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Casibari
Casibari is a settlement of Paradera, north of Hooiberg, in Aruba. Evidence of prehistoric rock drawings is still visible at the site. "Casibari" is an Indian name of Arawak (possibly Taíno) origin and can be explained as follows: CA as a prefix: where there are, SIBA (or CIBA) is stone and RI as a suffix is: good; so Where There are Good Stones. The name can also be explained as follows: CASIBA (or CACIBA) is hollow or cavern with RI is good; so Good Hole (cavern). This toponym also stands for ''cas di baril'', house of barrel, the first tin house of Aruba, made from oil barrels. Geography Landforms Aruba was mainly shaped by plate collisions that led to the creation of igneous rocks and their subsequent exposure. However, despite this volcanic origin, a significant portion of the surface features in this area consists of sedimentary landforms. This transformation occurred during the Upper Eocene epoch when sedimentary processes, like the formation of reef terraces, took ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ayo Rock Formations
Ayo Rock Formations are monolithic rock boulders located on the island of Aruba in the Caribbean, near Ayo village and about from the defunct natural bridge towards Casibari. Similarly, the Casibari Boulders are about inland between Natural Bridge and Oranjestad, the capital of Aruba, to the west of Boca Andicuri. History The Arawak people were the earliest settlers on the island. They used to visit Ayo Rock Formations so that they could hear incoming thunderstorms closing in on the island of Aruba. They also carved paintings in rocks called petroglyphs while performing religious rites. Formations One of the most unusual and notable rock formations on the island are the Casibari Boulders, which are tonalite rocks seen to the north of Hooiberg. They rise above the desert landscape giving a panoramic view of the island. They are located amidst cacti, and lizards are commonly encountered here. The boulders have unusual shapes resembling birds and dragons. There is no plausible ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hooiberg
( Dutch: /ˈɦojbɛrx/ ()) is a distinctively shaped, conical hill located at the heart of the island of Aruba. This geological formation is a prominent and recognizable landmark that has long captured the attention of locals and visitors alike—Hooiberg is Aruba's centerpiece. Name Many old place names ( toponyms) on Aruba have indigenous origins, but the language that was spoken in the past has been lost to posterity. Historically, this hill was known as ''Orcuyo,'' an old indigenous name. The hill has had various names throughout the years. In Spanish, it was called ''Cerro de Paja ó Pan de Azucar'', meaning "hill of straw", "sugar bread", or " sugarloaf". Sugarloaf refers to refined sugar shaped into a tall conical form, which was sold before the 1900s. Hooiberg is one of several formations named after Cerro Pan de Azucar (such as Pan de Azucar Island in the Philippines or Sugarloaf Mountain in Brazil). The Dutch gave it their own name, and the spelling of Hooiberg ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Aruba
Aruba, officially the Country of Aruba, is a constituent island country within the Kingdom of the Netherlands, in the southern Caribbean Sea north of the Venezuelan peninsula of Paraguaná Peninsula, Paraguaná and northwest of Curaçao. In 1986, Aruba became a constituent country within the Kingdom of the Netherlands and acquired the formal name the Country of Aruba. Aruba has an area of . Aruba measures in length from its northwestern to its southeastern end and is across at its widest point. Aruba is geologically located in South America, South-America, lying on the South-American continental shelf. Alongside Bonaire and Curaçao, Aruba forms a group referred to as the ABC islands (Leeward Antilles), ABC islands. The Dutch Caribbean encompasses the ABC islands along with the other three substantial islands, the SSS islands. In contrast to much of the Caribbean, which experiences humid tropical climates, Aruba has a dry climate with an arid Deserts and xeric shrublands, xer ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Paradera
Paradera is a small town and census region near the northeast end of the island of Aruba. The census region Paradera encompasses the town of Paradera as well as nearby settlements and neighborhoods within Paradera, including Ayo, Bloemond, Piedra Plat, and Shiribana. At the time of the 2010 census, Paradera proper had a population of 2,486. The Paradera census region had a population of 12,024. St. Philomena's Church, a Roman Catholic The Catholic Church (), also known as the Roman Catholic Church, is the largest Christian church, with 1.27 to 1.41 billion baptized Catholics worldwide as of 2025. It is among the world's oldest and largest international institut ... church, dominates the skyline relative to the rest of the town's buildings. The region of Paradera has an estimated area of 20.40 square kilometers. Population At the time of the 2010 census, the following settlements were counted as a part of the Paradera census region. Until the 2010 census, pre ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Arawak
The Arawak are a group of Indigenous peoples of northern South America and of the Caribbean. The term "Arawak" has been applied at various times to different Indigenous groups, from the Lokono of South America to the Taíno (Island Arawaks), who lived in the Greater Antilles and northern Lesser Antilles in the Caribbean. All these groups spoke related Arawakan languages. Name Early Spanish explorers and administrators used the terms ''Arawak'' and '' Caribs'' to distinguish the peoples of the Caribbean, with ''Carib'' reserved for Indigenous groups that they considered hostile and ''Arawak'' for groups that they considered friendly. In 1871, ethnologist Daniel Garrison Brinton proposed calling the Caribbean populace "Island Arawak" because of their cultural and linguistic similarities with the mainland Arawak. Subsequent scholars shortened this convention to "Arawak", creating confusion between the island and mainland groups. In the 20th century, scholars such as Irving Ro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Taíno
