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1898 Trilj Earthquake
The 1898 Trilj earthquake occurred on Saturday, July 2, 1898, near the town of Trilj in the then-Kingdom of Dalmatia, Austria-Hungary, with the moment magnitude of 6.7. The estimated intensity at the epicenter was VIII–IX on the Medvedev–Sponheuer–Karnik scale. It is one of the strongest earthquakes in Croatian history. This is also the first time an earthquake in Croatia were recorded by seismographs at Italian, German, British, Ukrainian, Russian and Slovenian seismic stations. Background The region of Dalmatia saw many large earthquake in the last 200 years as it lies on a convergent boundary region between Africa and Eurasia. Regional plate tectonics are complex, and involve the motions of numerous microplates and regional-scale structures. The Adriatic block immediately west of the earthquake is thought to move somewhat independently to Eurasia and Africa, driving surrounding faulting in Italy and along the eastern Adriatic coast from Croatia to Albania. Several large e ...
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Trilj
Trilj (, it, Treglia, la, Pons Tiluri) is a municipality and town in inland Dalmatia, Croatia. It is located northeast of Split. Population The total population of the municipality is 9,109, with 2,076 in Trilj itself and the rest in small villages. The list of settlements is as follows: * Bisko, population 395 * Budimir, population 106 * Čačvina, population 93 * Čaporice, population 389 * Gardun, population 83 * Grab, population 546 * Jabuka, population 306 * Kamensko, population 107 * Košute, population 1,740 * Krivodol, population 2 * Ljut, population 5 * , population 139 * Podi, population 13 * Rože, population 32 * Strizirep, population 31 * Strmendolac, population 181 * Tijarica, population 374 * Trilj, population 2,076 * Ugljane, population 398 * Vedrine, population 851 * Velić, population 288 * Vinine, population 24 * Vojnić Sinjski, population 577 * Voštane, population 42 * Vrabač, population 218 * Vrpolje, population 93 History In the ar ...
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Earthquakes In Croatia
An earthquake (also known as a quake, tremor or temblor) is the shaking of the surface of the Earth resulting from a sudden release of energy in the Earth's lithosphere that creates seismic waves. Earthquakes can range in intensity, from those that are so weak that they cannot be felt, to those violent enough to propel objects and people into the air, damage critical infrastructure, and wreak destruction across entire cities. The seismic activity of an area is the frequency, type, and size of earthquakes experienced over a particular time period. The seismicity at a particular location in the Earth is the average rate of seismic energy release per unit volume. The word ''tremor'' is also used for non-earthquake seismic rumbling. At the Earth's surface, earthquakes manifest themselves by shaking and displacing or disrupting the ground. When the epicenter of a large earthquake is located offshore, the seabed may be displaced sufficiently to cause a tsunami. Earthquakes c ...
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List Of Earthquakes In Croatia
This incomplete list of earthquakes in Croatia includes major earthquakes with epicenters within the country's current borders, as well as earthquakes that had a significant impact within Croatia. There was no systematic gathering of earthquake data in Croatia before the 19th century. The magnitudes and epicenters of earlier earthquakes cannot be reliably determined, although some estimates exist. Following the 1963 Skopje earthquake, SFR Yugoslavia, of which SR Croatia was a part of, implemented its first Code for Construction in Seismic Regions in 1964. Earthquakes See also * List of earthquakes in Italy * List of earthquakes in Slovenia * List of earthquakes in Balkan ** List of earthquakes in Bosnia and Herzegovina ** List of earthquakes in Albania References Bibliography * * * * * * External links

* {{Europe topic, List of earthquakes in Earthquakes in Croatia, * Lists of earthquakes by country, Croatia Lists of events in Croatia, Earthquakes ...
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Landslide
Landslides, also known as landslips, are several forms of mass wasting that may include a wide range of ground movements, such as rockfalls, deep-seated grade (slope), slope failures, mudflows, and debris flows. Landslides occur in a variety of environments, characterized by either steep or gentle slope gradients, from mountain ranges to coastal cliffs or even underwater, in which case they are called submarine landslides. Gravity is the primary driving force for a landslide to occur, but there are other factors affecting slope stability that produce specific conditions that make a slope prone to failure. In many cases, the landslide is triggered by a specific event (such as a heavy rainfall, an earthquake, a slope cut to build a road, and many others), although this is not always identifiable. Causes Landslides occur when the slope (or a portion of it) undergoes some processes that change its condition from stable to unstable. This is essentially due to a decrease in the She ...
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Vojnić
Vojnić ( sr-Cyrl, Војнић) is a municipality in Karlovac County, Croatia. There are 4,764 inhabitants, 45% of whom are Serbs and 37% of whom are Croats. The municipality is part of Kordun. Vojnić is underdeveloped municipality which is statistically classified as the First Category Area of Special State Concern by the Government of Croatia. Languages and names On the territory of Vojnić municipality, along with Croatian which is official in the whole country, as a second official language has been introduced Serbian language and Serbian Cyrillic alphabet. Demographics In 1991 the municipality of Vojnić had a population of 8,236. 7,366 (89.43%) were Serbs, 436 (5.29%) were Muslims, 116 (1.40%) were Croats and 318 (3.86%) were others. According to the 2011 census, the municipality consists of 46 settlements: * Brdo Utinjsko, population 73 * Bukovica Utinjska, population 80 * Donja Brusovača, population 122 * Dunjak, population 39 * Džaperovac, population 12 ...
