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Pulo Di Molfetta
Pulo di Molfetta is a doline located on the Murge plateau, in Apulia, southern Italy, around south-west of the city of Molfetta. It originated due to the collapse of the ceiling of one or more caves. It shares the local toponym ''pulo'' with other large dolines of the region, i.e. ''Pulicchio di Gravina'', ''Pulo di Molfetta'' and ''Pulicchio di Toritto''. See also * Pulo di Altamura * Pulicchio di Gravina * Gurio Lamanna * Molfetta Molfetta (; Molfettese: ) is a town located in the northern side of the Metropolitan City of Bari, Apulia, southern Italy. It has a well restored old city, and its own dialect. History The earliest local signs of permanent habitation are a ... Sources * {{Cite book, title=Storie inedite della città di Altamura , first=Tommaso , last=Berloco , year=1985 , publisher=ATA - Associazione Turistica Altamurana Pro Loco , url=https://www.scribd.com/document/371395521/Tommaso-Berloco-Storie-inedite-della-citta-di-Altamura , ref=storie-inedite ...
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Molfetta
Molfetta (; Molfettese: ) is a town located in the northern side of the Metropolitan City of Bari, Apulia, southern Italy. It has a well restored old city, and its own dialect. History The earliest local signs of permanent habitation are at the Neolithic site of Pulo, one of the most important such sites in southern Italy. The origins of the city can be traced to a small fishing port; antique graves testify to a fisherman's village in the fourth century BC. The position of the future city offered a valid landing to the commerce of Roman Rubo. The first indication of a toponym on the coast between ''Turenum'' (Trani) and ''Natiolum'' (Giovinazzo) is in the '' Itinerarium Provinciarum Antonini Augusti'', edited from a third-century core. The place denominated ''Respa'' was probably a wrong transcript of the toponym ''Melpha'', referring to a small village of fishermen. The first official document that mentions the city dates to November 925; it documents a ''civitas'' denomina ...
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Apulia
it, Pugliese , population_note = , population_blank1_title = , population_blank1 = , demographics_type1 = , demographics1_footnotes = , demographics1_title1 = , demographics1_info1 = , demographics1_title2 = , demographics1_info2 = , demographics1_title3 = , demographics1_info3 = , timezone1 = CET , utc_offset1 = +01:00 , timezone1_DST = CEST , utc_offset1_DST = +02:00 , postal_code_type = , postal_code = , area_code_type = ISO 3166 code , area_code = IT-75 , blank_name_sec1 = GDP (nominal) , blank_info_sec1 = €76.6 billion (2018) , blank1_name_sec1 = GDP per capita , blank1_info_sec1 = €19,000 (2018) , blank2_name_sec1 = HDI (2018) , blank2_info_sec1 = 0.845 · 18th of 21 , blank_name_sec2 = NUTS Region , blank_info_sec2 = ...
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Italy
Italy ( it, Italia ), officially the Italian Republic, ) or the Republic of Italy, is a country in Southern Europe. It is located in the middle of the Mediterranean Sea, and its territory largely coincides with the homonymous geographical region. Italy is also considered part of Western Europe, and shares land borders with France, Switzerland, Austria, Slovenia and the enclaved microstates of Vatican City and San Marino. It has a territorial exclave in Switzerland, Campione. Italy covers an area of , with a population of over 60 million. It is the third-most populous member state of the European Union, the sixth-most populous country in Europe, and the tenth-largest country in the continent by land area. Italy's capital and largest city is Rome. Italy was the native place of many civilizations such as the Italic peoples and the Etruscans, while due to its central geographic location in Southern Europe and the Mediterranean, the country has also historically been home ...
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Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ...
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Murge
The Altopiano delle Murge (Italian for "Murge plateau") is a karst topographic plateau of rectangular shape in southern Italy. Most of it lies within Apulia and corresponds with the sub-region known as Murgia or Le Murge. The plateau lies mainly in the Metropolitan City of Bari and the province of Barletta-Andria-Trani, but extends into the provinces of Brindisi and Taranto to the south, and into Matera in Basilicata to the west. The name is believed to originate from the Latin ''murex'', meaning "sharp stone". Geography and geology The Murge plateau covers a surface of some 4,000 km², bordered by the Ofanto river and the Tavoliere delle Puglie to the north, the Adriatic Sea to the northeast, and by the Messapic depression, which separates it from the Salento peninsula, to the south. It is usually divided into Alta Murgia (High Murgia), the highest area, with poorer vegetation, and Bassa Murgia (Lower Murgia), with more fertile land, extensively planted with olive-tre ...
