Geo final project

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Red Rocks Park is truly an incredible work of Mother Nature. It provides the only completely natural amphitheater in the world, and, more importantly, a detailed chronological map of the geologic history of Colorado.

Education Technology

Red Rocks Amphitheatre (Geology and Formation ) Guillermo Campillo Geo 111 12-07-2011

Fountain Formation North of Red Rocks ,[object Object]

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· archaeocyathid   o Cambrian - sessile, reef-building marine organisms of warm tropical and subtropical waters that lived during the early (lower) Cambrian period. · bioturbation   o Cambrian - the reworking of soils and sediments by animals or plants. Its effects include changing texture of sediments (diagenetic), bioirrigation and displacement of microorganisms and non-living particles. Common bioturbators include annelids and bivalves (mussels, clams, gastropods). · Burgess Shale   o Cambrian - located in the Canadian Rockies of British Columbia, is one of the world's most celebrated fossil fields. It is famous for the exceptional preservation of the soft parts of its fossils. At 505 million years (Middle Cambrian) old, it is one of the earliest fossil beds containing soft-part imprints. · Cambrian explosion   o Cambrian - the relatively rapid appearance, around 530 million years ago, of most major animal phyla, as demonstrated in the fossil record, accompanied by major diversification of organisms · Iapetus Ocean   Cambrian/Ordovician - Precursor to the Atlantic. An ocean that existed in the Neoproterozoic and Paleozoic eras of the geologic timescale (between 600 and 400 million years ago). The ocean disappeared with the Caledonian, Taconic and Acadian orogenies, when these three continents joined to form one big landmass called Laurussia.  maturity  Cambrian · Paleozoic Era   o Cambrian - the earliest of three geologic eras of the Phanerozoic Eon, spanning from roughly 541 to 252.2 million years ago. It is the longest of the Phanerozoic eras, and is subdivided into six geologic periods (from oldest to youngest): the Cambrian, Ordovician, Silurian, Devonian, Carboniferous, and Permian. · passive margin   o Cambrian - the transition between oceanic and continental crust which is not an active plate margin. It is constructed by sedimentation above an ancient rift, now marked by transitional crust. Continental rifting creates new ocean basins. ·  trilobite   o Cambrian - extinct marine arthropods that form the class Trilobita. Trilobites form one of the earliest known groups of arthropods. Trilobites finally disappeared in the mass extinction at the end of the Permian about 250 million years ago. The trilobites were among the most successful of all early animals, roaming the oceans for over 270 million years. ·  bentonites o  Ordovician - essentially impure clay consisting mostly of montmorillonite. Bentonite usually forms from weathering of volcanic ash, most often in the presence of water. However, the term bentonite, as well as a similar clay called tonstein, has been used to describe clay beds of uncertain origin. · Cincinnati arch   o Ordovician - when continents crashed together during the two orogeny's you have the Appalachian mountains and then a down drop into the Appalachian basin going west and then going west the next rise is the Cincinnati arch and the next basin is the Illinois basin.  epeir.

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