Introduction
Imagine trying to explore a mysterious world buried 6,370 kilometers beneath your feet. We can’t physically journey to the Earth’s center, but we’ve devised ingenious ways to uncover its secrets. By studying rocks from deep mines, analyzing magma from volcanic eruptions, and using high-tech drilling projects, we’re piecing together a fascinating picture of what lies beneath.
There are two sources for information about the interior of the earth:
a) Direct Sources
b) Indirect Sources
Direct Sources
Direct sources include rock materials from mining areas and molten magma from volcanic eruptions.
- Surface rock or the rocks we get from mining areas. Gold mines in South Africa reach depths of 3-4 km.
- Scientists are working on major projects such as the "Deep Ocean Drilling Project" and the "Integrated Ocean Drilling Project."
- The deepest drill at Kola in the Arctic Ocean has reached 12 km.
- Volcanic eruptions provide direct information as magma is available for laboratory analysis.
- These projects and natural events have provided a large volume of information through the analysis of materials collected at different depth
Indirect Sources
Indirect sources include meteors that at times reach the earth, gravitation, magnetic field, and seismic activity.
- Mining reveals that temperature, pressure, and material density increase with depth.
- Scientists estimate temperature, pressure, and density at various depths using the total thickness of the Earth.
- Meteors provide indirect information, as their materials and structures are similar to Earth's.
- Indirect sources include gravitation, magnetic field, and seismic activity.
- Gravitation varies with latitude, being greater at the poles and less at the equator due to differences in distance from the center.
- Gravity values differ according to the mass of the material and other factors, resulting in gravity anomalies that reveal mass distribution in the Earth's crust.
- Magnetic surveys provide information about the distribution of magnetic materials in the crust.
- Seismic activity offers crucial insights into Earth's interior.
Earthquake
It is the shaking of the earth, natural event. It is caused due to release of energy which generates waves that travel to all directions.
Question for Revision Notes - Interior of the Earth
Try yourself:Which one of the following is a direct source of the information about the interior of the Earth?
Explanation
Volcanic eruptions are direct sources of information about the interior of the earth. As and when the molten material (magma) is thrown onto the surface of the earth, during a volcanic eruption it becomes available for laboratory analysis.
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Why does the Earth Shake?
However, the tendency of movement overcomes the friction.
As a result, blocks get deformed. They slide over another: as a result energy releases.
Energy waves travel in all directions.
The point where energy releases is called focus/hypocenter. Above the focus point on the surface it is called the epicenter
Earthquake Waves
- All-natural earthquakes take place in the lithosphere (depth up to 200 km from the surface of the earth.)
- An instrument called ‘seismograph’ records the waves reaching the surface.
- Two types of waves — body waves and surface waves.
- Body waves are generated due to the release of energy at the focus and move in all directions traveling through the body of the earth. Hence, the name body waves.
- The body waves interact with the surface rocks and generate a new set of waves called surface waves. These waves move along the surface.
- The velocity of waves changes as they travel through materials with different densities.
- The denser the material, the higher is the velocity.
- Their direction also changes as they reflect or refract when coming across materials with different densities.
Body Waves.
They are called P and S-waves.
P-waves: Move faster and are the first to arrive at the surface. These are also called ‘primary waves’.
- The P-waves are similar to sound waves.
- They travel through gaseous, liquid, and solid materials (as sound).
- P-waves vibrate parallel to the direction of the wave (P for parallel).
- This exerts pressure on the material in the direction of the propagation.
- As a result, it creates density differences in the material leading to stretching and squeezing of the material
S-waves: Arrive at the surface with some time lag. These are called secondary waves.
- An important fact about S-waves is that they can travel only through solid materials. (important)
- It has helped scientists to understand the structure of the interior of the earth.
- Reflection causes waves to rebound whereas refraction makes waves move in different directions.
- These waves are more destructive. They cause the displacement of rocks, and hence, the collapse of structures occurs.
- The direction of vibrations of S-waves is perpendicular to the wave direction in the vertical plane.
- Hence, they create troughs and crests in the material through which they pass.
Surface Waves:
- The surface waves are the last to report on seismograph. These waves are more destructive.
- They cause displacement of rocks, and hence, the collapse of structures occurs
Question for Revision Notes - Interior of the Earth
Try yourself:
What is the point on the surface directly above the point where an earthquake originates?Explanation
- The epicenter is the point on the Earth's surface directly above the point where an earthquake originates.
- It is the location where the seismic waves reach the surface after being released from the focus or hypocenter underground.
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Propagation of Earth Quake Waves
P-Waves (Primary Waves)
- P-waves travel parallel to the direction of the wave.
- They cause vibrations in the rocks, exerting pressure in the direction of wave propagation.
- This results in stretching and squeezing of the material, creating density differences.
S-Waves (Secondary Waves)
- S-waves travel perpendicular to the direction of wave propagation.
