Edurev Geo Topics Flashcards
(79 cards)
Deepest depth of oil well drilled
8 km
Deepest mine in the world
Mponeng Gold Mine, 4 km
Deepest drilling project
Kola Superdeep Borehole, Murmansk Oblast, Russia (Arctic Ocean)
12 km
Indirect sources of info on earth’s interior
- Temperature
- Pressure
- Density
- Behaviour of seismic waves
- Meteorites
- Moon
On average, there is a rise of 1° for every ____ m of depth
32 m
Reasons for increase in heat and temperature in the earth’s interior
- Radioactive disintegration within rocks releases heat
- Internal and external forces like gravitational pull, weight of overlying rocks etc
- Chemical reactions
Due to the extreme temperatures in the interior of the earth, all matter within exists in liquid or gaseous state
FALSE
The extreme pressure solidifies matter, resulting in liquid state rocks
Properties of Aluminum in the Earth’s crust
- Third most abundant element in the crust
- Exists in stable combination with other materials like silicates and oxides
- High strength-to-weight ratio due to low density
- Superior malleability, corrosion resistance, good thermal and electrical conducitivity
Earth’s density
5.5 g/cm³
True or false: Earth’s density increases with depth
True
True or false: The gravitational force changes at different latitudes on the surface
True
Earth’s interior consists of how many sections? Name them
- Crust
- Asthenosphere
- Upper Mantle
- Lower Mantle
- Outer Core
- Inner Core
Direct sources of info about earth’s interior
- Deep earth mining and drilling
- Volcanic Eruptions
Second deepest mine in the world
TauTona Mine, 3.9 km
Seismic waves can be divided into 2:
- Body Waves
- Surface waves
Seismic body waves can be divided into 2:
- Primary waves (P waves)
- Secondary/ Shear waves (S waves)
Features of seismic body waves
- Generated due to release of energy at the focus of earthquake
- Move in all directions through the interior of the earth
Features of seismic surface waves
- Generated when body waves interact with surface rocks
- Longitudinal in nature
- Aka L-waves
- They move only along the surface
Features of P waves
- Longitudinal
- Fastest velocity: 6-15 km/s
- Can travel through solids, liquids and gases
Features of S waves
- Transverse
- Reach lower velocities compared to P waves
- Can’t pass through liquids or gases, only solids
- Particles swing side by side under the impact of S waves hence the name shear waves
How do seismic waves help us understand the earth’s interior
- Differences in arrival times
- Refraction - waves taking different paths than expected
- Shadow zones - absence of seismic waves
- Discontinuity in velocity as a function of depth indicate changes in composition and density
Velocities achieved by P waves
6-15 km/s
- Earth’s crust - less than 6 km/s
- Lower mantle - 13.5 km/s
- Inner core - 11 km/s
Velocities achieved by S waves
0-6 km/s
- Earth’s crust - 3-4 km/s
- Upper Mantle - 4-6 km/s
- Lower Mantle - 6-7 km/s
- Core indiscernible (0 - 3 km/s)
What’s a shadow zone
Area of the earth’s interior where seismic waves disappear