Medgidia
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Medgidia

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Medgidia

Medgidia (Romanian pronunciation: [med͡ʒiˈdi.a] or [med.d͡ʒiˈdi.a]; historical Turkish names: Karasu or Carasu, Mecidiye or Megidie) is a city in Constanța County, Northern Dobruja, south-eastern Romania.

Archaeological findings show that Dobruja was inhabited since the Neolithic period. Starting with 46 BC the region was administered by the Roman Empire. A castrum was built in the Carasu Valley, becoming the cradle of the settlement.

In 1417, the Turks invaded Dobruja. From the 15th century onwards, the region started to be colonized with a Muslim population. The settlement named "Karasu" (Turkish for "Black Water") was mentioned on the map of Iehuda ben Zara in 1497, in the notes of Paolo Giorgio (1590) and Evliya Çelebi (1653).

Modern Medgidia was built by the Ottoman administration on the place of the old Karasu beginning with 1856. It was built as a planned city to accommodate refugees from the Crimean War and to serve as an economic hub for the central zone of Dobruja. The town was named in honour of the sultan Abdülmecid I, the Ottoman sovereign of the period.

After the Russo-Turkish War of 1877–1878, Northern Dobruja became part of Romania. Medgidia was the last capital of Silistra Nouă County (1878–1879) before it was merged into Constanța County.

Medgidia is located between the Danube and the Black Sea, 39 km (24 mi) away from Constanța. The city is crossed by the Danube–Black Sea Canal west to east; the river Medgidia discharges into the Canal in Remus Opreanu village.

The general aspect of the relief is that of a low plateau with a limestone structure, covered with thick deposits of loess. The natural resources in the area consist of limestone deposits and kaolin sand. The limestone structure of the earth permits a natural filtering of the groundwater.

Medgidia features a semi-arid temperate continental climate, determined by its inland location within the Southern Dobruja Plateau and central Constanța County. The local climate exhibits a pronounced continentality, characterized by wide annual temperature variations and highly variable precipitation patterns. Due to low cloud cover and high solar radiation, the municipality experiences high rates of evapotranspiration, which frequently outstrip precipitation and result in a net moisture deficit. Extreme temperatures range from 41.1 °C in July 2007 to -23.0 °C in February 1954.

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