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Tripoli, Greece
Tripoli (; ) is a city in the central part of the Peloponnese, in Greece. It is the capital of the Peloponnese region as well as of the regional unit of Arcadia. The homonymous municipality had 44,165 inhabitants in 2021. Etymology In the Middle Ages the place was known as Drobolitsa, Droboltsá, or Dorboglitza, either from the Greek Hydropolitsa, 'Water City' or perhaps from the South Slavic for 'Plain of Oaks'. The association made by 18th- and 19th-century scholars with the idea of the " three cities" (Τρίπολις, τρεις πόλεις "three cities": variously Callia, Dipoena and Nonacris, mentioned by Pausanias without geographical context, or Tegea, Mantineia and Pallantium, or Mouchli, Tegea and Mantineia or Nestani, Mouchli and Thana), were considered paretymologies by G.C. Miles. An Italian geographical atlas of 1687 notes the fort of ''Goriza e Mandi et Dorbogliza''; a subsequent Italian geographical dictionary of 1827 attributes the name Dorbogliza to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Peloponnese (region)
The Peloponnese Region (, ) is a region in southern Greece. It borders Western Greece to the north and Attica to the north-east. The region has an area of about . It covers most of the Peloponnese peninsula, except for the northwestern subregions of Achaea and Elis which belong to Western Greece and a small portion of the Argolid peninsula that is part of Attica. Administration The Peloponnese Region was established in the 1987 administrative reform. With the 2011 Kallikratis plan, its powers and authority were redefined and extended. Along with the Western Greece and Ionian Islands regions, it is supervised by the Decentralized Administration of Peloponnese, Western Greece and the Ionian Islands based at Patras. The region is based at Tripoli and is divided into five regional units (pre-Kallikratis prefectures), * Arcadia, * Argolis, * Corinthia, * Laconia and * Messenia, which are further subdivided into 26 municipalities. The largest city of the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Pyrgos, Elis
Pyrgos () is a city in the northwestern Peloponnese, Greece, capital of the regional unit of Elis (regional unit), Elis and the seat of the Municipality of Pyrgos. The city is located in the middle of a plain, from the Ionian Sea. The river Alfeios flows into sea about south of Pyrgos. The population of the town Pyrgos is 26,052, and of the municipality 45,365 (2021). Pyrgos is west of Olympia, Greece, Olympia, southeast of Amaliada, southwest of Patras and west of Tripoli, Greece, Tripoli. Historical population Municipality The municipality Pyrgos was formed during the 2011 local government reform by the merger of the following 4 former municipalities, that became municipal units: *Iardanos *Oleni *Pyrgos *Volakas, Elis, Volakas The municipality has an area of 456.610 km2, the municipal unit 170.866 km2. Subdivisions The municipal unit of Pyrgos is divided into the following communities (settlements within the communities given in brackets): *Pyrgos (Pyrgos, A ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Continental Climate
Continental climates often have a significant annual variation in temperature (warm to hot summers and cold winters). They tend to occur in central and eastern parts of the three northern-tier continents (North America, Europe, and Asia), typically in the middle latitudes (40 to 55 or 60 degrees north), often within large landmasses, where prevailing winds blow overland bringing some precipitation, and temperatures are not moderated by oceans. Continental climates occur mostly in the Northern Hemisphere due to the large landmasses found there. Most of northeastern China, eastern and southeastern Europe, much of Russia south of the Arctic Circle, central and southeastern Canada, and the central and northeastern United States have this type of climate. Continentality is a measure of the degree to which a region experiences this type of climate. In continental climates, precipitation tends to be moderate in amount, concentrated mostly in the warmer months. Only a few areas—in th ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lake Taka
Lake Taka (Greek: Λίμνη Τάκα) is a temporary lake located in the south of a large basin called “Tripoli-Plateau” in Greece. In the winter, the southern part of the basin often gets flooded, and a lake forms from a large amount of fresh rainwater because of insufficient surface drainage. A wetland biotope quickly develops, and species of water-loving fauna appear. In the hot and dry summer, the lake dries up. Over time, karstification creates several ponors, where water leaves the basin through groundwater. Geography Lake Taka sits at an altitude of 650 meters east of Tegea and ca. 10 km south of Tripoli, Greece, Tripoli, the capital of Arcadia (regional unit), Arcadia. The lake collects rainwater, which comes from the mountains around the basin, called “Tripoli-Plateau” (length ca. 30 km and width between 12.5 and 25 km). In the hot and dry summer season, the temporary lake usually dries totally up (leaving some irrigation water in the dammed p ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mainalo
Mainalo (, ; ) is the tallest mountain in the Menalon highlands of the Peloponnese, and is located in Arcadia. The mountain's highest point, known as both ''Profitis Ilias'' and ''Ostrakina'', at a height of , is the highest point in Arcadia. The mountain has a length of from southwest of Tripoli to northeast of Vytina, and a width of from Zygovisti to Kapsas. The mountain is part of a Natura 2000 site, designated in March 2011, covering an area of . In the 19th and early 20th century, the mountain was known as ''Apano Chrepa''. While the mountain takes its name from the ancient Mount Mainalos, and the ancient city of Maenalus which stood at its summit, modern scholars now identify the location of the ancient mountain as "Ágios Ilías", a mountain further south near the town of Asea. The name was likely mistakenly connected to the mountain now known as Mainalo by earlier European travelers. According to ancient Greek mythology, Mount Mainalos got its name from Maena ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
