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Salobreña
Salobreña (, < Phoenician ''Salambina Salawbiniya'') is a town on the '''' in , Spain. It claims a history stretching back 6,000 years. There are two main parts of Salobreña; The first is The Old Town which sits atop a rocky prominence and is a cluster of whitewashed houses and steep narrow streets leading up to a tenth-century castle, called 'Castillo de Salobreña' and it is one of its main tourist attractions. The second part of Salobreña is new developments which spread from the bottom of the Old Town right to the beach. The whole town is almost surrounded by sugarcane field ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Costa Tropical
Costa Granadina is a comarca in southern Spain, corresponding to the Mediterranean coastline of the province of Granada. It is also but less frequently called the Costa Tropical or Costa de Granada. It is crossed by the N-340 coastal highway that runs southwest–northeast along Spain's Mediterranean coast, to the border with France. Within the last 4 years the A7 motorway has been extended along the coast from Nerja in the Málaga province to Motril where it links the A7 motorway to the A44 motorway which heads north from Motril to the city of Granada. Geography The Costa Granadina is made up mostly of agricultural zones and small resort towns and villages. What makes the Costa Granadina unique in comparison to the rest of the Spanish coast is that the mountains of the Sierra Nevada range fall to the very edge of the Mediterranean Sea on the rugged coastline. Except for ''la vega de Motril'', there are no flat areas for large urban sprawl. Climate The area east of Málaga is ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Province Of Granada
Granada is a province of southern Spain, in the eastern part of the autonomous community of Andalusia. It is bordered by the provinces of Albacete, Murcia, Almería, Jaén, Córdoba, Málaga, and the Mediterranean Sea (along the Costa Tropical). Its capital city is also called Granada. The province covers an area of . Its population was 921,338 , of whom about 30% live in the capital, and its average population density is . It contains 170 municipalities. Geography The tallest mountain in the Iberian Peninsula, Mulhacén, is located in Granada. It measures . The next highest mountains in the province are Veleta () and Alcazaba (). The river Genil, which rises in Granada, is one of the main tributaries of the Guadalquivir. Other important rivers include the Fardes, Monachil, Guadalfeo, Dílar, Ízbor, Verde and Darro. Granada shares the Sierra Nevada National Park (in the Sierra Nevada mountain range) with Almería province. Another important range is the Sierra de Baza. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Province Of Granada
Granada is a province of southern Spain, in the eastern part of the autonomous community of Andalusia. It is bordered by the provinces of Albacete, Murcia, Almería, Jaén, Córdoba, Málaga, and the Mediterranean Sea (along the Costa Tropical). Its capital city is also called Granada. The province covers an area of . Its population was 921,338 , of whom about 30% live in the capital, and its average population density is . It contains 170 municipalities. Geography The tallest mountain in the Iberian Peninsula, Mulhacén, is located in Granada. It measures . The next highest mountains in the province are Veleta () and Alcazaba (). The river Genil, which rises in Granada, is one of the main tributaries of the Guadalquivir. Other important rivers include the Fardes, Monachil, Guadalfeo, Dílar, Ízbor, Verde and Darro. Granada shares the Sierra Nevada National Park (in the Sierra Nevada mountain range) with Almería province. Another important range is the Sierra de Baza. Th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Guadalfeo
The Guadalfeo is a small river in the province of Granada, Spain between the Sierra Nevada mountain range and the coastal ranges of Sierra de la Contraviesa and Lújar. This river is formed by the merging of three rivers, the Rio Poqueira, Río Trevélez, and Cádiar. The Poqueira and the Trevélez join shortly before the confluence with the Cádiar near the town of Órgiva. The river flows through the region of La Alpujarra for much of its course and enters the sea near Motril after passing through a spectacular gorge between the Lújar and Chaparal mountains. Although it is often dried up by this point, its waters are often used for agricultural purposes. The Rules dam was recently built across the river near Vélez de Benaudalla at the head of the gorge, resulting in the creation of a large reservoir and the flooding of a section of the river valley. See also * List of rivers of Spain This is an incomplete list of rivers that are at least partially in Spain. The rivers f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Phoenicians
