Boca de Serpiente Formation | |
---|---|
Stratigraphic range: Priabonian | |
Type | Formation |
Lithology | |
Primary | Limestone |
Other | Hematite |
Location | |
Coordinates | 10°12′N62°00′W / 10.2°N 62.0°W |
Approximate paleocoordinates | 8°18′N55°24′W / 8.3°N 55.4°W |
Region | Gulf of Paria |
Country | Trinidad and Tobago |
Type section | |
Named for | Boca de la Serpiente |
The Boca de Serpiente Formation is a geologic formation in Trinidad and Tobago. The limestones stained red with hematite, preserve fossils dating back to the Priabonian period. [1]
The Gulf of Paria is a 7,800 km2 (3,000 sq mi) shallow semi-enclosed inland sea located between the island of Trinidad and the east coast of Venezuela. It separates the two countries by as little as 15 km at its narrowest and 120 km at its widest points. The tides within the Gulf are semi-diurnal in nature with a range of approximately 1m. The Gulf of Paria is considered to be one of the best natural harbors on the Atlantic coast of the Americas. The jurisdiction of the Gulf of Paria is split between Trinidad and Venezuela with Trinidad having control over approximately 2,940 km2 (1,140 sq mi) (37.7%) and Venezuela the remainder (62.3%).
The Columbus Channel or Serpent's Mouth, is a strait lying between Icacos Point in southwest Trinidad and Tobago and the north coast of Venezuela. It leads from the Atlantic Ocean to the Gulf of Paria. The channel is about nine miles (14 km) wide at its narrowest point.
Huevos is an island in the Republic of Trinidad and Tobago. The island is 1.01 km2 in area. It is one of the "Bocas Islands", which lie in the Bocas del Dragón between Trinidad and Venezuela.
The Bocas del Dragón are the series of straits separating the Gulf of Paria from the Caribbean Sea. There are four Bocas, from west to east:
Boca or BOCA may refer to:
Meretrix is a genus of edible saltwater clams, marine bivalve molluscs in the family Veneridae, the Venus clams. They appeared in the fossil record in the Cenomanian age.
The Gulf of Paria crossing is a hypothetical bridge or tunnel spanning the Gulf of Paria that would connect the island of Trinidad and South America.
The Tobago Volcanic Group is a geologic group in Trinidad and Tobago. It preserves radiolaria and ammonite fossils dating back to the Albian period. The formation contains the Bacolet Formation and comprises organic-rich, black pyritic siliceous mudstones and fine-grained volcaniclastic sandstones and siltstones.
The Manzanilla Formation is a geologic formation in Trinidad and Tobago. It preserves fossils dating back to the Middle Miocene period.
The Matura Formation is a geologic formation in Trinidad and Tobago. It preserves bivalve and gastropod fossils dating back to the Pliocene period.
The Morne l'Enfer Formation is a geologic formation in Trinidad and Tobago. It preserves fossils dating back to the Miocene to Early Pliocene period.
The Talparo Formation is a geologic formation in Trinidad and Tobago. It preserves fossils dating back to the Early Pliocene period.
The Tamana Formation is a geologic formation in Trinidad and Tobago. It preserves fossils dating back to the Burdigalian to Serravallian period.
The Brasso Formation is a geologic formation in Trinidad and Tobago. It preserves fossils dating back to the Early Eocene to Serravallian period.
The Brasso Clay is a geologic formation in Trinidad and Tobago. It preserves fossils dating back to the Neogene period.
The Nariva Formation is a geologic formation in Trinidad and Tobago. It preserves fossils dating back to the Paleogene period.
The Morne Diablo Limestone is a geologic formation in Morne Diablo, Trinidad and Tobago. It preserves fossils dating back to the Oligocene period. The formation is laterally equivalent to the Cipero Marl and San Fernando Formation.
Jennifer Rahim was a Trinidadian fiction writer, poet and literary critic.