- They cause vibrations in the vertical plane, creating troughs and crests in the material.
- The perpendicular movement leads to significant deformation in the rocks.
Surface Waves
- Surface waves travel along the Earth's surface.
- They are considered the most damaging type of earthquake waves.
- Surface waves cause severe vibrations, leading to substantial damage to structures on the surface.
The Emergence of Shadow Zone
- Earthquake waves get recorded in seismo- graphs located at far-off locations. However, there exist some specific areas where the waves are not reported. Such a zone is called the ‘shadow zone’.
- A zone between 105° and 145° from epicenter was identified as the shadow zone for both types of waves.
- The entire zone beyond 105° does not receive S-waves. The shadow zone of S-wave is much larger than that of the P-waves.
- The shadow zone of P-waves appears as a band around the earth between 105°and 145° away from the epicenter
Types of Earthquakes
- The most common ones are tectonic earthquakes. These are generated due to sliding of rocks along a fault plane.
- A special class of tectonic earthquakes is sometimes recognized as volcanic earthquakes. However, these are confined to areas of active volcanoes.
- In the areas of intense mining activity, sometimes the roofs of underground mines collapse causing minor tremors. These are called collapse earthquakes.
- Ground shaking may also occur due to the explosion of chemical or nuclear devices. Such tremors are called explosion earthquakes.
- The earthquakes that occur in the areas of large reservoirs are referred to as reservoir induced earthquakes
Measuring Earthquakes
- The earthquake events are scaled either according to the magnitude or intensity of the shock.
- The magnitude scale is known as the Richter scale.
- The magnitude relates to the energy released during the quake.
- The magnitude is expressed in absolute numbers, 0-10.
- The intensity scale is named after Mercalli, an Italian seismologist.
- The intensity scale takes into account the visible damage caused by the event.
- The range of intensity scale is from 1-12.
Effects of Earthquake
Earthquake is a natural hazard. The following are the immediate hazardous effects of earthquake:
- Ground Shaking
- Differential ground settlement
- Land and mud slides
- Soil liquefaction
- Ground lurching
- Avalanches
- Ground displacement
- Floods from dam and levee failures
- Fires
- Structural collapse
- Falling objects
- Tsunami
The first six listed above have some bearings upon landforms, while others may be considered the effects causing immediate concern to the life and properties of people in the region.
The effect of tsunami would occur only if the epicenter of the tremor is below oceanic waters and the magnitude is sufficiently high. Tsunamis are waves generated by tremors and not an earthquake in itself.
Though the actual quake activity lasts for a few seconds, its effects are devastating provided the magnitude of the quake is more than 5 on the Richter scale.
Question for Revision Notes - Interior of the Earth
Try yourself:
Which type of earthquake waves can travel through solid materials only?Explanation
- S-waves can travel through solid materials only, unlike P-waves which can travel through gaseous, liquid, and solid materials.
- The direction of vibrations of S-waves is perpendicular to the wave direction in the vertical plane.
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Structure of the Earth
The Crust
- It is the outermost solid part of the earth.
- It is brittle in nature.
- The thickness of the crust varies under the oceanic and continental areas. Oceanic crust is thinner as compared to the continental crust.
- The mean thickness of the oceanic crust is 5 km whereas that of the continental is around 30 km.
- It is as much as 70 km thick in the Himalayan region.
The Mantle
- The portion of the interior beyond the crust is called the mantle.
- The mantle extends from Moho’s discontinuity to a depth of 2,900 km.
- The upper portion of the mantle is called asthenosphere.
- The word astheno means weak. It is considered to be extending up to 400 km.
- It is the main source of magma that finds its way to the surface during volcanic eruptions. It has a density higher than the crust’s (3.4 g/cm3).
- The crust and the uppermost part of the mantle are called the lithosphere. Its thickness ranges from 10-200 km.
- The lower mantle extends beyond the asthenosphere. It is in solid-state
The Core
- The core-mantle boundary is located at the depth of 2,900 km.
- The outer core is in a liquid state while the inner core is in solid-state.
- The core is made up of very heavy material mostly constituted by nickel and iron. It is sometimes referred to as the nife layer.
Question for Revision Notes - Interior of the Earth
Try yourself:The innermost layer of the earth is?
Explanation
The innermost layer of the earth is known as the core. It is divided into inner core and outer core. It comprises of a high concentration of nickel and iron.
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A volcano is a place where gases, ashes, and/or molten rock material – lava – escape to the ground.
- A volcano is called an active volcano if the materials mentioned are being released or have been released out in the recent past.
- The mantle contains a weaker zone called asthenosphere.
- The material in the upper mantle(asthenosphere ) portion is called magma.
- Once it starts moving towards the crust or it reaches the surface, it is referred to as lava.