Phoenicia () was an ancient Semitic-speaking peoples, ancient thalassocracy, thalassocratic civilization originating in the Levant region of the eastern Mediterranean, primarily located in modern Lebanon. The territory of the Phoenician city-states extended and shrank throughout their history, and they possessed several enclaves such as Arwad and Tell Sukas (modern Syria). The core region in which the Phoenician culture developed and thrived stretched from Tripoli, Lebanon, Tripoli and Byblos in northern Lebanon to Mount Carmel in modern Israel. At their height, the Phoenician possessions in the Eastern Mediterranean stretched from the Orontes River mouth to Ashkelon. Beyond its homeland, the Phoenician civilization extended to the Mediterranean from Cyprus to the Iberian Peninsula. The Phoenicians were a Ancient Semitic-speaking peoples, Semitic-speaking people of somewhat unknown origin who Ethnogenesis, emerged in the Levant around 3000 BC. The term ''Phoenicia'' is an ancien ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bronze Age
The Bronze Age is a historic period, lasting approximately from 3300 BC to 1200 BC, characterized by the use of bronze, the presence of writing in some areas, and other early features of urban civilization. The Bronze Age is the second principal period of the three-age system proposed in 1836 by Christian Jürgensen Thomsen for classifying and studying ancient societies and history. An ancient civilization is deemed to be part of the Bronze Age because it either produced bronze by smelting its own copper and alloying it with tin, arsenic, or other metals, or traded other items for bronze from production areas elsewhere. Bronze is harder and more durable than the other metals available at the time, allowing Bronze Age civilizations to gain a technological advantage. While terrestrial iron is naturally abundant, the higher temperature required for smelting, , in addition to the greater difficulty of working with the metal, placed it out of reach of common use until the end o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeolithic Period
The Paleolithic or Palaeolithic (), also called the Old Stone Age (from Greek: παλαιός ''palaios'', "old" and λίθος ''lithos'', "stone"), is a period in human prehistory that is distinguished by the original development of stone tools, and which represents almost the entire period of human prehistoric technology. It extends from the earliest known use of stone tools by hominins, 3.3 million years ago, to the end of the Pleistocene, 11,650 cal BP. The Paleolithic Age in Europe preceded the Mesolithic Age, although the date of the transition varies geographically by several thousand years. During the Paleolithic Age, hominins grouped together in small societies such as bands and subsisted by gathering plants, fishing, and hunting or scavenging wild animals. The Paleolithic Age is characterized by the use of knapped stone tools, although at the time humans also used wood and bone tools. Other organic commodities were adapted for use as tools, includ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neolithic Period
The Neolithic period, or New Stone Age, is an Old World archaeological period and the final division of the Stone Age. It saw the Neolithic Revolution, a wide-ranging set of developments that appear to have arisen independently in several parts of the world. This "Neolithic package" included the introduction of farming, domestication of animals, and change from a hunter-gatherer lifestyle to one of settlement. It began about 12,000 years ago when farming appeared in the Epipalaeolithic Near East, and later in other parts of the world. The Neolithic lasted in the Near East until the transitional period of the Chalcolithic (Copper Age) from about 6,500 years ago (4500 BC), marked by the development of metallurgy, leading up to the Bronze Age and Iron Age. In other places the Neolithic followed the Mesolithic (Middle Stone Age) and then lasted until later. In Ancient Egypt, the Neolithic lasted until the Protodynastic period, 3150 BC.Karin Sowada and Peter Grave. Egypt in the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alluvial Plain
An alluvial plain is a largely flat landform created by the deposition of sediment over a long period of time by one or more rivers coming from highland regions, from which alluvial soil forms. A floodplain is part of the process, being the smaller area over which the rivers flood at a particular period of time, whereas the alluvial plain is the larger area representing the region over which the floodplains have shifted over geological time. As the highlands erode due to weathering and water flow, the sediment from the hills is transported to the lower plain. Various creeks will carry the water further to a river, lake, bay, or ocean. As the sediments are deposited during flood conditions in the floodplain of a creek, the elevation of the floodplain will be raised. As this reduces the channel floodwater capacity, the creek will, over time, seek new, lower paths, forming a meander (a curving sinuous path). The leftover higher locations, typically natural levees at the margins ... [...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] |
