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Salobreña
Salobreña () is a town on the ''Costa Granadina'' in Granada, 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 Moorish 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 fields on each side along the coast and further inland. Another tourist attraction in Salobreña is 'El Peñón' (The Rock), which divides two of Salobreña's five beaches and juts out between Playa La Guardia and Playa de la Charca/Solamar and into the sea. History Geological background At the close of the last glacial maximum, the Motril-Salobreña plain on which Salobreña now stands was not yet land: rather it ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Costa Granadina
Costa Granadina (; "Granadan Coast") is a comarca (Spain), 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. This comarca was established in 2003 by the Government of Andalusia. It is crossed by the N-340 coastal highway that runs southwest–northeast along Spain's Mediterranean Sea, 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 province of Málaga, 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 (Spain), Sierra Nevada range fall to the very edg ... [...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. Geography It stands on the southwestern side of the Sierra Nevada. 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 Mediterranean Sea between Salobreña and Motril after passing through a spectacular gorge between the Lújar and Chaparal mountains. Climate The reservoir was built in 2002. The Guadalfeo monitoring network (5 automatic weather stations) was installed on the river in 2004 to monitor the snow dynamics of the Sierra Mountain. The network is managed by the Andalusian Institute for Earth System Research. The area is worth studying as it is a n ... [...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. There are certain conception about the ''autonomous community of Granada'' being separate from Andalusia. The new autonomous community would consist of the provinces of Granada, Almería and Málaga. The conception has not yet found a response. 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. Oth ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Motril
Motril () is a town and municipality of Spain belonging to the province of Granada, in the autonomous community of Andalusia. The main settlement is located a few kilometers inland, separated from the Port of Motril by the Guadalfeo delta. Motril is the second most populated municipality in the province, with 60,368 inhabitants as of 2016. History Although its exact origins remain unclear, Motril started as a Phoenician enclave, and continued to exist in Roman times. Sugarcane was brought to the area by Arabs as a result of the Muslim conquest of the Iberian Peninsula. The area yielded to the Catholic Monarchs in 1489. The settlements of Pataura (an '' alquería'' featuring irrigated land) and Jolúcar (featuring mainly cattle pasture) belonged to Motril. At the turn of the 16th century its population was still overwhelmingly Muslim, and so King Ferdinand prohibited Christians from living in Motril and ruled that those Christians who owned possessions there were to reloca ... [...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. There are certain conception about the ''autonomous community of Granada'' being separate from Andalusia. The new autonomous community would consist of the provinces of Granada, Almería and Málaga. The conception has not yet found a response. 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. Oth ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Tajo De Los Vados
The Tagus ( ; ; ) is the longest river in the Iberian Peninsula. The river rises in the Montes Universales between Cuenca and Teruel, in mid-eastern Spain, flows , generally westward, and empties into the Atlantic Ocean in Lisbon. Name The river's Latin name is ''Tagus''. While the etymology is unclear, the most probable etymological origin for the hydronym ''Tagus'' is Indo-European *(s)tag- ('to drip'). Geography Source The Tagus River originates at an elevation of 1,593 meters above sea level in a place known as Fuente García, within the municipality of Frías de Albarracín in Teruel, Spain. Its source is located between the Muela de San Juan (1,830 m) and Cerro de San Felipe (1,839 m), in the Sierra de Albarracín, which belongs to the Montes Universales in the western branch of the Iberian System. Course The river flows through Spain for , passing through four autonomous communities (Aragón, Castilla-La Mancha, Madrid, and Extremadura) and a total of six prov ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Phoenicians
Phoenicians were an ancient Semitic group of people who lived in the Phoenician city-states along a coastal strip in the Levant region of the eastern Mediterranean, primarily modern Lebanon and the Syrian coast. They developed a maritime civilization which expanded and contracted throughout history, with the core of their culture stretching from Arwad in modern Syria to Mount Carmel. The Phoenicians extended their cultural influence through trade and colonization throughout the Mediterranean, from Cyprus to the Iberian Peninsula, evidenced by thousands of Phoenician inscriptions. The Phoenicians directly succeeded the Bronze Age Canaanites, continuing their cultural traditions after the decline of most major Mediterranean basin cultures in the Late Bronze Age collapse and into the Iron Age without interruption. They called themselves Canaanites and referred to their land as Canaan, but the territory they occupied was notably smaller than that of Bronze Age Canaan. The name ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bronze Age
The Bronze Age () was a historical period characterised principally by the use of bronze tools and the development of complex urban societies, as well as the adoption of writing in some areas. The Bronze Age is the middle principal period of the three-age system, following the Stone Age and preceding the Iron Age. Conceived as a global era, the Bronze Age follows the Neolithic, with a transition period between the two known as the Chalcolithic. The final decades of the Bronze Age in the Mediterranean basin are often characterised as a period of widespread societal collapse known as the Late Bronze Age collapse (), although its severity and scope are debated among scholars. An ancient civilisation is deemed to be part of the Bronze Age if 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 producing areas elsewhere. Bronze Age cultures were the first to History of writing, develop writin ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Palaeolithic Period
The Paleolithic or Palaeolithic ( years ago) ( ), also called the Old Stone Age (), 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 Hominini, hominins, 3.3 million years ago, to the end of the Pleistocene, 11,650 Before Present#Radiocarbon calibration, cal Before Present, 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 band society, bands and subsisted by gathering plants, fishing, and hunting or scavenging wild animals. The Paleolithic Age is characterized by the use of Knapping, knapped stone tools, although at the time humans also used wood and bone tools. Other organic commodities were adapted for ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Neolithic Period
The Neolithic or New Stone Age (from Greek 'new' and 'stone') is an archaeological period, the final division of the Stone Age in Mesopotamia, Asia, Europe and Africa (c. 10,000 BCE to c. 2,000 BCE). 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. The term 'Neolithic' was coined by Sir John Lubbock in 1865 as a refinement of the three-age system. The Neolithic began about 12,000 years ago, when farming appeared in the Epipalaeolithic Near East and Mesopotamia, and later in other parts of the world. It lasted in the Near East until the transitional period of the Chalcolithic (Copper Age) from about 6,500 years ago (4500 BCE), marked by the development of metallurgy, leading up to the Bronze Age and Iron Age. In other places, th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Alluvial Plain
An alluvial plain is a plain (an essentially flat landform) created by the deposition of sediment over a long period 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 time. In contrast, 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 curved path). The leftover higher locations, typically natural levees at the margins of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
