Interior of the Earth Flashcards
All natural EQs take place in?
Lithosphere
About P, S, L waves
- Speed comparison: P > S > L
- Only waves moving along the wave: P - waves
- S & L waves can travel only through Solid, whereas P waves travel through Solid, Liquid, Gas
- Speed of P - waves: S > L > G (Different media)
- Shadow Zone (S): +105° to -105° and
Shadow Zone (P): +105° to +142° and -105° to -142°
Types of EQs
Remember: TV Cinema Easy Route
- Tectonic EQ
- Volcanic EQ
- Collapse EQ
- Explosive EQ
- Reservoir Induced EQ
Tsunamis are waves generated by ______ but not an ______ in itself
Tremors and EQ
Primary reason for Tsunami: EQ
Secondary reason for Tsunami: Tremors
Note: Tsunamis can even occur due to Volcanic eruptions, Submarine landslides, etc
Facts about Earth’s Interior
- Almost all layers are Solid, however Asthenosphere (Weak - Semi Solid like Toothpaste) and Outer Core (Liquid)
- Asthenosphere - Upper layer of Mantle extending upto 400 Km
- Lithosphere - Crust + Upper most part of Mantle (upto 200 Km)
Density value at surface, at centre, and average
At surface ρ = 2.7 g/cm3
Average ρ = 5.5 g/cm3
At center ρ = 13 g/cm3
Discontinuities of interior of Earth
Remember: CMR Given Lavishly
- Outer Crust - Inner Crust: Conrad
- Inner Crust - Outer Mantle: Moho
- Outer Mantle - Inner Mantle: Repetti
- Inner Mantle - Outer Core: Gutenberg
- Outer Core - Inner Core: Lehmann
Note: Bullen Discontinuity lies within the core differentiating based upon the density between Liquid Core and Solid Core
Materials that reach ground from a Volcano
- Lava Flows
- Pyroclastic Debris
- Volcanic Bombs
- Ash and Dust
- Gases such as N & S - compounds, H2, Cl, Ar
Type of Volcano - Shield Volcano
- Low Viscosity → Free Basalt Flow (Mostly Basalt only)
- Largest type of volcanoes
- Generally, non - explosive
- Examples: Mauna Loa and Mauna Kea (Largest Volcano: Mauna Loa)
Type of Volcano - Stratovolcanoes (or) Composite Volcanoes
- High Viscosity → Thick Lava Flow
- Caldera is part of Stratovolcanoes
- Most explosive
- Examples: Mt Stromboli (Light house of Mediterranean), Mt Vesuvius, Krakatoa, and Mt Fuji
Type of Volcanoes - Flood Basalt Volcanoes
- Least viscosity → Lava flows like River
- Fissure type of Volcanoes
- Examples: Siberian Traps, Deccan Traps, Snake Basin, Icelandic Shield, and Canadian Shield
Type of Volcano - Cinder Cone
- Releases only Pyroclastic products
- Generally found in NW America
Active Volcanoes are?
Stromboli, Krakatoa, Vesuvius, Etna, and Barren Island (A&N Islands)
Dormant Volcanoes Example
Mt Kilimanjaro
Extinct Volcanoes
Mt Kenya → In general, any volcano before going extinct releases fumaroles or solfataras
Basic Volcanoes
- Rich in Fe and Mg (Mafic)
- Less Viscous and Less Explosive
- Dark Color
- High Temperature
Acidic Volcanoes
- Rich in Silica
- High Viscous and High Explosive
- Light Color
- Low Temperature