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The La Toca Formation is a geologic formation in the northern and eastern part of the Dominican Republic. The formation, predominantly an alternating sequence of marls and turbiditic sandstones, breccias and conglomerates, is renowned for the preservation of insects and other arthropods in amber, known as Dominican amber. The formation is dated to the Burdigalian to Langhian stages of the Miocene period (Hemingfordian in the NALMA classification).

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dbo:abstract
  • The La Toca Formation is a geologic formation in the northern and eastern part of the Dominican Republic. The formation, predominantly an alternating sequence of marls and turbiditic sandstones, breccias and conglomerates, is renowned for the preservation of insects and other arthropods in amber, known as Dominican amber. The formation is dated to the Burdigalian to Langhian stages of the Miocene period (Hemingfordian in the NALMA classification). (en)
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  • La Toca Formation (en)
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  • Redmond (en)
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  • La Toca mine (en)
dbp:otherlithology
dbp:overlies
dbp:period
  • Langhian (en)
dbp:prilithology
dbp:region
  • Duarte, Hermanas Mirabal, Puerto Plata Province, Samaná Province & La Vega Provinces (en)
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  • 1982 (xsd:integer)
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  • 19.2 -69.3
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  • The La Toca Formation is a geologic formation in the northern and eastern part of the Dominican Republic. The formation, predominantly an alternating sequence of marls and turbiditic sandstones, breccias and conglomerates, is renowned for the preservation of insects and other arthropods in amber, known as Dominican amber. The formation is dated to the Burdigalian to Langhian stages of the Miocene period (Hemingfordian in the NALMA classification). (en)
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  • La Toca Formation (en)
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  • 19.200001 (xsd:float)
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  • -69.300003 (xsd:float)
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