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Gardun
Gardun is a village at the top of the hill of Gardun, just 1 km south of Trilj. In the 1997, excavations of the remains of legionary fortress of Tilurium started on the southern outskirts of the village. Tilurium guarded the entrance to the Cetina valley from the south and the approach to the provincial capital at Salona Salona ( grc, Σάλωνα) was an ancient city and the capital of the Roman province of Dalmatia. Salona is located in the modern town of Solin, next to Split, in Croatia. Salona was founded in the 3rd century BC and was mostly destroyed in t ....Smith, D., Gaffney, V., Grossman, D., Howard, A.J., Milosevic, A., Ostir, K., Podobnikar, T., Smith, W., Tetlow, E., Tingle, M., and Tinsley, H. 2006. Assessing the later prehistoric environmental archaeology and landscape development of the Cetina Valley, Croatia. ''Environmental Archaeology'' 11 (2): 171-186 References {{coord, 43.6117, N, 16.7181, E, source:hrwiki_region:HR, format=dms, display=title ...
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1667 Dubrovnik Earthquake
The 1667 Dubrovnik earthquake was one of the three most devastating earthquakes to hit what is now modern Croatia in the last 2,400 years, since records began. The entire city was almost destroyed and around 3,000 to 5,000 people were killed. The city's Rector Simone Ghetaldi was killed and over three quarters of all public buildings were destroyed. At the time, Dubrovnik was the capital of the Republic of Ragusa. The earthquake marked the beginning of the end of the Republic. Tectonic setting Dubrovnik's region is located in the eastern part of the Adriatic Sea and is a narrow strip of land, dotted by a series of bays, with the Dinaric Alps in the background, and hundreds of islands along the coast. The city of Dubrovnik was built in the most seismically active area in Croatia, which makes earthquakes the strongest in the whole country. It is the only Croatian town that is shown in red on the seismic map, which means that it is exposed to potential hazard of the strongest earth ...
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Kingdom Of Dalmatia
The Kingdom of Dalmatia ( hr, Kraljevina Dalmacija; german: Königreich Dalmatien; it, Regno di Dalmazia) was a crown land of the Austrian Empire (1815–1867) and the Cisleithanian half of Austria-Hungary (1867–1918). It encompassed the entirety of the region of Dalmatia, with its capital at Zadar. History The Habsburg monarchy had annexed the lands of Dalmatia after the Napoleonic War of the First Coalition: when Napoleon Bonaparte launched his Italian Campaign into the Habsburg duchies of Milan and Mantua in 1796, culminating in the Siege of Mantua, he compelled Emperor Francis II to make peace. In 1797 the Treaty of Campo Formio was signed, whereby the Habsburg emperor renounced possession of the Austrian Netherlands and officially recognized the independence of the Italian Cisalpine Republic. In turn, Napoleon ceded to him the possessions of the Republic of Venice, including the Dalmatian coast (Venetian Dalmatia) and the Bay of Kotor (Venetian Albania). ''La Sereniss ...
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1962 Makarska Earthquake
The 1962 Makarska earthquakes occurred on January 7 to January 11 near the towns of Podgora and Makarska in Dalmatia, Croatia (at the time part of SFR Yugoslavia). The event is what is known as a doublet earthquake where there are two or more mainshocks occurring in a short span of time. The two earthquake measured 6.2 on the moment magnitude scale. The first tremor was assigned VIII (''Severe''), and the second event IX (''Violent'') on the Modified Mercalli intensity scale. The earthquakes killed a total of 6 people, and caused damage to vulnerable structures. A tsunami may have been triggered by the quakes according to nearby tide gauges. Geological location Dalmatia, the southern part of Croatia, is located in a tectonic thrust zone in the Adriatic basin with the African and Eurasian plates colliding within it. However, some believe that the entirety of the Adriatic lies in a separate micro-plate known as the Apulia-Adriatic micro-plate that moves northeast into the Swiss ...
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Plate Tectonics
Plate tectonics (from the la, label=Late Latin, tectonicus, from the grc, τεκτονικός, lit=pertaining to building) is the generally accepted scientific theory that considers the Earth's lithosphere to comprise a number of large tectonic plates which have been slowly moving since about 3.4 billion years ago. The model builds on the concept of ''continental drift'', an idea developed during the first decades of the 20th century. Plate tectonics came to be generally accepted by geoscientists after seafloor spreading was validated in the mid to late 1960s. Earth's lithosphere, which is the rigid outermost shell of the planet (the crust and upper mantle), is broken into seven or eight major plates (depending on how they are defined) and many minor plates or "platelets". Where the plates meet, their relative motion determines the type of plate boundary: '' convergent'', '' divergent'', or ''transform''. Earthquakes, volcanic activity, mountain-building, and oceanic tr ...
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