2011 Greek Census
The 2011 Population and Housing Census (), branded as (), was a population census in Greece conducted by the Hellenic Statistical Authority on behalf of the Greek state between 10 and 24 May 2011. It was conducted as part of the 2011 European Union census. Its purpose was to enumerate the number of people in the country as well as survey the social characteristics of the population. The census was available in 8 languages other than Greek language, Greek: English language, English, Albanian language, Albanian, French language, French, Vietnamese language, Vietnamese, Russian language, Russian, Arabic, Urdu and Dari (Persian), Dari. The final results of the census were announced on 28 December 2012, with a minor correction in 2014. According to final results, the total resident population of Greece was 10,815,197 on census day. There was a margin of error of 2.84%. Scope and format The 2011 census was carried out to ascertain the number of people in Greece at the time of the census ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Polje
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. Geology A polje, in geological terminology, is a large, flat-floored depression within karst limestone, whose long axis develops in parallel with major structural trends and can become several miles (tens of kilometers) long. Superficial deposits tend to accumulate along the floor. Drainage may be either by surface watercourses (as an ''open polje'') or by swallow holes (as a ''closed polje'') or ponors. Usually, the ponors cannot transmit entire flood flows, so many poljes become wet-season lakes. The structure of some poljes is related to the geological structure, but others are purely the result of lateral dissolut ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Köppen Climate Classification
The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indicates a tropical rainforest climate. The system assigns a temperature subgroup for all groups other than those in the ''A'' group, indicated by the third letter for climates in ''B'', ''C'', ''D'', and the second letter for climates in ''E''. Other examples include: ''Cfb'' indicating an oceanic climate with warm summers as indicated by the ending ''b.'', while ''Dwb'' indicates a semi-Monsoon continental climate, monsoonal continental climate ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mediterranean Climate
A Mediterranean climate ( ), also called a dry summer climate, described by Köppen and Trewartha as ''Cs'', is a temperate climate type that occurs in the lower mid-latitudes (normally 30 to 44 north and south latitude). Such climates typically have dry summers and wet winters, with summer conditions being hot and winter conditions typically being mild. These weather conditions are typically experienced in the majority of Mediterranean-climate regions and countries, but remain highly dependent on proximity to the ocean, altitude and geographical location. The dry summer climate is found throughout the warmer middle latitudes, affecting almost exclusively the western portions of continents in relative proximity to the coast. The climate type's name is in reference to the coastal regions of the Mediterranean Sea, which mostly share this type of climate, but it can also be found in the Atlantic portions of Iberia and Northwest Africa, the Pacific portions of the United States ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kingdom Of Greece (Wittelsbach)
The Kingdom of Greece (, romanized: ''Vasíleion tis Elládos'', pronounced ) was the Greek nation-state established in 1832 and was the successor state to the First Hellenic Republic. It was internationally recognised by the Treaty of Constantinople, where Greece also secured its full independence from the Ottoman Empire after nearly four centuries. It remained a Kingdom until 1924, when the Second Hellenic Republic was proclaimed, and from the Republic's collapse in 1935 to its dissolution by the Regime of the Colonels in 1973. A referendum following the regime's collapse in 1974 confirmed the effective dissolution of the monarchy and the creation of the Third Hellenic Republic. For much of its existence, the Kingdom's main ideological goal was the Megali Idea (Greek: Μεγάλη Ιδέα, romanized: Megáli Idéa, lit. 'Great Idea'), which sought to annex lands with predominately Greek populations. King Otto of the House of Wittelsbach ruled as an absolute monarch fro ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ibrahim Pasha Of Egypt
Ibrahim Pasha ( ''Ibrāhīm Bāshā''; 1789 – 10 November 1848) was an Egyptian general and politician; he was the commander of both the Egyptian and Ottoman armies and the eldest son of Muhammad Ali, the Ottoman Wāli and unrecognized Khedive of Egypt and Sudan. He was the second ruler of Egypt from the Muhammad Ali Dynasty and ruled from 20 July 1848 to 10 November 1848. Ibrahim served as a general in the Egyptian army that his father established during his reign, taking his first command of Egyptian forces when he was merely a teenager. In the final year of his life, he was appointed Regent for his still-living father and became the effective ruler of Egypt and Sudan, owing to the latter's ill health. His rule also extended over the other dominions that his father had brought under Egyptian rule, namely Syria, Hejaz, Morea, Thasos, and Crete. Ibrahim pre-deceased his father, dying 10 November 1848, only four months after rising to power. He was succeeded as Regent by his n ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
