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Ličko Polje (Lika)
Ličko Polje () is a polje (karstic field) in the Lika region, located in Croatia. Being the largest in Croatia, the field covers an area of 465 km2, and consists of five smaller fields: Lipovo, Kosinjsko, Pazariško, Brezovo and Gospićko. The field is characterized by some inselberg An inselberg or monadnock ( ) is an isolated rock hill, knob, ridge, or small mountain that rises abruptly from a gently sloping or virtually level surrounding plain. In Southern Africa, a similar formation of granite is known as a koppie, an ...s, among them Zir (852 m), Otež (745 m) and Debeljak (882 m). The population is engaged in crops and farming. Largest settlement is Gospić. References {{Dinaric Alps' karst fields Plains of Croatia Geology of Croatia ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lika-Senj County
Lika-Senj County (, ) is a county in Croatia that includes most of the Lika region and some northern coastline of the Adriatic near the town of Senj, including the northern part of the Pag island. Its center is Gospić. The county is the least populated (42.469 in 2022) and among the least prosperous ones, though it is the largest county in the country by area and includes the Plitvice Lakes National Park and Sjeverni (North) Velebit National Park, some of Croatia's major tourist attractions. Geography The county has a total area of 5353 km2. Administrative division Lika-Senj County is administratively subdivided into 12 units of local government: * Town of Gospić (county seat) * Town of Novalja * Town of Otočac * Town of Senj * Municipality of Brinje * Municipality of Donji Lapac * Municipality of Karlobag * Municipality of Lovinac * Municipality of Perušić * Municipality of Plitvička Jezera (''Plitvice Lakes'') * Municipality of Udbina * Municipal ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Velebit
Velebit (; ; ) is the largest, though not the highest, mountain range in Croatia. The range forms a part of the Dinaric Alps and is located along the Adriatic coast, separating it from Lika in the interior. Velebit begins in the northwest near Senj with the Vratnik mountain pass and ends 145 km to the southeast near the source of the Zrmanja river northwest of Knin. Its highest peak is the Vaganski vrh at 1,757 m. Major mountain passes on Velebit include the aforementioned Vratnik or Senjsko bilo at 694 m.a.s.l., where the '' Josephina'' connects Senj with Josipdol; Oštarijska vrata at 928 m.a.s.l. that connects Karlobag and Gospić; and Prezid at 766 m.a.s.l. that connects Obrovac and Gračac. Velebit is characterized by its simple, solid form, stiff cliffs, the lack of vegetation on the seaward side (towards the Velebit Channel), and the wood-covered slopes of the Lika side. The basic geological characteristic of the mountains is karst; flora and fauna are abunda ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gospić
Gospić () is a town in Lika, Croatia. It is the seat of the Lika-Senj County. Geography Gospić is located in the mountainous and sparsely populated region of Lika. It is the administrative center of Lika-Senj County. Gospić is located near the Lika River in the middle of a karst field ( Ličko Polje). Municipality * Aleksinica, population 169 * Barlete, population 28 * Bilaj, population 162 * , population 25 * Brušane, population 134 * Budak, population 151 * Bužim, population 74 * Debelo Brdo I, population 61 * Debelo Brdo II, population 8 * Divoselo, population 4 * Donje Pazarište, population 125 * Drenovac Radučki, population 0 * Gospić, population 6,575 * Kalinovača, population 94 * Kaniža Gospićka, population 401 * Klanac, population 100 * Kruščica, population 0 * Kruškovac, population 20 * Kukljić, population 13 * Lički Čitluk, population 4 * Lički Novi, population 298 * Lički Osik, population 1,914 * Lički Ribnik, populatio ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lika (river)
The Lika is a river in Croatia which gives its name to the Lika region. It is long and it has a basin with an area of . Its average discharge at the measurement station in Bilaj (covering 225 km2 of the basin) is 7.33 m3/s, and it can go completely dry. It is known as a sinking river because at the end of its course, it flows into a series of ponors or swallow-holes and disappears from the surface. The Lika River rises near the village of Kukljić at the foot of the Velebit Mountains, flows in a northwesterly direction past the town of Gospić, enters and leaves Lake Krušćica, and continues to the northwest until it sinks into the karst topography Karst () is a topography formed from the dissolution of soluble carbonate rocks such as limestone and Dolomite (rock), dolomite. It is characterized by features like poljes above and drainage systems with sinkholes and caves underground. Ther ... at ponors near Lipovo Polje. Etymology and names The name is mostly likely t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Lika