- The material that reaches the ground includes lava flows, pyroclastic debris, volcanic bombs, ash and dust, and gases such as nitrogen compounds, sulphur compounds, and minor amounts of chlorine, hydrogen, and argon.
- Volcanoes are classified on the basis of the nature of eruption and the form developed at the surface. Major types of volcanoes are as follows:
Shield Volcanoes
Barring the basalt flows, the shield volcanoes are the largest of all the volcanoes on the earth.
- The Hawaiian volcanoes are the most famous examples.
- These volcanoes are mostly made up of basalt, a type of lava that is very fluid when erupted.
- For this reason, these volcanoes are not steep.
- They become explosive if somehow water gets into the vent; otherwise, they are characterized by low explosivity.
- The upcoming lava moves in the form of a fountain and throws out the cone at the top of the vent and develops into a cinder cone.
Composite Volcanoes
- These volcanoes are characterized by eruptions of cooler and more viscous lavas than basalt.
- These volcanoes often result in explosive eruptions.
- Along with lava, large quantities of pyroclastic material and ashes find their way to the ground.
- This material accumulates in the vicinity of the vent openings leading to the formation of layers, and this makes the mounts appear as composite volcanoes. more than 50 m. Individual flows may extend for hundreds of km.
- The Deccan Traps from India, presently covering most of the Maharashtra plateau, are a much larger flood basalt province.
Caldera
- These are the most explosive of the earth’s volcanoes.
- They are usually so explosive that when they erupt they tend to collapse on themselves rather than building any tall structure.
- The collapsed depressions are called calderas.
- Their explosiveness indicates that the magma chamber supplying the lava is not only huge but is also in close vicinity.
Flood Basalt Provinces
- These volcanoes outpour highly fluid lava that flows for long distances.
- Some parts of the world are covered by thousands of sq. km of thick basalt lava flows. There can be a series of flows with some flows attaining a thickness.
Mid-Ocean Ridge Volcanoes
- These volcanoes occur in oceanic areas.
- There is a system of mid-ocean ridges more than 70,000 km long that stretches through all the ocean basins.
- The central portion of this ridge experiences frequent eruptions.
Question for Revision Notes - Interior of the Earth
Try yourself:
Which intrusive form is characterized by a large dome-shaped body with a level base and connected by a pipe-like conduit from below?Explanation
- Lacolith is characterized by a large dome-shaped body with a level base and connected by a pipe-like conduit from below.
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Intrusive Forms
- The lava that is released during volcanic eruptions on cooling develops into igneous rocks.
- The cooling may take place either on reaching the surface or also while the lava is still in the crustal portion.
- Depending on the location of the cooling of the lava, igneous rocks are classified as volcanic rocks (cooling at the surface) and plutonic rocks (cooling in the crust).
The lava that cools within the crustal portions assumes different forms. These forms are called
intrusive forms
Batholiths
- A large body of magmatic material that cools in the deeper depth of the crust develops in the form of large domes.
- They appear on the surface only after the denudational processes remove the overlying materials.
- They cover large areas, and at times, assume depth that may be several km. These are granitic bodies.
- Batholiths are the cooled portion of magma chambers.
Lacoliths
- These are large dome-shaped intrusive bodies with a level base and connected by a pipe-like conduit from below.
- It resembles the surface volcanic domes of the composite volcanoes, only these are located at deeper depths.
- It can be regarded as the localized source of lava that finds its way to the surface.
- The Karnataka plateau is spotted with domal hills of granite rocks.
- Most of these, now exfoliated, are examples of laccoliths or batholiths.
Lopolith, Phacolith, and Sills
- As and when the lava moves upwards, a portion of the same may tend to move in a horizontal direction wherever it finds a weak plane.
- It may get rested in different forms. In case it develops into a saucer shape, concave to the sky body, it is called lopolith.
- A wavy mass of intrusive rocks, at times, is found at the base of synclines or at the top of anticline in the folded igneous country. Such wavy materials have a definite conduit to source beneath in the form of magma chambers (subsequently developed as batholiths). These are called the phacoliths.
- The near horizontal bodies of the intrusive igneous rocks are called sill or sheet, depending on the thickness of the material. The thinner ones are called sheets while the thick horizontal deposits are called sills.
Dykes
- When the lava makes its way through cracks and the fissures developed in the land, it solidifies almost perpendicular to the ground.
- It gets cooled in the same position to develop a wall-like structure. Such structures are called dykes.
- These are the most commonly found intrusive forms in the western Maharashtra area.
- These are considered the feeders for the eruptions that led to the development of the Deccan traps.
Conclusion
Even though we can’t travel to the Earth’s core, our innovative methods are unveiling the hidden world beneath us. By combining direct samples from deep within the Earth with clever indirect observations, scientists are continually enhancing our understanding of this mysterious and fascinating realm. The journey to the center of the Earth might be out of reach, but our quest to uncover its secrets is very much alive and exciting.