A microearthquake (or microquake) is a very low intensity earthquake which is 2.0 or less in magnitude. They are very rarely felt beyond 8 km (5 mi) from their epicenter. In addition to having natural tectonic causes, they may also be seen as a result of underground nuclear testing or even large detonations of conventional explosives for producing excavations. They normally cause no damage to life or property, and are very rarely felt by people.
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| - Μικροσεισμός (el)
- Gempa mikro (in)
- 微小地震 (ja)
- 미소지진 (ko)
- Microearthquake (en)
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| - Gempa mikro adalah gempa bumi yang memiliki nilai magnitudo kecil (kurang dari 2 SR). Gempa bumi ini hanya dapat dirasakan oleh orang-orang yang berada dalam radius 8 kilometer. Gempa mikro sering terjadi pada reservoir geotermal yang dipicu oleh terbentuknya rekahan pada batuan reservoir ketika dilakukan injeksi fluida. Sehingga gempa mikro dapat digolongkan sebagai induced earthquakes. (in)
- 미소지진(Microearthquake)이란 규모 2.0 이하의 매우 작은 크기의 지진을 의미한다. 미소지진의 경우에는 진앙에서 약 8 km 이상 떨어진 곳에서는 거의 느낄 수 없다. 미소지진은 자연적인 판 구조론적 원인 외에도 지하 핵실험이나 발파를 위한 재래식 폭발 등 인공지진으로도 발생할 수 있다. 미소지진은 거의 대부분 인간의 생명이나 재산에 큰 피해를 주지 않으며 사람들도 거의 느끼지 못한다. 예외적으로 2011년 10월 7일 7시 20분 일본 도야마현 동부 지진(최대진도 1)의 경우 규모 Mj2.4의 미소지진이었으나 당시 산사태로 인한 낙석으로 1명이 사망하였고 일본에서 가장 작은 규모로 사망자가 발생한 지진으로 기록되었다. 미소지진은 화산 분화가 가까운 화산의 화구 인근에서 잘 발생하며, 화산성 지진의 일종으로 미소지진이 발생하기도 한다. (ko)
- Μικροσεισμός λέγεται ο πολύ χαμηλής έντασης σεισμός ο οποίος μπορεί να είναι 2,0 ή λιγότερο σε μέγεθος. Είναι πολύ σπάνια αισθητός πέρα από 8 χλμ από το επίκεντρο του. Εκτός από να έχει φυσικά τεκτονικά αίτια, μπορεί να θεωρηθεί αποτέλεσμα υπόγειας πυρηνικής δοκιμής ή ακόμη και από μεγάλες εκρήξεις συμβατικών εκρηκτικών σε εκσκαφές. Συνήθως δεν προκαλεί απώλειες από ζωές ή καταστροφές κτιρίων και πολύ σπάνια τον αισθάνεται ο άνθρωπος. (el)
- A microearthquake (or microquake) is a very low intensity earthquake which is 2.0 or less in magnitude. They are very rarely felt beyond 8 km (5 mi) from their epicenter. In addition to having natural tectonic causes, they may also be seen as a result of underground nuclear testing or even large detonations of conventional explosives for producing excavations. They normally cause no damage to life or property, and are very rarely felt by people. (en)
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| - Μικροσεισμός λέγεται ο πολύ χαμηλής έντασης σεισμός ο οποίος μπορεί να είναι 2,0 ή λιγότερο σε μέγεθος. Είναι πολύ σπάνια αισθητός πέρα από 8 χλμ από το επίκεντρο του. Εκτός από να έχει φυσικά τεκτονικά αίτια, μπορεί να θεωρηθεί αποτέλεσμα υπόγειας πυρηνικής δοκιμής ή ακόμη και από μεγάλες εκρήξεις συμβατικών εκρηκτικών σε εκσκαφές. Συνήθως δεν προκαλεί απώλειες από ζωές ή καταστροφές κτιρίων και πολύ σπάνια τον αισθάνεται ο άνθρωπος. Μικροσεισμοί συμβαίνουν συχνά κοντά σε ηφαίστεια καθώς πλησιάζει η έκρηξη τους και σε ορισμένες περιοχές εκμετάλλευσης για τη γεωθερμική ενέργεια, όπως κοντά στο στη . (el)
- A microearthquake (or microquake) is a very low intensity earthquake which is 2.0 or less in magnitude. They are very rarely felt beyond 8 km (5 mi) from their epicenter. In addition to having natural tectonic causes, they may also be seen as a result of underground nuclear testing or even large detonations of conventional explosives for producing excavations. They normally cause no damage to life or property, and are very rarely felt by people. Microquakes occur often near volcanoes as they approach an eruption, and frequently in certain regions exploited for geothermal energy, such as near Geyserville in Northern California. These occur so continuously that the current USGS event map for that location usually shows a substantial number of small earthquakes at that location. (en)
- Gempa mikro adalah gempa bumi yang memiliki nilai magnitudo kecil (kurang dari 2 SR). Gempa bumi ini hanya dapat dirasakan oleh orang-orang yang berada dalam radius 8 kilometer. Gempa mikro sering terjadi pada reservoir geotermal yang dipicu oleh terbentuknya rekahan pada batuan reservoir ketika dilakukan injeksi fluida. Sehingga gempa mikro dapat digolongkan sebagai induced earthquakes. (in)
- 미소지진(Microearthquake)이란 규모 2.0 이하의 매우 작은 크기의 지진을 의미한다. 미소지진의 경우에는 진앙에서 약 8 km 이상 떨어진 곳에서는 거의 느낄 수 없다. 미소지진은 자연적인 판 구조론적 원인 외에도 지하 핵실험이나 발파를 위한 재래식 폭발 등 인공지진으로도 발생할 수 있다. 미소지진은 거의 대부분 인간의 생명이나 재산에 큰 피해를 주지 않으며 사람들도 거의 느끼지 못한다. 예외적으로 2011년 10월 7일 7시 20분 일본 도야마현 동부 지진(최대진도 1)의 경우 규모 Mj2.4의 미소지진이었으나 당시 산사태로 인한 낙석으로 1명이 사망하였고 일본에서 가장 작은 규모로 사망자가 발생한 지진으로 기록되었다. 미소지진은 화산 분화가 가까운 화산의 화구 인근에서 잘 발생하며, 화산성 지진의 일종으로 미소지진이 발생하기도 한다. (ko)
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