islands 728: 348: 135:Geologic history, stratigraphy, and tectonics 57:"Geology of the United States Virgin Islands" 8: 302:https://pubs.usgs.gov/pp/p1631/P1631-tag.pdf 735: 721: 713: 355: 341: 333: 108:Learn how and when to remove this message 294: 7: 280:Jealousy formation, the Miocene and 139:Although the island chain comprises 46:adding citations to reliable sources 14: 185:different large vents close by. 22: 33:needs additional citations for 1: 1095:Geology of the United States 744:Geology of the United States 697:Virgin Islands Coral Reef NM 368:United States Virgin Islands 1116: 576:Delegates to U.S. Congress 162:on oceanic plateau crust. 374: 1046:Northern Mariana Islands 581:Congressional district 571:USVI Police Department 313:Graves, R. P. 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U.S. Virgin Islands
Mesozoic
Saint Croix
Saint Thomas
Saint John
pillow basalt
Early Cretaceous
Radiolarian
chert
clinopyroxene
andesite
basalt
limestone
calcite
Turonian
Santonian
marble
conglomerate
Late Cretaceous

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