पृथ्वी की आंतरिक संरचना की समझ प्राप्त करने के लिए भूकंप सर्वेक्षण का क्या महत्व है? विस्तार से विश्लेषण कीजिए। / To what extent does seismic investigation contribute to our understanding of the Earth's interior structure? Analyze its significance in detail.
Introduction
11 words
Main Body
Seismic waves: P-waves (3); long-lived; S-waves: 4-5 km/s (transverse). Body waves
From P-waves:
1. Inner wave (solid word element) - The closer the interior, lower the need of wave and the i-waves directly opposite mark the frost
2. Helps in determining interior densities due to earth P-wave shadow zone by i-waves can travel through solid, liquid
From S-waves:
1. Interior is non-homogenous as to extent of refraction
2. Mantle (test) is also non-homogenous so refraction is away from the core
3. The core is keyed (outer core)
1. Inner wave (solid word element) - The closer the interior, lower the need of wave and the i-waves directly opposite mark the frost
2. Helps in determining interior densities due to earth P-wave shadow zone by i-waves can travel through solid, liquid, solid, liquid
From S-waves:
1. Interior is non-homogenous as to extent of refraction
2. Mantle (test) is also non-homogenous so refraction is away from the core
3. The core is keyed (outer core)
— Kush Motwani · AIR 11
Diagram
Earth's internal structure with labels: epicenter, hypocenter/focus, crust, core, mantle, inner core, outer core, and wave patterns marked as P-wave and S-wave shadow zones, with Mohorovičić discontinuity notation
- Includes labeled diagram
- Explains P and S wave behavior
- Discusses shadow zones
- Mentions Mohorovičić discontinuity
- Uses seismic methodology
Kush Motwani
Salient features of World's Physical Geography
Earth's interior structure
Seismic investigation methods
174
Total words
4
Paragraphs
technical and explanatory
Tone