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Pulo Di Altamura
Pulo di Altamura is a doline located on the Murge plateau ( Apulia, Italy). It is the largest doline in that region and it is located about north-west of the city of Altamura. It shares the local toponym ''pulo'' with other large dolines of the region, i.e. ''Pulicchio di Gravina'', ''Pulo di Molfetta'' and ''Pulicchio di Toritto''. Dimensions The perimeter, measured on the edge of the doline, is around . The larger diameter is abit bigger than and it is never lower than . The depth is around . Etymology The etymology of toponym ''pulo'' is currently unknown. It is used only in the Murge plateau to denote a doline, while it is unused in other regions of Apulia. The term is also used for the nearby dolines Pulo di Molfetta, Pulicchio di Gravina and Pulicchio di Toritto (''pulicchio'' means small ''pulo''), and it is attested as early as in the 17th century, since Domenico Santoro in 1688 wrote "luogo detto dalli Cittadini lo Pulo" (place called by Altamura people 'Pulo') ...
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Pulicchio Di Gravina
Pulicchio di Gravina (in the local dialect ''Pulícchie'' or ''Pulidde'') is the second-largest doline in the Murge plateau (in Apulia, southern Italy) after Pulo di Altamura. It falls into the territory of Gravina in Puglia, being located about north of the latter, close to the border with Altamura's territory. It shares the local toponym ''pulo'' with other large dolines of the region, i.e. Pulo di Altamura, Pulo di Molfetta and Pulicchio di Toritto. The doline is very close to other two karst landforms, Gurio Lamanna and Tre Paduli. Dimensions The doline is shaped like an egg and it is highly regular, with the slope almost constant on all its sides (as shown on the map's level curves). The biggest length (in direction NNW-SE) is equal to . The doline is somewhat wider in the northern part () than in the southern part (). Its perimeter is approximately , while the maximum depth is . The lowest point has height from the sea level. Therefore, the doline turns out to be ...
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Gurio Lamanna
Gurio Lamanna (also incorrectly called Gurlamanna) is a doline shaped like a coat of arms located in the Murge plateau and falling into Gravina in Puglia's territory, on the border with Altamura, Apulia, southern Italy. It is "one of the largest karst landforms of the Murge plateau" C. Colamonico (1917), p. 21 and it is located very close to other two dolines, namely Pulicchio di Gravina and Tre Paduli. Depending on the type of geomorphologic classification employed and the author who suggested it, the karst landform can be defined either a doline or a "karst basin" ( it, bacino carsico). It is traditionally called "karst basin", following the suggestion of Carmelo Colamonico, who first studied the doline and saw in its large size and shallow depth a good reason to distinguish it from a normal doline. C. Colamonico (1917), p. 22 The definition of "karst basin", used by Carmelo Colamonico, has been introduced by Renato Biasutti. Carmelo Colamonico stated that Gurio Lamanna i ...
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Karst
Karst is a topography formed from the dissolution of soluble rocks such as limestone, dolomite, and gypsum. It is characterized by underground drainage systems with sinkholes and caves. It has also been documented for more weathering-resistant rocks, such as quartzite, given the right conditions. Subterranean drainage may limit surface water, with few to no rivers or lakes. However, in regions where the dissolved bedrock is covered (perhaps by debris) or confined by one or more superimposed non-soluble rock strata, distinctive karst features may occur only at subsurface levels and can be totally missing above ground. The study of ''paleokarst'' (buried karst in the stratigraphic column) is important in petroleum geology because as much as 50% of the world's hydrocarbon reserves are hosted in carbonate rock, and much of this is found in porous karst systems. Etymology The English word ''karst'' was borrowed from German in the late 19th century, which entered German much earlier ...
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Landforms Of Apulia
A landform is a natural or anthropogenic land feature on the solid surface of the Earth or other planetary body. Landforms together make up a given terrain, and their arrangement in the landscape is known as topography. Landforms include hills, mountains, canyons, and valleys, as well as shoreline features such as bays, peninsulas, and seas, including submerged features such as mid-ocean ridges, volcanoes, and the great ocean basins. Physical characteristics Landforms are categorized by characteristic physical attributes such as elevation, slope, orientation, stratification, rock exposure and soil type. Gross physical features or landforms include intuitive elements such as berms, mounds, hills, ridges, cliffs, valleys, rivers, peninsulas, volcanoes, and numerous other structural and size-scaled (e.g. ponds vs. lakes, hills vs. mountains) elements including various kinds of inland and oceanic waterbodies and sub-surface features. Mountains, hills, plateaux, and plains are the fo ...
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