2002 Kosovo Earthquake
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2002 Kosovo Earthquake
The 2002 Gjilan earthquake was a 5.7 magnitude earthquake that occurred on April 24, 2002 at 12:51:50 p.m. CET. This earthquake had a Mercalli intensity of VII (''Very Strong''). It occurred at a depth of 10 km, causing very strong shaking across much of Gjilan, moderate shaking in some parts in Ferizaj, and light tremors across Kosovo, and some tremors across neighboring parts of Kosovo. Earthquake The earthquake was one of the strongest earthquake to hit Kosovo in many years. The epicenter was 2 km south of Gjilan, and its hypocenter was 10 km deep. In the area close to the epicenter, the greatest recorded Mercalli intensity for the DYFI map (Did You Feel It?) was VIII (Severe). Impact According to The Irish Times, a man died and at least 100 people were injured. The dead man was Mehmet Salibichaj, a local barber from Gjilan. The earthquake caused damage to homes, shops etc. The earthquake lasted 15 seconds, and many stayed in shelters. Power Outages and br ...
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Central European Time
Central European Time (CET) is a standard time which is 1 hour ahead of Coordinated Universal Time (UTC). The time offset from UTC can be written as UTC+01:00. It is used in most parts of Europe and in a few North African countries. CET is also known as Middle European Time (MET, German: MEZ) and by colloquial names such as Amsterdam Time, Berlin Time, Brussels Time, Madrid Time, Paris Time, Rome Time, Warsaw Time or even Romance Standard Time (RST). The 15th meridian east is the central axis for UTC+01:00 in the world system of time zones. As of 2011, all member states of the European Union observe summer time (daylight saving time), from the last Sunday in March to the last Sunday in October. States within the CET area switch to Central European Summer Time (CEST, UTC+02:00) for the summer. In Africa, UTC+01:00 is called West Africa Time (WAT), where it is used by several countries, year round. Algeria, Morocco, and Tunisia also refer to it as ''Central European ...
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Mainshock
In seismology, the mainshock is the largest earthquake in a sequence, sometimes preceded by one or more foreshocks, and almost always followed by many aftershocks. Foreshock A foreshock is an earthquake that occurs before a larger seismic event (the mainshock) and is related to it in both time and space. The designation of an earthquake as ''foreshock'', ''mainshock'' or aftershock is only possible after the full sequence of events has happened. Aftershock In seismology, an aftershock is a smaller earthquake that follows a larger earthquake, in the same area of the main shock, caused as the displaced crust adjusts to the effects of the main shock. Large earthquakes can have hundreds to thousands of instrumentally detectable aftershocks, which steadily decrease in magnitude and frequency according to known laws. In some earthquakes the main rupture happens in two or more steps, resulting in multiple main shocks. These are known as doublet earthquakes, and in general can b ...
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Geology Of Kosovo
The geology of Kosovo includes a variety of different tectonic and stratigraphic features. Geologic history, stratigraphy and tectonics *Kacanik Flysch *Vrska Cuka granite: An example of Carpatho-Balkan units. Early Paleozoic granites followed by a gap in the Aptian and pelagic clastic rocks from the Cretaceous. *Novo Brdo area: Part of the Central Vardar zone. Situated south of a highly tectonized domain. Novo Brdo schist formed in the Triassic in a volcano-sedimentary basin. *Brezovica harzburgite. References

Geology of Kosovo, {{geology-stub ...
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Earthquakes In Europe
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 Episodic tremor and slip, 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 ...
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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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List Of Earthquakes In Albania
This is an incomplete list of earthquakes in Albania. See also * Geology of Albania * List of earthquakes in Greece * List of earthquakes in Croatia * List of earthquakes in Italy * List of earthquakes in 2019 References

{{Europe topic, List of earthquakes in Lists of earthquakes by country, Albania Earthquakes in Albania, Lists of events in Albania, Earthquakes ...
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List Of Earthquakes In Kosovo
This is an incomplete list of earthquakes in Kosovo. Kosovo is a country with relatively high seismic activity in the Balkan Peninsula. In different periods Kosovo has faced small and large earthquakes. Since the establishment of Kosovo Seismological Survey in 2008 there have been 901 earthquakes in Kosovo with a magnitude of 1.5 and up to 5.2 on the Richter scale. References {{Europe topic, List of earthquakes in Kosovo earthquakes Earthquakes 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 ...
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List Of Earthquakes In 2002
This is a list of earthquakes in 2002. Only earthquakes of magnitude 6 or above are included, unless they result in damage and/or casualties, or are notable for some other reason. All dates are listed according to UTC time. Compared to other years Overall By death toll * Note: At least 10 casualties By magnitude * Note: At least 7.0 magnitude By month January *A magnitude 6.0 earthquake struck Pacific-Antarctic Ridge, on January 1 at a depth of . * A magnitude 6.3 struck Mindanao, on January 1 at a depth of . * A magnitude 6.2 struck Fiji islands, on January 2 at a depth of . * A magnitude 7.2 struck Vanuatu, on January 2 at a depth of . * A magnitude 6.2 struck Hindu Kush, on January 3 at a depth of . * A magnitude 6.6 struck Vanuatu, on January 3 at a depth of . * A magnitude 5.3 struck Tajikistan, on January 9 at a depth of . Killing 3 people * A magnitude 6.7 struck near the north coast of New Guinea, on January 10 at a depth of , Killing 1 Person. * A magnitude ...
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Aftershock
In seismology, an aftershock is a smaller earthquake that follows a larger earthquake, in the same area of the main shock, caused as the displaced crust adjusts to the effects of the main shock. Large earthquakes can have hundreds to thousands of instrumentally detectable aftershocks, which steadily decrease in magnitude and frequency according to a consistent pattern. In some earthquakes the main rupture happens in two or more steps, resulting in multiple main shocks. These are known as doublet earthquakes, and in general can be distinguished from aftershocks in having similar magnitudes and nearly identical seismic waveforms. Distribution of aftershocks Most aftershocks are located over the full area of fault rupture and either occur along the fault plane itself or along other faults within the volume affected by the strain associated with the main shock. Typically, aftershocks are found up to a distance equal to the rupture length away from the fault plane. The pattern ...
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Gjilan
Gjilan, or Gnjilane ( sr-cyr, Гњилане) is the eighth largest city in Kosovo and seat of Gjilan Municipality and Gjilan District. Name Ottoman chronicler Evliya Çelebi mentions ''Morava'' as a settlement of the Sanjak of Vučitrn. Çelebi writes that: "The seventeen day journey from Constantinople (Istanbul) to pass through Vranje, Novo Brdo, Kriva Reka (Egridere) and Morava (Gjilan). The etymology of Gjilan is disputed. Albanian sources claim that the town (initially a village) obtained its name from Bahti Beg Gjinolli of Gjinaj clan that ruled the region of Vushtrri ( Llap and Drenica), and populated this area in the 18th century (around 1750). History In 1342, a place called Morava was visited by Serbian King Stefan Dušan (later Emperor, r. 1331–1355).Kostić 1922, p. 126 A fort was built nearby in the 14th century. Gornja Morava ("Upper Morava") was known as simply Morava under Ottoman rule, and it extended west of the Upper Žegra–Budriga–Cern ...
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