The Taíno are the Indigenous peoples of the Caribbean, Indigenous peoples of the Greater Antilles and surrounding islands. At the time of European contact in the late 15th century, they were the principal inhabitants of most of what is now The Bahamas, Cuba, the Dominican Republic, Haiti, Jamaica, Puerto Rico, and the northern Lesser Antilles. The Lucayan people, Lucayan branch of the Taíno were the first New World peoples encountered by Christopher Columbus, in the Lucayan Archipelago, Bahama Archipelago on October 12, 1492. The Taíno historically spoke an Arawakan languages, Arawakan language. Granberry and Vescelius (2004) recognized two varieties of the Taino language: "Classical Taino", spoken in Puerto Rico and most of Hispaniola, and "Ciboney Taino", spoken in the Bahamas, most of Cuba, western Hispaniola, and Jamaica. They lived in agricultural societies ruled by caciques with fixed settlements and a Matrilineality, matrilineal system of kinship and inheritance. Taíno ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plate Tectonics
Plate tectonics (, ) is the scientific theory that the Earth's lithosphere comprises a number of large tectonic plates, which have been slowly moving since 3–4 billion years ago. The model builds on the concept of , an idea developed during the first decades of the 20th century. Plate tectonics came to be accepted by Earth science, geoscientists after seafloor spreading was validated in the mid-to-late 1960s. The processes that result in plates and shape Earth's crust are called ''tectonics''. Tectonic plates also occur in other planets and moons. Earth's lithosphere, the rigid outer shell of the planet including the crust (geology), crust and upper mantle, is fractured into seven or eight major plates (depending on how they are defined) and many minor plates or "platelets". Where the plates meet, their relative motion determines the type of plate boundary (or fault (geology), fault): , , or . The relative movement of the plates typically ranges from zero to 10 cm annu ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Igneous Rock
Igneous rock ( ), or magmatic rock, is one of the three main rock types, the others being sedimentary and metamorphic. Igneous rocks are formed through the cooling and solidification of magma or lava. The magma can be derived from partial melts of existing rocks in either a planet's mantle or crust. Typically, the melting is caused by one or more of three processes: an increase in temperature, a decrease in pressure, or a change in composition. Solidification into rock occurs either below the surface as intrusive rocks or on the surface as extrusive rocks. Igneous rock may form with crystallization to form granular, crystalline rocks, or without crystallization to form natural glasses. Igneous rocks occur in a wide range of geological settings: shields, platforms, orogens, basins, large igneous provinces, extended crust and oceanic crust. Geological significance Igneous and metamorphic rocks make up 90–95% of the top of the Earth's crust by volume. Igneous rock ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Sedimentary Rock
Sedimentary rocks are types of rock (geology), rock formed by the cementation (geology), cementation of sediments—i.e. particles made of minerals (geological detritus) or organic matter (biological detritus)—that have been accumulated or deposited at Earth's surface. Sedimentation is any process that causes these particles to settle in place. Geological detritus originates from weathering and erosion of existing rocks, or from the solidification of molten lava blobs erupted by volcanoes. The geological detritus is transported to the place of deposition by water, wind, ice or Mass wasting, mass movement, which are called agents of denudation. Biological detritus is formed by bodies and parts (mainly shells) of dead aquatic organisms, as well as their fecal mass, suspended in water and slowly piling up on the floor of water bodies (marine snow). Sedimentation may also occur when dissolved minerals precipitate from aqueous solution, water solution. The sedimentary rock cover of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Upper Eocene
The Eocene ( ) is a geological epoch that lasted from about 56 to 33.9 million years ago (Ma). It is the second epoch of the Paleogene Period in the modern Cenozoic Era. The name ''Eocene'' comes from the Ancient Greek (''Ēṓs'', 'Dawn') and (''kainós'', "new") and refers to the "dawn" of modern ('new') fauna that appeared during the epoch.See: *Letter from William Whewell to Charles Lyell dated 31 January 1831 in: * From p. 55: "The period next antecedent we shall call Eocene, from ήως, aurora, and χαινος, recens, because the extremely small proportion of living species contained in these strata, indicates what may be considered the first commencement, or ''dawn'', of the existing state of the animate creation." The Eocene spans the time from the end of the Paleocene Epoch to the beginning of the Oligocene Epoch. The start of the Eocene is marked by a brief period in which the concentration of the carbon isotope 13C in the atmosphere was exceptionally low in co ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Epoch
In chronology and periodization, an epoch or reference epoch is an instant in time chosen as the origin of a particular calendar era. The "epoch" serves as a reference point from which time is measured. The moment of epoch is usually decided by congruity, or by following conventions understood from the epoch in question. The epoch moment or date is usually defined from a specific, clear event of change, an ''epoch event''. In a more gradual change, a deciding moment is chosen when the ''epoch criterion'' was reached. Calendar eras Pre-modern eras * The Yoruba calendar (''Kọ́jọ́dá'') uses 8042 BC as the epoch, regarded as the year of the creation of Ile-Ife by the god Obatala, also regarded as the creation of the earth. * '' Anno Mundi'' it. "Year of the World"(years since the creation of the world) is used in ** the Byzantine calendar (5509 BC). ** the Hebrew calendar (3761 BC). * The Mesoamerican Long Count Calendar uses the creation of the fourth worl ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Reef
A reef is a ridge or shoal of rock, coral, or similar relatively stable material lying beneath the surface of a natural body of water. Many reefs result from natural, abiotic component, abiotic (non-living) processes such as deposition (geology), deposition of sand or wave erosion planning down rock outcrops. However, reefs such as the coral reefs of tropical waters are formed by biotic component, biotic (living) processes, dominated by corals and coralline algae. Artificial reefs, such as shipwrecks and other man-made underwater structures, may occur intentionally or as the result of an accident. These are sometimes designed to increase the physical complexity of featureless sand bottoms to attract a more diverse range of organisms. They provide shelter to various aquatic animals which help prevent extinction. Another reason reefs are put in place is for aquaculture, and fish farmers who are looking to improve their businesses sometimes invest in them. Reefs are often quite n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
