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Vallparadís Park
Vallparadís Park (in Catalan language, Catalan and officially ''Parc de Vallparadís'')The translation would correspond to the term "Valleparaíso", in reference to the first settlers who found the waters of the confluence of the torrents and fertile lands. is a natural urban space located in the municipality of Terrassa, in the province of Barcelona, Spain. Its construction began in 1991, from several previous approaches during the 19th and 20th centuries, which culminated in the final drafting of the project by Manuel Ribas i Piera. The park was declared an ''Bien de Interés Cultural'' by the Government of Spain. From north to south it is about 3.5 km long, and averages about 100 m wide. The first fossil findings in the area date back a million years; samples of Pleistocene flora and fauna have been discovered at the Cal Guardiola site, while the first evidence of human presence dates back to the Iberians, Iberian period, found at the Egosa settlement. This site would eve ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mapa Parque De Vallparadís
Mapa or MAPA may refer to: People * Alec Mapa (born 1965), American actor, comedian and writer * Dennis Mapa (born 1969), Filipino economist and statistician * Jao Mapa (born 1976), Filipino actor * Placido Mapa Jr. (born 1932), Filipino businessman, economist, and government official * Suraj Mapa (born 1980), Sri Lankan actor * Victorino Mapa (1855–1927), Filipino chief justice and government official Other uses * Mapa (song), "Mapa" (song), a 2021 song by SB19 * Mexican American Political Association * Mapa (publisher), an Israeli subsidiary of Ituran * Mapa Group, a Turkish conglomerate * Mapa, a company producing latex gloves that merged with Hutchinson SA in 1973 * Most Affected People and Areas, a climate justice concept See also * * Mappa (other) * Mapah (other) {{disambiguation, surname ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Monumental Church Complex Of Sant Pere De Terrassa
Monumental church complex of Sant Pere is a Bien de Interés Cultural landmark in Terrassa, Province of Barcelona, Spain. The Romanesque complex of churches includes Sant Pere, Sant Miquel and Santa Maria (San Pedro, San Miguel and Santa María). They are situated at the confluence of Vallparadís and Monner (now Park Vallparadís), the most important artistic area of the city, which is noted for Catalan Romanesque art. It was the site of the former Diocese of Egara, an old Visigoth nucleus, in the 5th-8th centuries. History The three churches were built near the old Roman Égara (whose remains are still preserved), which was the seat of the Bishop of Égara around the year 450 and lasted until the Saracen invasion in the 8th century. The episcopal group adhered to the ancient Byzantine model of three churches: San Pedro, Santa Maria and San Miguel. After a long construction process, the current churches, of Romanesque design, were completed in present form during the 11th an ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Volcanic Rock
Volcanic rock (often shortened to volcanics in scientific contexts) is a rock formed from lava erupted from a volcano. In other words, it differs from other igneous rock by being of volcanic origin. Like all rock types, the concept of volcanic rock is artificial, and in nature volcanic rocks grade into hypabyssal and metamorphic rocks and constitute an important element of some sediments and sedimentary rocks. For these reasons, in geology, volcanics and shallow hypabyssal rocks are not always treated as distinct. In the context of Precambrian shield geology, the term "volcanic" is often applied to what are strictly metavolcanic rocks. Volcanic rocks and sediment that form from magma erupted into the air are called "volcaniclastics," and these are technically sedimentary rocks. Volcanic rocks are among the most common rock types on Earth's surface, particularly in the oceans. On land, they are very common at plate boundaries and in flood basalt provinces. It has been estimated t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Metamorphic Rock
Metamorphic rocks arise from the transformation of existing rock to new types of rock in a process called metamorphism. The original rock (protolith) is subjected to temperatures greater than and, often, elevated pressure of or more, causing profound physical or chemical changes. During this process, the rock remains mostly in the solid state, but gradually recrystallizes to a new texture or mineral composition. The protolith may be an igneous, sedimentary, or existing metamorphic rock. Metamorphic rocks make up a large part of the Earth's crust and form 12% of the Earth's land surface. They are classified by their protolith, their chemical and mineral makeup, and their texture. They may be formed simply by being deeply buried beneath the Earth's surface, where they are subject to high temperatures and the great pressure of the rock layers above. They can also form from tectonic processes such as continental collisions, which cause horizontal pressure, friction, and distorti ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Quaternary
The Quaternary ( ) is the current and most recent of the three periods of the Cenozoic Era in the geologic time scale of the International Commission on Stratigraphy (ICS). It follows the Neogene Period and spans from 2.58 million years ago to the present. The Quaternary Period is divided into two epochs: the Pleistocene (2.58 million years ago to 11.7 thousand years ago) and the Holocene (11.7 thousand years ago to today, although a third epoch, the Anthropocene, has been proposed but is not yet officially recognised by the ICS). The Quaternary Period is typically defined by the cyclic growth and decay of continental ice sheets related to the Milankovitch cycles and the associated climate and environmental changes that they caused. Research history In 1759 Giovanni Arduino proposed that the geological strata of northern Italy could be divided into four successive formations or "orders" ( it, quattro ordini). The term "quaternary" was introduced by Jules Desnoye ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Catalan Coastal Depression
