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Guaduas Formation
The Guaduas Formation ( es, Formación Guaduas, K2P1G, K2E1G, KPgg, KTg, TKg, Ktg) is a geological formation of the Middle Magdalena Basin and the Altiplano Cundiboyacense, Eastern Ranges of the Colombian Andes. The predominantly shale with coalbed formation dates to the Late Cretaceous and Paleogene periods; Maastrichtian-Paleocene epochs, and has a maximum thickness of . Fossils of '' Coussapoa camargoi'', '' Ficus andrewsi'', '' Berhamniphyllum sp.'' and '' Archaeopaliurus boyacensis'' have been found in coalbeds in Zipaquirá and Tasco, Boyacá. Etymology The formation was first described by Hettner in 1894 and named in 1931 by Hubach after Guaduas, Cundinamarca, former northern territory of the Panche.Montoya & Reyes, 2005, p.51 Description Lithologies The Guaduas Formation consists mainly of shales with intercalated sandstone beds. The formation contains coalbeds that are widely explored in the area. Fossil remains of '' Coussapoa camargoi'', '' Ficus andrewsi'', ' ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Maastrichtian
The Maastrichtian () is, in the ICS geologic timescale, the latest age (uppermost stage) of the Late Cretaceous Epoch or Upper Cretaceous Series, the Cretaceous Period or System, and of the Mesozoic Era or Erathem. It spanned the interval from . The Maastrichtian was preceded by the Campanian and succeeded by the Danian (part of the Paleogene and Paleocene). The Cretaceous–Paleogene extinction event (formerly known as the Cretaceous–Tertiary extinction event) occurred at the end of this age. In this mass extinction, many commonly recognized groups such as non-avian dinosaurs, plesiosaurs and mosasaurs, as well as many other lesser-known groups, died out. The cause of the extinction is most commonly linked to an asteroid about wide colliding with Earth, ending the Cretaceous. Stratigraphic definitions Definition The Maastrichtian was introduced into scientific literature by Belgian geologist André Hubert Dumont in 1849, after studying rock strata of the Chalk Group c ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Formation (geology)
A geological formation, or simply formation, is a body of rock having a consistent set of physical characteristics ( lithology) that distinguishes it from adjacent bodies of rock, and which occupies a particular position in the layers of rock exposed in a geographical region (the stratigraphic column). It is the fundamental unit of lithostratigraphy, the study of strata or rock layers. A formation must be large enough that it can be mapped at the surface or traced in the subsurface. Formations are otherwise not defined by the thickness of their rock strata, which can vary widely. They are usually, but not universally, tabular in form. They may consist of a single lithology (rock type), or of alternating beds of two or more lithologies, or even a heterogeneous mixture of lithologies, so long as this distinguishes them from adjacent bodies of rock. The concept of a geologic formation goes back to the beginnings of modern scientific geology. The term was used by Abraham Gottlob Wer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Cretaceous–Paleogene Boundary
The Cretaceous–Paleogene (K–Pg) boundary, formerly known as the Cretaceous–Tertiary (K–T) boundary, is a geological signature, usually a thin band of rock containing much more iridium than other bands. The K–Pg boundary marks the end of the Cretaceous Period, the last period of the Mesozoic Era, and marks the beginning of the Paleogene Period, the first period of the Cenozoic Era. Its age is usually estimated at around 66 million years, with radiometric dating yielding a more precise age of 66.043 ± 0.011 Ma. The K–Pg boundary is associated with the Cretaceous–Paleogene extinction event, a mass extinction which destroyed a majority of the world's Mesozoic species, including all dinosaurs except for birds. Strong evidence exists that the extinction coincided with a large meteorite impact at the Chicxulub crater and the generally accepted scientific theory is that this impact triggered the extinction event. The word "Cretaceous" is derived from the Latin "creta" (ch ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fossilworks
Fossilworks is a portal which provides query, download, and analysis tools to facilitate access to the Paleobiology Database The Paleobiology Database is an online resource for information on the distribution and classification of fossil animals, plants, and microorganisms. History The Paleobiology Database (PBDB) originated in the NCEAS-funded Phanerozoic Marine Pale ..., a large relational database assembled by hundreds of paleontologists from around the world. History Fossilworks was created in 1998 by John Alroy and is housed at Macquarie University. It includes many analysis and data visualization tools formerly included in the Paleobiology Database.{{cite web, title=Frequently asked questions, url=http://www.fossilworks.org/cgi-bin/bridge.pl?page=FAQ, publisher=Fossilworks, access-date=17 December 2021 References {{Reflist External links {{Wikidata property, P842 * [Baidu] |
Sandstone
