Test 2 Chapter 12 Flashcards
Explain why Earth is just the right size.
Earth is the right size to retain an atmosphere of the appropriate size to keep oxygen and
greenhouse gases in concentrations appropriate for life. If Earth were more massive, the
atmosphere would retain large amounts of ammonia and methane and would be too thick and too
hostile for life. If the Earth were smaller, the important gases, such as oxygen, would escape and
the planet would lack the atmosphere it currently has.
In what way does Earth’s molten, metallic core help protect Earth’s life-forms?
The molten core allows for the existence of a magnetic field, which in turn protects life from
cosmic rays that would be lethal and would strip away the atmosphere.
Why is Earth’s location in the solar system ideal for the development of complex life-forms like
humans?
The location of Earth in the solar system prevents it from being too hot (like Venus) or too cold
(like Mars). This ideal temperature allowed higher life to evolve over time.
What two elements made up most of the very early universe?
The very early universe was made up mostly of hydrogen and helium
Name the cataclysmic event in which an exploding massive star produces elements heavier than
iron.
Elements heavier than iron are formed at extreme temperatures during the explosive death of
large stars. These cataclysmic events are called supernova events
Briefly describe the formation of the planets from the solar nebula.
The solar nebula was a large, rotating cloud of interstellar dust and gas. As the nebula
contracted, most of its matter collected in the center to form the protosun. The remaining
materials flattened into a rotating disk, and the matter in the disk gradually cooled and
condensed into masses of icy, rocky, and metallic materials. Through repeated collisions and
accretion, these masses became the planets we have today.
Describe the conditions on Earth during the Hadean.
During the Hadean, Earth was mainly covered by a large magma ocean. Within this magma,
buoyant masses of molten rock rose to the surface to produce thin crustal rocks. The iron-rich
molten core formed during this time and through chemical differentiation, the major divisions of
Earth’s interior were formed
What is meant by outgassing, and what modern phenomenon serves that role today?
Outgassing is the process through which gases trapped in the planet’s interior were released.
Today, hundreds of active volcanoes continue outgassing processes.
List the most abundant gasses that were added to Earth’s early atmosphere through the process of
outgassing.
The most abundant gases added to Earth’s early atmosphere through outgassing were mainly
water vapor, carbon dioxide, and sulfur dioxide
Why was the evolution of photosynthesizing bacteria important for the evolution of large oxygen
consuming organisms like ourselves?
Early photosynthesizing bacteria were responsible for adding oxygen to the oceans, and as the
number of these organisms increased, oxygen began to build in the atmosphere, making the
evolution of higher life-forms possible.
Why was rainwater highly acidic in Earth’s early history
Early in Earth’s history, large amounts of sulfur dioxide were present in the atmosphere,
released from outgassing associated with large-scale volcanism. This sulfur dioxide combined
with water in the atmosphere to form sulfuric acid, creating the acidic rainwater.
How does the ocean remove carbon dioxide from the Earth’s atmosphere? What role do tiny
marine organisms, such as foraminifera, play in the removal of carbon dioxide?
Carbon dioxide dissolved in seawater often joins other atoms or molecules to produce various
chemical precipitates. The most common compound generated by this process is calcium
carbonate (CaCO3), a mineral that makes up the shells and hard parts of many tiny marine plants
and animals. Foraminifera make their shells of calcium carbonate using carbon dioxide from
seawater, and, when they die, their shells accumulate on the seafloor and essentially “lock up”
carbon dioxide that was taken in from the atmosphere.
Briefly explain how low-density continental crust was produced from Earth’s rocky mantle.
It is from Earth’s rocky mantle that low-density, silica-rich minerals were gradually distilled to
form continental crust. Partial melting of mantle rocks generates low-density, silica-rich
materials that buoyantly rise to the surface to form Earth’s crust, leaving behind the dense mantle
rocks.
Describe how cratons came into being.
Craton formation begins with the collision and accretion of small crustal fragments. Deep in
these collision-formed fragments, partial melting generated silica-rich magmas that rose and
intruded the rocks above resulting in the formation of crustal provinces that, in turn, accreted
with other provinces into large crustal blocks called cratons.
What is the supercontinent cycle? What supercontinent proceeded Pangaea?
The supercontinent cycle is the rifting and dispersal of one very large continent (supercontinent)
followed by a long period of time where the fragments are reassembled into a new supercontinent
with a different configuration. The supercontinent Rodinia preceded the supercontinent Pangaea