Why Earthquakes Are Increasing Worldwide: Kya Duniya Mein Bhukamp Badh Rahe Hain?
Aaj ke samay mein jab bhi hum news kholte hain, kahin na kahin bhukamp (Earthquake) ki khabar zaroori milti hai. Kabhi Turkey, kabhi Japan, aur kabhi hamare pyare Bharat ke Delhi-NCR ya Himalayan regions mein dharti kanpti hui mehsoos hoti hai.
Lekin kya waqayi duniya mein bhukamp badh gaye hain, ya hamari detection technology behtar ho gayi hai? Is article mein hum Seismology aur Geology ki gahraiyon mein utrenge aur iska asli kaaran janenge.

Bhukamp Kya Hai aur Ye Kyun Aate Hain? (The Basic Science)
Bhukamp ka aana ek natural process hai. Hamari dharti ke niche Tectonic Plates hoti hain jo lagatar dhere-dhere move karti rehti hain. Jab ye plates aapas mein takrati hain ya ek doosre se ragad khati hain, to bahut bhari matra mein energy release hoti hai, jise hum Seismic Waves ke roop mein mehsoos karte hain.
Kya Sach Mein Earthquakes Badh Rahe Hain? (Global Trends)
Global data ke mutabiq, har saal duniya mein lakhon bhukamp aate hain, lekin unme se zyadatar itne chhote hote hain ki humein pata bhi nahi chalta.
1. Better Detection Technology
Pehle hamare paas gine-chune Seismograph hote the. Aaj duniya bhar mein hazaron sensitive stations hain jo halki si halchal ko bhi record kar lete hain. Isliye humein aisa lagta hai ki bhukamp ki sankhya badh gayi hai.
2. Population Density aur Media Coverage
Pehle jab sunsaan ilako mein bhukamp aate the, to khabar nahi banti thi. Aaj har kone mein abaadi hai aur social media ki wajah se har chhota jhatka turant viral ho jata hai.
Earthquake Badhne Ke Mukhya Kaaran (Key Reasons)
Science ke mutabiq kuch aise factors hain jo seismic activity ko trigger kar rahe hain:
1. Tectonic Plate Movements
Earth ki outer shell 7 badi aur kai chhoti plates mein banti hui hai. Pacific Ring of Fire ek aisa kshetra hai jahan sabse zyada halchal hoti hai. India ki plate (Indian Plate) lagatar Eurasian plate ko push kar rahi hai, jis wajah se Himalayan region mein khatra badh raha hai.
2. Climate Change aur Melting Glaciers
Ye sunne mein ajeeb lag sakta hai, lekin Global Warming ka bhukamp se gehra rishta hai. Jab bade glaciers pighalte hain, to zameen par se bahut bhari wazan (pressure) hat jata hai. Is process ko Isostatic Rebound kehte hain, jo niche dabi fault lines ko active kar sakta hai.
3. Human-Induced Earthquakes (Insaani Galtiyan)
Insaan ki kuch activities bhi dharti ko hila rahi hain:
- Fracking: Tel aur gas nikalne ke liye zameen mein high-pressure paani dalna.
- Mining: Bade paimane par khudaai karna jiske karan crustal stress badhta hai.
- Reservoir-Induced Seismicity: Bahut bade baandh (Dams) banana, jisse pani ka bhari pressure tectonic balance bigad deta hai.
India Par Iska Kya Asar Hai? (Indian Context)
Bharat ka lagbhag 59% hissa bhukamp ke khatre mein aata hai.
- Zone V (Highest Risk): Isme North-East India, Jammu-Kashmir, Himachal, Uttarakhand aur Rann of Kutch aate hain.
- Delhi-NCR: Ye Zone IV mein aata hai, jahan ka khatra lagatar badh raha hai kyunki ye kai fault lines ke upar basa hai.
Earthquake Se Kaise Bachen? (Safety & Preparedness)
Bhukamp ko roka nahi ja sakta, lekin nuksan kam kiya ja sakta hai:
- Drop, Cover, and Hold on: Turant zameen par baithein aur kisi mazboot table ke niche chhupien.
- Earthquake-Resistant Buildings: Ghar banate waqt seismic codes ka sakti se palan karein.
- Emergency Kit: Paani, sookha khana, torch aur first-aid kit hamesha taiyar rakhein.
Conclusion: Science vs Myths
Ant mein, ye kehna galat nahi hoga ki dharti ki andaruni halchal hamesha se rahi hai. Halanki insaani gatividhiyan aur climate change ise thoda trigger kar rahe hain, lekin main wajah dharti ka natural evolution hi hai. Humein darne ke bajaye Disaster Management aur Science par bharosa rakhna chahiye.
Earthquake FAQ: Aksar Pooche Jaane Wale Sawal
Technically, bhukamp ki sankhya utni hi hai, lekin behtar **Seismic Technology** ki wajah se ab hum bahut chhote jhatkon ko bhi record kar paate hain, isliye aisa lagta hai ki ye badh gaye hain.
Haan, glaciers ke pighalne se dharti ki crust par se wazan kam hota hai, jisse **Tectonic Plates** mein halchal ho sakti hai. Ise ‘Isostatic Rebound’ kaha jata hai.
Bharat mein **Himalayan region** (J&K, Himachal, Uttarakhand) aur North-East India sabse zyada khatre wale ‘Zone 5’ mein aate hain.
Nahi, abhi tak aisi koi technology nahi hai jo bilkul sahi waqt aur jagah bata sake, lekin **Early Warning Systems** kuch seconds pehle alert bhej sakte hain.
Delhi kai local **Fault Lines** ke upar basa hai aur ye Himalayan region ke kareeb hai, isliye yahan seismic activity zyada mehsoos hoti hai.
Agar aap ghar ke andar hain, to kisi mazboot furniture ke niche chhupien. Agar bahar hain, to building, ped aur bijli ke khambon se door khule maidan mein jayein.
**Fracking (Oil extraction)**, bade baandhon (Dams) mein pani ka bhari dabav aur gehri mining se dharti ke andar stress badhta hai jo bhukamp la sakta hai.
Richter Scale bhukamp ki **Intensity (Tivrata)** naapne ka ek paimana hai. 7 se upar ki tivrata wale bhukamp vinashkari mane jate hain.
Scientific roop se ye puri tarah sabit nahi hai, lekin janwar dharti ki **P-waves** (jo insaano ko mehsoos nahi hoti) ko sun sakte hain, isliye wo ajeeb behave karne lagte hain.
Ye Pacific Ocean ke charo taraf ka ek rasta hai jahan duniya ke **90% bhukamp** aur zyadaactive volcanoes paye jate hain.
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