Lika () is a traditional region of Croatia proper, roughly bound by the Velebit mountain from the southwest and the Plješevica mountain from the northeast. On the north-west end Lika is bounded by Ogulin-Plaški basin, and on the south-east by the Malovan pass. Today most of the territory of Lika (Brinje, Donji Lapac, Gospić, Lovinac, Otočac, Perušić, Plitvička Jezera, Udbina and Vrhovine) is part of Lika-Senj County. Josipdol, Plaški and Saborsko are part of Karlovac County and Gračac is part of Zadar County, and it takes up about 12% of Croatia, Croatia's land area. Major towns include Gospić, Otočac, and Gračac, most of which are located in the karst poljes of the rivers of Lika (river), Lika, Gacka and others. The Plitvice Lakes National Park and Northern Velebit National Park are also in Lika. History Antiquity Since the first millennium BC the region was inhabited by the Iapodes, an ancient people related to Illyrians. During the Gallic invasion of the Balk ... [...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] |
Croatia
Croatia, officially the Republic of Croatia, is a country in Central Europe, Central and Southeast Europe, on the coast of the Adriatic Sea. It borders Slovenia to the northwest, Hungary to the northeast, Serbia to the east, Bosnia and Herzegovina and Montenegro to the southeast, and shares a maritime border with Italy to the west. Its capital and largest city, Zagreb, forms one of the country's Administrative divisions of Croatia, primary subdivisions, with Counties of Croatia, twenty counties. Other major urban centers include Split, Croatia, Split, Rijeka and Osijek. The country spans , and has a population of nearly 3.9 million. The Croats arrived in modern-day Croatia, then part of Illyria, Roman Illyria, in the late 6th century. By the 7th century, they had organized the territory into Duchy of Croatia, two duchies. Croatia was first internationally recognized as independent on 7 June 879 during the reign of Duke Branimir of Croatia, Branimir. Tomislav of Croatia, Tomis ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Croatian Encyclopedia
The ''Croatian Encyclopedia'' () is a Croatian general encyclopedia An encyclopedia is a reference work or compendium providing summaries of knowledge, either general or special, in a particular field or discipline. Encyclopedias are divided into article (publishing), articles or entries that are arranged Alp ... (with the national component), published in 1999–2009 by the Miroslav Krleža Institute of Lexicography. Overview The project began in 1999, and it represents a fifth iteration of the encyclopedic tradition that was established by Mate Ujević's ''Croatian Encyclopedia'', and continued in the '' Encyclopedia of the Lexicographical Institute'', as well as the two editions of its ''General Encyclopedia''. Eleven volumes were published in the period 1999–2009, with a new volume appearing every year. It is named "Croatian" encyclopedia (colloquially ''Croatica'') in the tradition of general-knowledge encyclopedias as ''Britannica''. Online edition The f ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inselberg
An inselberg or monadnock ( ) is an isolated rock hill, knob, ridge, or small mountain that rises abruptly from a gently sloping or virtually level surrounding plain. In Southern Africa, a similar formation of granite is known as a koppie, an Afrikaans word ("little head") from the Dutch diminutive word ''kopje''. If the inselberg is dome-shaped and formed from granite or gneiss, it can also be called a bornhardt, though not all bornhardts are inselbergs. An inselberg results when a body of rock resistant to erosion, such as granite, occurring within a body of softer rocks, is exposed by differential erosion and lowering of the surrounding landscape. Etymology Inselberg The word ''inselberg'' is a loan word from German, and means "island mountain". The term was coined in 1900 by geologist Wilhelm Bornhardt (1864–1946) to describe the abundance of such features found in eastern Africa. At that time, the term applied only to arid landscape features. However, it has ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Plains Of Croatia
In geography, a plain, commonly known as flatland, is a flat expanse of land that generally does not change much in elevation, and is primarily treeless. Plains occur as lowlands along valleys or at the base of mountains, as coastal plains, and as plateaus or Highland, uplands. Plains are one of the major landforms on earth, being present on all continents and covering more than one-third of the world's land area. Plains in many areas are important for agriculture. There are various types of plains and biomes on them. Description A plain or flatland is a flat expanse of land with a layer of grass that generally does not change much in elevation, and is primarily treeless. Plains occur as lowlands along valleys or at the base of mountains, as coastal plains, and as plateaus or Highland, uplands. Plains are one of the major landforms on earth, where they are present on all continents, and cover more than one-third of the world's land area. In a valley, a plain is enclosed on tw ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