The Catalan Coastal Depression, ca, Depressió Litoral Catalana, is a natural depression between the Catalan Pre-Coastal Range and the Mediterranean Sea. It is part of the Catalan Mediterranean System. Geography The Catalan Coastal Depression runs roughly in a NE-SW direction along parts of the following comarques: Empordà, Gironès, Selva, Maresme, Vallès, Barcelonès, Baix Llobregat, Penedès, Tarragonès, Baix Camp and Baix Ebre. The Catalan Coastal Depression is about 300 km long and 20 km wide on average. Some of the main Catalan cities are located in this area. Ecology Much of the surface of the Catalan Coastal Depression is subject to severe land degradation, owing mainly to urban sprawl. See also *Catalan Coastal Range The Catalan Coastal Range ( ca, Serralada Litoral Catalana, ) is a system of mountain ranges running parallel to the Mediterranean Sea coast in Catalonia, Spain. It is part of the Catalan Mediterranean System. Its main axis runs be ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fluvial Erosion
In geography and geology, fluvial processes are associated with rivers and streams and the deposits and landforms created by them. When the stream or rivers are associated with glaciers, ice sheets, or ice caps, the term glaciofluvial or fluvioglacial is used. Fluvial processes Fluvial processes include the motion of sediment and erosion or deposition on the river bed. The movement of water across the stream bed exerts a shear stress directly onto the bed. If the cohesive strength of the substrate is lower than the shear exerted, or the bed is composed of loose sediment which can be mobilized by such stresses, then the bed will be lowered purely by clearwater flow. In addition, if the river carries significant quantities of sediment, this material can act as tools to enhance wear of the bed ( abrasion). At the same time the fragments themselves are ground down, becoming smaller and more rounded (attrition). Sediment in rivers is transported as either bedload (the coarser frag ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neogene
The Neogene ( ), informally Upper Tertiary or Late Tertiary, is a geologic period and system that spans 20.45 million years from the end of the Paleogene Period million years ago ( Mya) to the beginning of the present Quaternary Period Mya. The Neogene is sub-divided into two epochs, the earlier Miocene and the later Pliocene. Some geologists assert that the Neogene cannot be clearly delineated from the modern geological period, the Quaternary. The term "Neogene" was coined in 1853 by the Austrian palaeontologist Moritz Hörnes (1815–1868). During this period, mammals and birds continued to evolve into modern forms, while other groups of life remained relatively unchanged. The first humans (''Homo habilis'') appeared in Africa near the end of the period. Some continental movements took place, the most significant event being the connection of North and South America at the Isthmus of Panama, late in the Pliocene. This cut off the warm ocean currents from the Pacific to th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Terrassa Museum
The Terrassa Museum is a museum entity which encompasses all the municipally owned museums in the city of Terrassa. It belongs to the History Museum and Monument Network of CataloniaVilaweb.cat ' access data 21/10/2010 and the Barcelona Provincial Council Local Museum Network. The Terrassa Museum has different areas, elements and collections related to the cultural heritage of Terrassa. It comprises the following sections: Vallparadís monastery-castle Vallparadís monastery-castle is the main section of the Terrassa museum. It was originally a defensive structure from the 12th century which was later converted into a monastery in the 14th-15th century. In 1959, it was opened to house the Municipal Art Museum and currently houses a permanent exhibition on the evolution of the territory and human settlement in Terrassa from the first Neolithic inhabitants to contemporary times. Churches of Sant Pere The monumental complex of the churches of Sant Pere encompasses the churches of San ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Carthusian Castle Of Vallparadís
The Carthusians, also known as the Order of Carthusians ( la, Ordo Cartusiensis), are a Latin enclosed religious order of the Catholic Church. The order was founded by Bruno of Cologne in 1084 and includes both monks and nuns. The order has its own rule, called the ''Statutes'', and their life combines both eremitical and cenobitic monasticism. The motto of the Carthusians is , Latin for "The Cross is steady while the world turns." The Carthusians retain a unique form of liturgy known as the Carthusian Rite. The name ''Carthusian'' is derived from the Chartreuse Mountains in the French Prealps: Bruno built his first hermitage in a valley of these mountains. These names were adapted to the English '' charterhouse'', meaning a Carthusian monastery.; french: Chartreuse; german: Kartause; it, Certosa; pl, Kartuzja; es, Cartuja Today, there are 23 charterhouses, 18 for monks and 5 for nuns. The alcoholic cordial Chartreuse has been produced by the monks of Grande Chartreuse s ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
