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The dynamic Earth · The dynamics of the geosphere

Structure and dynamics of the geosphere

The deepest hole ever drilled, the Kola Superdeep Borehole, barely reached 12 km in depth before the temperature and pressure made it unworkable. Compared with the $6{,}371\ \text{km}$ that separate the surface from the center of the Earth, that is an insignificant mark. Our entire picture of the planet's interior therefore comes from indirect methods.

Methods for studying the Earth's interior

The deepest mines barely reach $4\ \text{km}$ and boreholes $12\ \text{km}$, yet we know for certain that at a depth of $2{,}900\ \text{km}$ there is a layer of liquid metal: how can we map the interior of a planet if we have only scratched its crust?

Cross-section of the Earth showing the crust, mantle and liquid outer core. Seismic waves leave the focus, travel down through the mantle along curved paths and return to the surface at stations A and B. focus station A station B crust seismic waves mantle outer core (liquid) not to scale
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The deepest mine in the world reaches a depth of barely $4\ \text{km}$, while the radius of the Earth is about $6\,370\ \text{km}$. Explain why almost everything we know…

The deepest mine in the world reaches a depth of barely $4\ \text{km}$, while the radius of the Earth is about $6\,370\ \text{km}$. Explain why almost everything we know about the Earth's interior comes from indirect methods, and give one example of a direct method and one of an indirect method.

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S-type seismic waves do not pass through the outer core, whereas P-waves do, although their speed is reduced. What does this fact tell us about the physical state of the…

S-type seismic waves do not pass through the outer core, whereas P-waves do, although their speed is reduced. What does this fact tell us about the physical state of the outer core? Explain your reasoning.

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The model according to chemical composition

The Earth is like a peach with a thin skin, a thick juicy layer, and a pit in the center. Scientists group the layers by what they are made of.

Diagram of the layers of the geosphere according to the compositional model: crust, mantle and core crust mantle core
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Order the following layers of the geosphere from the surface to the center of the planet: inner core, mantle, outer core, crust. Then state which of them occupies the…

Order the following layers of the geosphere from the surface to the center of the planet: inner core, mantle, outer core, crust. Then state which of them occupies the largest part of the Earth's volume.

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The model according to mechanical behavior

At the surface, rocks break suddenly during earthquakes along faults like the San Andreas Fault, yet in mountain ranges we see strata of solid rock folded in gentle curves as if they were made of plasticine: why do the same materials behave so differently at different depths?

Cross-section of the Earth's outer layers according to their mechanical behavior: rigid lithosphere broken into plates, which includes the crust and the upper part of the mantle; plastic asthenosphere of the upper mantle, which flows slowly; and mesosphere, the more rigid lower mantle plate boundaries crust upper part of the mantle lithosphere rigid, in plates asthenosphere plastic: it flows very slowly (upper mantle) mesosphere more rigid (lower mantle) thicknesses not to scale
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Explain in your own words what the lithosphere is, which layers of the geosphere form it, and how it differs from the crust.

Explain in your own words what the lithosphere is, which layers of the geosphere form it, and how it differs from the crust.

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The geothermal gradient and convection currents

In the gold mines of South Africa, almost 4 km underground, the rock walls are at over $50\ ^{\circ}\text{C}$ (about $122\ ^{\circ}\text{F}$) and the air has to be cooled with tons of ice: at what rate does the interior of the geosphere heat up, and what effect does that heat have on the deep rocks?

Animation of the mantle's convection currents: dots rise along the blue paths (hot material) and sink along the green ones (cold material), staggered in a slow loop. heat from the core and radioactive decay
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Look at the diagram of the Earth's interior. Name the layers marked with numbers 1 to 4 and state one characteristic of each (physical state or composition).

Look at the diagram of the Earth's interior. Name the layers marked with numbers 1 to 4 and state one characteristic of each (physical state or composition).

1 2 3 4 1 → ? 2 → ? 3 → ? 4 → ?
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Convection currents exist in the mantle: hot material rises and cold material sinks. Explain what causes these currents and how they relate to the movement of the…

Convection currents exist in the mantle: hot material rises and cold material sinks. Explain what causes these currents and how they relate to the movement of the lithosphere.

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Back to the beginning: At a depth of 12 km in the Kola borehole, the temperature reached about $180\ ^{\circ}\text{C}$ (about $356\ ^{\circ}\text{F}$); the average gradient there was lower than the typical $30\ ^{\circ}\text{C/km}$. The rock, hot and under enormous pressure, behaved plastically and tended to close the hole, making it impossible to keep drilling. That is why scientists rely on indirect methods.

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