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Ess 101 B Midterm Exam Questions And Answers | Latest Update 2026/2027 | Graded A+ | 100% Assured Pass.

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Ess 101 B Midterm Exam Questions And Answers | Latest Update 2026/2027 | Graded A+ | 100% Assured Pass. Match the magma type with the appropriate tectonic setting where it likely forms: Iceland - ANSWER- basalt Match the magma type with the appropriate tectonic setting where it likely forms: Sierra Nevada Batholith - ANSWER- granite Match the magma type with the appropriate tectonic setting where it likely forms: Phillipine Islands - ANSWER- andesite The Columbia Plateau is composed of rock rich in - ANSWER- basalt How do we know that Earth was created from the debris of a previous star system? - ANSWER- Dense elements exist that could only have been formed through a Supernova event Steps of the Nebular Hypothesis - ANSWER- - Supernova and formation of primordial dust cloud - condensation of primordial dust. Forms disk-shaped nebular cloud rotating counterclockwise - Proto sun and planets begin to form - Accretion of planetesimals and differentiation of planets and moons - Existing solar system takes shape The melting temperature of granitic magma (wet melt) - ANSWER- increases as pressure is reduced (as it rises) A partial melt of the asthenosphere will not rise toward the surface because - ANSWERthe above question is incorrect because an asthenospheric melt will rise towards the surface Evidence to support the nebular hypothesis - ANSWER- - planets and moons revolve in a counter-clockwise direction (v. random) - Planetary orbits are aligned along the sun's equatorial plane (v. random) - Observations from Hubble and radio astronomy - Jovian planets are located far enough away from the sun that molecular hydrogen is cool and dense enough to remain in their atmosphere - Terrestrial planets are close enough to the sun that molecular hydrogen would be too heated, not dense enough to remain in the atmosphere What's the mantle made of? - ANSWER- Fe-Mg Silicate Characteristics of Terrestrial Planets - ANSWER- - Close to the sun, dense - Small, rocky (silicate minerals, metallic cores) Characteristics of Jovian Planets - ANSWER- - Far from the sun, low density - Large, gaseous (hydrogen, methane) Can you explain why the earth and terrestrial planets have so little molecular hydrogen comprising their respective atmospheres; yet the primarodial dust cloud was mostly comprised of hydrogen gas? - ANSWER- - Key word: heat. What's the crust made of? - ANSWER- Fe-Mg-Al Silicate Differentiated earth order (starting from center) - ANSWER- - Iron-Nickel Core - Fe-Mg Silicate Mantle - Fe-Mg-Al Silicate Crust (ocean and continental) - Oceans - Atmosphere How is the earth compositionally zoned? - ANSWER- Along a density gradient How did the earth become compositionally zoned? - ANSWER- - accretion of planetesimals - initial heating due to kinetic energy of colliding planetesimals and compressional heating - Additional heating from radioactive decay

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Ess 101 B
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Ess 101 B

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Ess 101 B Midterm Exam Questions And Answers |
Latest Update 2026/2027 | Graded A+ | 100%
Assured Pass.

Match the magma type with the appropriate tectonic setting where it likely forms:
Iceland - ANSWER- basalt

Match the magma type with the appropriate tectonic setting where it likely forms: Sierra
Nevada Batholith - ANSWER- granite

Match the magma type with the appropriate tectonic setting where it likely forms:
Phillipine Islands - ANSWER- andesite

The Columbia Plateau is composed of rock rich in - ANSWER- basalt

How do we know that Earth was created from the debris of a previous star system? -
ANSWER- Dense elements exist that could only have been formed through a
Supernova event

Steps of the Nebular Hypothesis - ANSWER- - Supernova and formation of primordial
dust cloud

- condensation of primordial dust. Forms disk-shaped nebular cloud rotating counter-
clockwise

- Proto sun and planets begin to form

- Accretion of planetesimals and differentiation of planets and moons

- Existing solar system takes shape

The melting temperature of granitic magma (wet melt) - ANSWER- increases as
pressure is reduced (as it rises)

A partial melt of the asthenosphere will not rise toward the surface because - ANSWER-
the above question is incorrect because an asthenospheric melt will rise towards the

,surface




Evidence to support the nebular hypothesis - ANSWER- - planets and moons revolve in
a counter-clockwise direction (v. random)

- Planetary orbits are aligned along the sun's equatorial plane (v. random)

- Observations from Hubble and radio astronomy

- Jovian planets are located far enough away from the sun that molecular hydrogen is
cool and dense enough to remain in their atmosphere

- Terrestrial planets are close enough to the sun that molecular hydrogen would be too
heated, not dense enough to remain in the atmosphere


What's the mantle made of? - ANSWER- Fe-Mg Silicate\

Characteristics of Terrestrial Planets - ANSWER- - Close to the sun, dense

- Small, rocky (silicate minerals, metallic cores)

Characteristics of Jovian Planets - ANSWER- - Far from the sun, low density

- Large, gaseous (hydrogen, methane)

Can you explain why the earth and terrestrial planets have so little molecular hydrogen
comprising their respective atmospheres; yet the primarodial dust cloud was mostly
comprised of hydrogen gas? - ANSWER- - Key word: heat.



What's the crust made of? - ANSWER- Fe-Mg-Al Silicate

Differentiated earth order (starting from center) - ANSWER- - Iron-Nickel Core
- Fe-Mg Silicate Mantle
- Fe-Mg-Al Silicate Crust (ocean and continental)
- Oceans

, - Atmosphere

How is the earth compositionally zoned? - ANSWER- Along a density gradient
How did the earth become compositionally zoned? - ANSWER- - accretion of
planetesimals

- initial heating due to kinetic energy of colliding planetesimals and compressional
heating

- Additional heating from radioactive decay

- melting point reached, dense iron sinks to core while lighter minerals are displaced
outwards

- earth becomes compositionally zoned based on density

- convective overturn in asthenosphere, mantle, and outer core continues today

Why did the earth heat up and then rapidly cool during the differentiation process? -
ANSWER- - Conduction: SLOW, rate of heat leaving too slow to cool the rapidly heating
planet, therefore liquification

- Convection: FAST, liquid--> solid, rapid cooling


What's the inner and outer core of the earth made of? - ANSWER- Iron-Nickel Core

Inner core in which phase? - ANSWER- solid

Outer core in which phase? - ANSWER- liquid

What evidence do scientists use to support the inferred compositional zonation? -
ANSWER- - meteorological evidence
- density properties of the earth
- magnetic field evidence
- seismic wave evidence

Describe meteorological evidence supporting differentiated earth - ANSWER- - same
meteors hitting the earth since it has been formed. From observing and tracking the
composition and quantities of material making up meteorites, inferences regarding the
material composition of the planet can be made

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