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Miskolc
Miskolc (UK: /ˈmiːʃkɒlts/ MEESH-kolts, US: /ˈmɪʃkoʊlts/ MISH-kohlts; Hungarian: [ˈmiʃkolt͡s] ⓘ; Czech and Slovak: Miškovec; German: Mischkolz; Yiddish: Mishkoltz; Romanian: Mișcolț) is a city in northeastern Hungary, known for its heavy industry. With a population of 143,502 as of 2024, Miskolc is the fourth largest city in Hungary, behind Budapest, Debrecen, and Szeged. It is also the county capital of Borsod-Abaúj-Zemplén and the regional centre of Northern Hungary.
The name derives from Miško, Slavic form of Michael. Miškovec → Miskolc with the same development as Lipovec → Lipólc, Lipóc. The name is associated with the Miskolc clan (also Miskóc or Myscouch, Slovak Miškovec, plural Miškovci) named after the settlement or vice versa. Earliest mentions are que nunc vocatur Miscoucy (around 1200), de Myschouch (1225), Ponyt de genere Myscouch (1230), in Miscovcy (1245).
The city lies at the meeting point of different geographical regions – east of the Bükk mountains, in the valley of the river Sajó and the streams Hejő and Szinva. According to the 2001 Census the city has a total area of 236.68 km2 (91.38 sq mi). The ground level slopes gradually; the difference between the highest and lowest area is about 800 m (2,600 ft).
The lowest areas are the banks of the river Sajó, with an altitude of 110–120 m (360–390 ft). The area belongs to the Great Plain region and is made up of sedimentary rocks. Between the Avas hill and Diósgyőr lies the hilly area of the Lower Bükk (250–300 m or 820–980 ft) consisting of sandstone, marl, clay, layers of coal, from the tertiary period, and volcanic rocks from the Miocene.
The Central Bükk, a gently sloping mountainous area with an altitude between 400 and 600 m (1,300 and 2,000 ft), is situated between Diósgyőr and Lillafüred; the area is made up of limestone, slate, dolomite and other rocks from the Triassic period. The surface was formed mostly by karstic erosions.
The highest area, the 600–900 m (2,000–3,000 ft) high Higher Bükk bore Bükk Highlands begin at Lillafüred. This mostly consists of sea sediments (limestone, slate, dolomite) from the Paleozoic and Mesozoic, and volcanic rocks like diabase and porphyry. Several caves can be found in the area. The city is also known for the lowest temperature ever recorded in Hungary at−35 °C (−31 °F).
Summers are fresh but sometimes warm and humid in Miskolc. Daytime temperatures of 20–30 °C (68–86 °F) or higher are commonplace. Snow and ice are dominant during the winter season. Miskolc receives about 120 centimetres of snowfall annually. Days below freezing and nights below −20 °C (−4 °F) both occur in the winter.
The area has been inhabited since ancient times – archaeological findings date back to the Paleolithic, proving human presence for over 70,000 years [citation needed]. Its first known dwellers were the Cotini, one of the Celtic tribes. The area has been occupied by Hungarians since the "Conquest" in the late 9th century. It was first mentioned by this name around 1210 AD. The Miskóc clan lost their power when King Charles I centralized his power by curbing the power of the oligarchs.
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Miskolc
Miskolc (UK: /ˈmiːʃkɒlts/ MEESH-kolts, US: /ˈmɪʃkoʊlts/ MISH-kohlts; Hungarian: [ˈmiʃkolt͡s] ⓘ; Czech and Slovak: Miškovec; German: Mischkolz; Yiddish: Mishkoltz; Romanian: Mișcolț) is a city in northeastern Hungary, known for its heavy industry. With a population of 143,502 as of 2024, Miskolc is the fourth largest city in Hungary, behind Budapest, Debrecen, and Szeged. It is also the county capital of Borsod-Abaúj-Zemplén and the regional centre of Northern Hungary.
The name derives from Miško, Slavic form of Michael. Miškovec → Miskolc with the same development as Lipovec → Lipólc, Lipóc. The name is associated with the Miskolc clan (also Miskóc or Myscouch, Slovak Miškovec, plural Miškovci) named after the settlement or vice versa. Earliest mentions are que nunc vocatur Miscoucy (around 1200), de Myschouch (1225), Ponyt de genere Myscouch (1230), in Miscovcy (1245).
The city lies at the meeting point of different geographical regions – east of the Bükk mountains, in the valley of the river Sajó and the streams Hejő and Szinva. According to the 2001 Census the city has a total area of 236.68 km2 (91.38 sq mi). The ground level slopes gradually; the difference between the highest and lowest area is about 800 m (2,600 ft).
The lowest areas are the banks of the river Sajó, with an altitude of 110–120 m (360–390 ft). The area belongs to the Great Plain region and is made up of sedimentary rocks. Between the Avas hill and Diósgyőr lies the hilly area of the Lower Bükk (250–300 m or 820–980 ft) consisting of sandstone, marl, clay, layers of coal, from the tertiary period, and volcanic rocks from the Miocene.
The Central Bükk, a gently sloping mountainous area with an altitude between 400 and 600 m (1,300 and 2,000 ft), is situated between Diósgyőr and Lillafüred; the area is made up of limestone, slate, dolomite and other rocks from the Triassic period. The surface was formed mostly by karstic erosions.
The highest area, the 600–900 m (2,000–3,000 ft) high Higher Bükk bore Bükk Highlands begin at Lillafüred. This mostly consists of sea sediments (limestone, slate, dolomite) from the Paleozoic and Mesozoic, and volcanic rocks like diabase and porphyry. Several caves can be found in the area. The city is also known for the lowest temperature ever recorded in Hungary at−35 °C (−31 °F).
Summers are fresh but sometimes warm and humid in Miskolc. Daytime temperatures of 20–30 °C (68–86 °F) or higher are commonplace. Snow and ice are dominant during the winter season. Miskolc receives about 120 centimetres of snowfall annually. Days below freezing and nights below −20 °C (−4 °F) both occur in the winter.
The area has been inhabited since ancient times – archaeological findings date back to the Paleolithic, proving human presence for over 70,000 years [citation needed]. Its first known dwellers were the Cotini, one of the Celtic tribes. The area has been occupied by Hungarians since the "Conquest" in the late 9th century. It was first mentioned by this name around 1210 AD. The Miskóc clan lost their power when King Charles I centralized his power by curbing the power of the oligarchs.
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