India
Embed This Widget
Add the script tag and a data attribute to embed this widget.
Embed via iframe for maximum compatibility.
<iframe src="https://quakefyi.com/iframe/entity//" width="420" height="400" frameborder="0" style="border:0;border-radius:10px;max-width:100%" loading="lazy"></iframe>Paste this URL in WordPress, Medium, or any oEmbed-compatible platform.
https://quakefyi.com/entity//Add a dynamic SVG badge to your README or docs.
[](https://quakefyi.com/entity//)Use the native HTML custom element.
India terletak di Asia dan memiliki klasifikasi risiko seismik High. Total 1 gempa bumi telah tercatat di negara ini. Gempa bumi terbesar yang tercatat di negara ini mencapai magnitudo 4,5. Dengan populasi 1.417.492.000 dan luas daratan 3.287.263 km², peristiwa seismik dapat memiliki implikasi signifikan terhadap infrastruktur dan keselamatan publik.
Tinjauan Seismik
India's seismic landscape is dominated by two fundamentally different earthquake environments. The Himalayan arc in the north, created by the ongoing collision of the Indian Plate with Asia, represents one of the world's most dangerous seismic zones, capable of generating great earthquakes exceeding magnitude 8.5. The Indian Plate interior — the ancient stable craton — is generally less seismic but has produced devastating intraplate earthquakes where ancient [[fault]] systems are reactivated by far-field stresses. The country is formally divided into five seismic zones (I through V), with Zone V encompassing the northeastern states, Jammu and Kashmir, Himachal Pradesh, Uttarakhand, and parts of Gujarat. The Andaman and Nicobar Islands lie at an active [[subduction-zone]] and are highly seismic.
India's seismic history includes some of the most catastrophic earthquakes of the 20th century. The 1905 Kangra earthquake (magnitude 7.8) killed over 19,000 people in the Punjab Himalaya. The 1934 Bihar-Nepal earthquake (magnitude 8.1) killed more than 10,000 in the Gangetic plains. The 1950 Assam earthquake (magnitude 8.6) remains one of the largest continental earthquakes ever recorded, triggering massive landslides and riverine floods. The 1993 Latur earthquake (magnitude 6.2) in Maharashtra exposed the hidden hazard of intraplate events, killing nearly 10,000 people in villages built of stone masonry. The 2001 Bhuj earthquake (magnitude 7.7) in Gujarat devastated the Kutch region, killing over 20,000 people and becoming a watershed event for Indian earthquake engineering and building codes. [[aftershock]] sequences from Indian Himalayan earthquakes can extend for years, complicating recovery efforts.
The tectonic framework of India reflects 50 million years of continental collision following the closure of the Tethys Ocean. The Indian Plate continues to move northward at roughly 45–50 millimetres per year relative to Asia, and while much of this motion is now accommodated within the thickened Tibetan crust, 15–20 millimetres per year is still taken up by active shortening across the Himalayan thrust belt. The Main Frontal Thrust (MFT) is the most active structure in the Indian Himalaya, and paleoseismic investigations show evidence of great prehistoric earthquakes exceeding magnitude 8.5 that ruptured the entire arc length of the fault. The Andaman Trench to the southeast is a fully active [[subduction-zone]] where the Indian Plate descends beneath the Sunda Plate, generating frequent moderate to large earthquakes and the occasional great tsunami-generating event, as seen in the 2004 earthquake. [[intensity]] maps from historical Indian earthquakes reveal the complex interaction between source, path, and local site conditions across the subcontinent's varied geology.
Gempa Terbaru
| Mag. | Lokasi | Waktu | |
|---|---|---|---|
| Tidak ada gempa bumi terbaru. | |||
Peristiwa Historis yang Menonjol
Earthquakes Near Major Cities in India
Pertanyaan yang Sering Diajukan
India is located in a high seismic risk zone, meaning earthquakes are frequent and can be destructive. A total of 1 earthquakes have been recorded in India's seismic history.
The largest recorded earthquake in India had a magnitude of 4.5. Earthquakes of this size can cause significant damage depending on depth, location, and local building standards.
India has had 1 recorded earthquakes. This count includes events of all magnitudes detected by seismic monitoring networks. The actual number of earthquakes may be higher, as smaller events can go undetected.
India is classified in the "High" seismic zone, located in Asia. Seismic zones indicate the relative level of earthquake hazard based on historical activity, geological conditions, and proximity to tectonic plate boundaries.
Selama gempa bumi, Merunduk, Berlindung, dan Bertahan. Berlindung di bawah meja atau meja yang kokoh, lindungi kepala dan leher Anda, dan bertahan hingga guncangan berhenti. Jika di luar ruangan, pindah ke area terbuka jauh dari bangunan dan kabel listrik.
Risiko gempa bumi suatu negara dinilai menggunakan beberapa faktor: kedekatan dengan batas lempeng tektonik, seismisitas historis (frekuensi dan magnitudo kejadian masa lalu), kondisi geologi, kepadatan penduduk di zona seismik, dan penegakan standar bangunan. QuakeFYI menetapkan zona seismik dari 0 (tanpa risiko) hingga 4 (sangat tinggi) berdasarkan faktor-faktor tersebut.
Zona seismik adalah wilayah geografis yang diklasifikasikan berdasarkan tingkat bahaya gempa bumi. Zona 0 memiliki risiko yang dapat diabaikan, Zona 1 memiliki risiko rendah, Zona 2 memiliki risiko sedang, Zona 3 memiliki risiko tinggi, dan Zona 4 memiliki risiko sangat tinggi. Zona-zona ini ditentukan oleh data gempa bumi historis, kondisi tektonik, dan kondisi geologi.
Negara-negara di sepanjang Cincin Api Pasifik mengalami gempa bumi paling banyak. Jepang, Indonesia, Chili, Filipina, dan Iran secara konsisten mencatat aktivitas seismik tertinggi. Amerika Serikat (terutama Alaska dan California), Turki, dan Meksiko juga termasuk negara-negara dengan aktivitas seismik tertinggi.
Kepadatan penduduk memperbesar risiko gempa bumi karena lebih banyak orang dan infrastruktur yang terpapar potensi kerusakan. Gempa bumi magnitudo 7,0 di kota yang padat penduduknya dapat menyebabkan ribuan korban, sementara kejadian yang sama di area tak berpenghuni mungkin tidak menyebabkan korban. Standar bangunan dan kesiapsiagaan darurat sangat mengurangi risiko di area padat penduduk.
Kepadatan seismik mengukur konsentrasi aktivitas gempa bumi relatif terhadap luas daratan suatu negara, dinyatakan sebagai gempa bumi per 1.000 kilometer persegi. Kepadatan seismik yang tinggi menunjukkan aktivitas gempa bumi yang sering per satuan luas, membantu membandingkan risiko seismik antara negara-negara dengan ukuran berbeda.
Aktivitas Seismik di Sekitar
Ringkasan Tahunan
Keselamatan Gempa Bumi
India berada di zona risiko seismik tinggi. Kesiapsiagaan menghadapi gempa bumi sangat direkomendasikan.
- Merunduk, Berlindung, dan Bertahan saat terjadi guncangan
- Simpan peralatan darurat dengan air, makanan, dan pertolongan pertama
- Identifikasi tempat aman di setiap ruangan jauh dari jendela dan benda berat
- Ketahui rute evakuasi tsunami jika berada di area pantai