Sandstone is a clastic sedimentary rock composed mainly of sand-sized (0.0625 to 2 mm) silicate grains. Sandstones comprise about 20–25% of all sedimentary rocks. Most sandstone is composed of quartz or feldspar (both silicates) because they are the most resistant minerals to weathering processes at the Earth's surface. Like uncemented sand, sandstone may be any color due to impurities within the minerals, but the most common colors are tan, brown, yellow, red, grey, pink, white, and black. Since sandstone beds often form highly visible cliffs and other topographic features, certain colors of sandstone have been strongly identified with certain regions. Rock formations that are primarily composed of sandstone usually allow the percolation of water and other fluids and are porous enough to store large quantities, making them valuable aquifers and petroleum reservoirs. Quartz-bearing sandstone can be changed into quartzite through metamorphism, usually related to ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Panche People
The Panche or Tolima is an indigenous group of people in what is now Colombia. Their language is unclassified – and possibly unclassifiable – but may have been Cariban. They inhabited the southwestern parts of the department of Cundinamarca and the northeastern areas of the department of Tolima, close to the Magdalena River. At the time of the Spanish conquest, more than 30,000 Panche were living in what would become the New Kingdom of Granada. Early knowledge about the Panche has been compiled by scholar Pedro Simón. According to the latter, the word ''panche'' in their own Panche language means "cruel" and "murderer". Panche territory The Panche were inhabiting the lower altitude southwestern areas of the Cundinamarca department, close to the Magdalena River. Their northern neighbours were the Muzo in the northeast and the Pantágora in the northwest, in the east the Muisca, in the southeast the Sutagao and to the south and southwest the Pijao. The northern limits we ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tasco, Boyacá
Tasco is a town and municipality in the Valderrama Province, part of the Colombian department of Boyacá. Tasco is situated on the Altiplano Cundiboyacense at altitudes ranging from to . The Chicamocha River flows through the municipality which borders Socha in the north, Corrales and Gámeza in the south, Socotá in the east and Betéitiva and Paz de Río in the west. The urban centre is located at an altitude of at from the department capital Tunja. Etymology Tasco in the Chibcha language of the Muisca means "Enclosure or mansion of the sovereign".Etymology Municipalities Boyacá - Excelsio.net History The area of Tasco was inhabited by the Boche and Pirgua tribes, before the |
Ficus Andrewsi
''Ficus'' ( or ) is a genus of about 850 species of woody trees, shrubs, vines, epiphytes and hemiepiphytes in the family (biology), family Moraceae. Collectively known as fig trees or figs, they are native throughout the tropics with a few species extending into the semi-warm temperate zone. The common fig (''F. carica'') is a temperate species native to southwest Asia and the Mediterranean region (from Afghanistan to Portugal), which has been widely cultivated from ancient times for its fruit, also referred to as figs. The fruit of most other species are also edible though they are usually of only local economic importance or eaten as bushfood. However, they are extremely important food resources for wildlife. Figs are also of considerable cultural importance throughout the tropics, both as objects of worship and for their many practical uses. Description ''Ficus'' is a pantropical genus of trees, shrubs, and vines occupying a wide variety of ecological niches; most a ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Coussapoa
''Coussapoa'' is a genus of flowering plants belonging to the family Urticaceae. Its native range is Mexico, Central & Southern Tropical America. Species: *'' Coussapoa angustifolia'' *'' Coussapoa arachnoidea'' *''Coussapoa argentea'' *'' Coussapoa asperifolia'' *'' Coussapoa batavorum'' *'' Coussapoa brevipes'' *''Coussapoa chocoensis'' *'' Coussapoa cinnamomea'' *''Coussapoa cinnamomifolia'' *'' Coussapoa contorta'' *''Coussapoa crassivenosa'' *'' Coussapoa cupularis'' *'' Coussapoa curranii'' *''Coussapoa darienensis'' *''Coussapoa david-smithii'' *''Coussapoa dolichandra'' *''Coussapoa duquei'' *''Coussapoa echinata'' *''Coussapoa ferruginea'' *''Coussapoa floccosa'' *''Coussapoa fulvescens'' *''Coussapoa glaberrima'' *''Coussapoa herthae'' *''Coussapoa jatun-sachensis'' *'' Coussapoa latifolia'' *'' Coussapoa leprieurii'' *''Coussapoa longipedunculata'' *''Coussapoa macerrima'' *'' Coussapoa manuensis'' *''Coussapoa microcarpa'' *''Coussapoa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paleogene
The Paleogene ( ; British English, also spelled Palaeogene or Palæogene; informally Lower Tertiary or Early Tertiary) is a geologic period, geologic period and system that spans 43 million years from the end of the Cretaceous Period million years ago (annum, Mya) to the beginning of the Neogene Period Mya. It is the beginning of the Cenozoic Era of the present Phanerozoic Eon. The earlier term Tertiary Period was used to define the span of time now covered by the Paleogene Period and subsequent Neogene Period; despite no longer being recognised as a formal stratigraphy, stratigraphic term, 'Tertiary' is still widely found in earth science literature and remains in informal use. Paleogene is often abbreviated "Pg" (but the United States Geological Survey uses the abbreviation PE for the Paleogene on the Survey's geologic maps). During the Paleogene, evolution of mammals, mammals diversified from relatively small, simple forms into a large group of diverse animals in the wake of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Saunders_Quarry-1.jpg "Click for more on -> Sandstone")
