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- زلزال قشم 2005 هو زلزالٌ وقعَ في قشم في إيران بتاريخ 27 نوفمبر 2005. (ar)
- The 2005 Qeshm earthquake occurred on November 27 at 13:52 IRST (10:22 UTC) on the sparsely populated Qeshm Island off Southern Iran, killing 13 people and devastating 13 villages. It was Iran's second major earthquake of 2005, following the one at Zarand in February. The epicenter was about 1,500 kilometers (930 mi) south of Tehran, close to Iran's southern borders. Initial measurements showed that the earthquake registered about 6.0 on the moment magnitude scale, although that was reduced to 5.8 after further analysis. More than 400 minor aftershocks followed the main quake, 36 of which were greater than magnitude 2.5. The earthquake occurred in a remote area during the middle of the day, limiting the number of fatalities. Iranian relief efforts were effective and largely adequate, leading the country to decline offers of support from other nations and UNICEF. Qeshm Island is part of the Simply Folded Belt, the most seismically active part of the Zagros fold and thrust belt. Similar to most earthquakes in the area, the 2005 event resulted from reverse slip faulting. Since it lies in such a seismically active area, there is a high risk of destructive earthquakes in Iran; 1 in 3,000 deaths are attributable to earthquakes. One geophysicist has cited the lack of strict building codes as a serious concern. (en)
- 2005年格什姆地震是伊朗標準時間2005年11月27日下午13点52分（协调世界时10點22分）发生在伊朗南部格什姆岛的一场强烈地震。虽然当地人口稀少，但地震还是造成13人死亡，并使13个村庄受到毁灭性打击。这是该国继2005年2月的扎兰德地震以来遭受的又一场重大地震，震央位于德黑兰以南约1500公里，接近伊朗南部边境。初步测量结果表明地震的矩震级为6.0级，不过在进一步分析后调低至5.8级。主震后还发生了约400次轻度余震，其中36次的矩震级在2.5级以上。地震发生在偏远地区，时间又是中午，所以死亡人数较少。伊朗的救援工作卓有成效，各种抗震资源准备充足，伊朗得以直接开展自救，无需依赖他国和国际组织援助。 格什姆岛是扎格罗斯简单褶皱带的组成部分，后者是（Zagros fold and thrust belt）中地震活动最活跃的地区。与当地大部分地震类似，2005年这场地震也是逆滑断层的产物。由于所处位置地震活动频繁，伊朗遇到破坏性地震的风险也很高，进入20世纪以来，平均每3,000名伊朗人中就有1人死于地震相关事件。某地球物理学家认为，伊朗的建筑施工标准和品质也存在严重问题。这些都是伊朗地震频发并且造成惨重人员伤亡的原因。 (zh)
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- The Portuguese fortress in Qeshm was damaged in the earthquake. (en)
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- زلزال قشم 2005 هو زلزالٌ وقعَ في قشم في إيران بتاريخ 27 نوفمبر 2005. (ar)
- 2005年格什姆地震是伊朗標準時間2005年11月27日下午13点52分（协调世界时10點22分）发生在伊朗南部格什姆岛的一场强烈地震。虽然当地人口稀少，但地震还是造成13人死亡，并使13个村庄受到毁灭性打击。这是该国继2005年2月的扎兰德地震以来遭受的又一场重大地震，震央位于德黑兰以南约1500公里，接近伊朗南部边境。初步测量结果表明地震的矩震级为6.0级，不过在进一步分析后调低至5.8级。主震后还发生了约400次轻度余震，其中36次的矩震级在2.5级以上。地震发生在偏远地区，时间又是中午，所以死亡人数较少。伊朗的救援工作卓有成效，各种抗震资源准备充足，伊朗得以直接开展自救，无需依赖他国和国际组织援助。 格什姆岛是扎格罗斯简单褶皱带的组成部分，后者是（Zagros fold and thrust belt）中地震活动最活跃的地区。与当地大部分地震类似，2005年这场地震也是逆滑断层的产物。由于所处位置地震活动频繁，伊朗遇到破坏性地震的风险也很高，进入20世纪以来，平均每3,000名伊朗人中就有1人死于地震相关事件。某地球物理学家认为，伊朗的建筑施工标准和品质也存在严重问题。这些都是伊朗地震频发并且造成惨重人员伤亡的原因。 (zh)
- The 2005 Qeshm earthquake occurred on November 27 at 13:52 IRST (10:22 UTC) on the sparsely populated Qeshm Island off Southern Iran, killing 13 people and devastating 13 villages. It was Iran's second major earthquake of 2005, following the one at Zarand in February. The epicenter was about 1,500 kilometers (930 mi) south of Tehran, close to Iran's southern borders. Initial measurements showed that the earthquake registered about 6.0 on the moment magnitude scale, although that was reduced to 5.8 after further analysis. More than 400 minor aftershocks followed the main quake, 36 of which were greater than magnitude 2.5. The earthquake occurred in a remote area during the middle of the day, limiting the number of fatalities. Iranian relief efforts were effective and largely adequate, leadi (en)
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- زلزال قشم 2005 (ar)
- 2005 Qeshm earthquake (en)
- 2005年格什姆地震 (zh)
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