
Geology 104 - Spring 2007
Lecture #26
Virgin Islands and Dry Tortugas NP
Dry Tortugas NP
Topography and historty
- "Dry" = no fresh water; "Tortugas" =
turtles
- Discovered by Spanish in 1513
- NM 1935, NP 1992
- 7 keys + shoals (shallow areas of ocean)
- Islands change in shape & size
Geology
1. Rocks
- No bedrock exposed. Probably underlain by:
- Key Largo Limestone
- Miami Oolite
- Most islands composed entirely of sand (oolites & broken
coral)
2. Reefs
- Holocene & living corals
- 15 m thick
- Same species as in bedrock
- These are "stony corals"
- Colonial animals
- Hexagonal
- Calcite exoskeletons
- "Soft corals" live on shoals
- No hard skeleton
- Octagonal
- Threats to reefs
- Overfishing
- Global warming
- Too warm > "bleaching" > 95% die
West Indies Archipelago
- Consists of the Bahamas, the Greater Antilles, the Lesser
Antilles, and the Netherland Antilles
- Each chain of islands includes volcanic rocks
- Only the Lesser Antilles are currently active
Virgin Islands NP
Topography and History
- Pre-columbian inhabitants, Danish plantations, bought by
US
- NP 1956
- On island of St. John in the corner where the Greater Antilles
meet the Lesser
- Accessible only by ferry
Geology
1. Stratigraphy
|
Rocks |
Age |
| Coral reefs |
Quaternary (Holocene) |
| Hans Lollik & other fms (igneous) |
Tertiary |
| Outer Bass & Louisenhoi fms (lavas,
limestones) |
Cretaceous |
2. Plate Tectonics
- Volcanic rocks were erupted along subduction zones
- Caribbean Plate has complex history
- All 3 types of boundaries can be seen in Caribbean today
- Continuing volcanic activity along eastern subduction zone
- Mont Pelee on Martinique in 1902
- Soufriére on Guadalupe in 1976
- Soufriere Hills on Montserrat 1995-present
3. Marine features
- Terraces (= wave cut platforms) form at sea level by wave
erosion.
- When sea level rises/falls, terraces may form at different
levels.
- Sea level was affected by Pleistocene glaciers and by tectonic
movements.
- Coral reefs
- Patch reefs
- Coral reefs are among the most diverse ecosystems on Earth.
- Beaches
- No permanent streams on the island
- Beaches form from material carried ashore by waves
Virgin
Islands slides
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