Gurio Lamanna | |
---|---|
Location | Gravina in Puglia, Apulia, Italy |
Coordinates | 40°54′32″N16°25′33″E / 40.90885°N 16.425761°E |
Depth | 38 meters (125 ft) [1] |
Length | 900 meters (3,000 ft) [1] |
Geology | Karst |
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" [2] 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" (Italian : 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. [3] The definition of "karst basin", used by Carmelo Colamonico, has been introduced by Renato Biasutti. [4] [5] Carmelo Colamonico stated that Gurio Lamanna is "one of the best examples of karst basin in the Murge plateau". [3]
The doline has an external perimeter of over 3 kilometers (1.9 mi), an average length of 900 meters (3,000 ft) ca. and a maximum depth of 38 meters (125 ft). It covers an area of 68,000 square meters (730,000 sq ft). [1] Its walls have a low steepness compared to the nearby doline Pulicchio di Gravina. The bottom of the doline is flat "like a table"; such a flat expanse of land is very uncommon in the barren and hilly landscape of the Murge region. From this point of view, it may be likened to another large "karst basin", that is the expanse of Pescariello (Altamura), far wider and similarly karst. [1]
The doline includes a sinkhole, into which part of the rainwater collected in its drainage basin flows out.
The whole flat area contains a deep layer of fertile soil, L'intera area piatta contiene un notevole strato di terreno fertile, consequence of the millenary erosion and which is successfully cultivated together with the nearby doline Tre Paduli. Also because of this, the area is different from the stony, arid and difficult to grow Murge region.
During the storms, the water in the doline reaches a relatively high level. This water flows out partly via the sinkhole partly via the porous limestone external walls. The water is absorbed in a very short time, usually a few hours. Water stagnates longer in the central area, which is also the lowest. In this central area, at the time of Carmelo Colamonico (1917), there was a tree and a pit for rainwater, while today there is an open tank used for rainwater. [6]
Close to the doline are the ruins of a small XX century primary school both for children and adults.
The doline (or "karst basin") was practically unknown among scientists and scholars until the first study published by Carmelo Colamonico in 1917. [7] Previously it had been cited only by F. Virgilio (1900), who called it just "Gurio". [8] [9]
Carmelo Colamonico was the first person who called it with its name. He noticed that on the maps of the Italian geographic institute Istituto Geografico Militare of that time the area, comprising a cluster of buildings nearby, was just named Masseria Crocetta, but its real name instead was Masseria Gurio Lamanna. Carmelo Colamonico identified the real nome of the area (Masseria Gurio Lamanna) and first used the term "Gurio Lamanna" to refer to the doline. [8] As a proof of the correctness of Carmelo Colamonico's intuition, the word gurio is used in the Murge region to denote a large and flat sinkhole collecting a large amount of rainwater. [8]
The origin of the karst basin Gurio Lamanna can be explained with karst processes. The water coming from the relative drainage basin has slowly but constantly eroded (according to the usual double action - chemical and mechanical - of rainwater, typical of karst phenomena) the area, leading to the formation of the wide flat area full of fertile soil that is visible today. [2]
Carmelo Colamonico hypothesized that, initially, there may have been a ditch in direction NW-SE caused by tectonic phenomena. Nevertheless, he noticed that today's dimensions would have never been reached if there had not been the double action of rainwater coming from such a large drainage basin (karst). [2]
Rainwater mainly comes from two lamas, one located NW and the other NE. Both of them contribute to the erosion phenomenon, although the NW lama probably contributed (and still contributes) more than the NE lama. The erosion occurred (and still occurs) mainly in the northern direction in the region between the two lamas. [2]
Karst is a topography formed from the dissolution of soluble carbonate rocks such as limestone and dolomite. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. There is some evidence that karst may occur in more weathering-resistant rocks such as quartzite given the right conditions.
A sinkhole is a depression or hole in the ground caused by some form of collapse of the surface layer. The term is sometimes used to refer to doline, enclosed depressions that are also known as shakeholes, and to openings where surface water enters into underground passages known as ponor, swallow hole or swallet. A cenote is a type of sinkhole that exposes groundwater underneath. Sink and stream sink are more general terms for sites that drain surface water, possibly by infiltration into sediment or crumbled rock.
Landforms are categorized by characteristic physical attributes such as their creating process, shape, elevation, slope, orientation, rock exposure, and soil type.
A polje, also called karst polje or karst field, is a large flat plain found in karstic geological regions of the world, with areas usually in the range of 5–400 km2 (2–154 sq mi). The name derives from the Slavic languages, where polje literally means 'field', whereas in English polje specifically refers to a karst plain or karst field.
In geology, a depression is a landform sunken or depressed below the surrounding area. Depressions form by various mechanisms.
Acquaviva delle Fonti is a town and comune of 20,446 inhabitants, in the Metropolitan City of Bari, in Apulia, Italy. Acquaviva is famous for its characteristic red onions, which have been awarded the DOP mark. The main monuments are the Palazzo de Mari, the Co-Cathedral of Sant'Eustachio and the ancient village. The town is located on the Murge plateau at an elevation of 300 metres (980 ft) above sea level, and is 26 kilometres (16 mi) from the Adriatic Sea and Bari, which is the biggest city of the region. The Ionian Sea is more than 45 kilometres (28 mi) to the south.
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The Parco Nazionale dell'Alta Murgia is a national park in Apulia, southern Italy, established in 2004. It lies in the Murgia geographical area, with its headquarters in the town of Gravina in Puglia, and has an area of 677.39 square kilometres. It is part of a larger Special Protection Area established to protect the grass steppe, lesser kestrel's habitat.
The Altopiano delle Murge is a karst topographic plateau of rectangular shape in southern Italy. Most of it lies within Puglia 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'.
Škocjan Caves Regional Park is located in the Škocjan Karst, a vast flat landscape that lies at an elevation between 420 and 450 m in the southeast part of the Karst area. Following its independence, Slovenia committed itself to protecting the Škocjan Caves area; for this reason, it established Škocjan Caves Regional Park and its managing authority, the Škocjan Caves Park Public Service Agency.
The Metropolitan City of Bari is a metropolitan city in the Apulia region of Italy. Its capital is the city of Bari. It replaced the province of Bari and includes the city of Bari and some forty other comuni. It was first created by the reform of local authorities and then established by the Law 56/2014. It has been operative since January 1, 2015.
Cedar Sink is a vertical-walled large depression or sinkhole in the ground, located in Edmonson County, Kentucky and contained within and managed by Mammoth Cave National Park. The sinkhole measures 300 feet (91.4 m) from the top sandstone plateau to the bottom of the sink and was caused by collapse of the surface soil. The landscape is karst topography, which means the region is influenced by the dissolution of soluble rocks. Sinkholes, caves, and dolines typically characterize these underground drainage systems. Cedar Sink has a bottom area of about 7 acres (2.8 ha) and has more fertile soil compared to the ridgetops.
Pulo di Altamura is a doline located on the Murge plateau. It is the largest doline in that region and it is located about 6 kilometers (3.7 mi) 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.
Pulicchio di Gravina is the second-largest doline in the Murge plateau after Pulo di Altamura. It falls into the territory of Gravina in Puglia, located about 10 kilometers (6.2 mi) 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.
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Vito Carmelo Colamonico (Colamonaco) was an Italian geographer, geologist and scholar. His works include studies on some karst dolines and landforms of Italy, such as Pulo di Altamura, Pulicchio di Gravina and Gurio Lamanna.
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