Archean Eon Flashcards
Three reasons why there are no rocks older than 4.0 Billion Years Old.
- Due to Metamorphism and Deformation
- Deeply Buried Beneath Younger Rocks
- Contains Few Fossils of any use for Biostratigraphy
Rapidly-rotating, hot, barren, waterless planet, bombarded by meteorites and comets. Wherein there is no continents, intense cosmic radiation, no organisms, and widespread volcanism.
The Precambrian Earth
Five events that summarizes the events of the Archean Eon.
- Differentiation of Earth’s Layers
- Formation of the Atmosphere
- Formation of the Oceans
- Formation of the Continents
- Earth’s Earliest Organisms
Two principal division of the Earth’s surface.
Continents and Ocean Basins
The significant difference between the continents and the ocean basins is called __________.
Relative Levels
remarkably flat features that have the appearance of plateaus protruding above sea level.
Continents
the average depth of the ocean floor is about _______ kilometers
3.8 Kilometres Below Sea Level
The plateaus protruding above sea
level has an average elevation of about _______ kilometer.
0.8 Kilometres
Earth’s first crust was probably composed of ________.
Basalt
The formation of continental crust is simply a continuation
of the ___________ ____________ of Earth materials that
began during the final accretionary stage of our planet.
Gravitational Segregation
Description of Earth’s core.
Metallic
Description of Earth’s Mantle.
Rocky
Description of Earth’s Crust.
Low-Density & Silica-rich
The age of the oldest continental crust is
uncertain, but we can be sure that at least
some was present by ________ billion years ago.
4.0 BYA
Name and Age of the Oldest Mineral Found in Sedimentary Rocks in Australia.
Zircons (ZrSiO₄)
4.4 BYO
True or False
From the geologic perspective, a continent is defined by its size, location, who discovered it, or whether it is surrounded by oceans.
False, it should not be defined by such factors.
Defined by the rocks it’s
made of and how it came to be that matter.
Continents
The largest features of the continents can be
grouped into two distinct categories.
Stable Interiors and Mountain Belts
Extensive, flat stable areas that have been eroded nearly to sea level.
Stable Interiors
Uplifted regions of
deformed rocks.
Mountain Belts
Tend to be long, narrow features at the margins of continents, and the flat, stable areas are typically located in the
interior of the continents.
Mountain Belts
Expansive, flat regions composed of deformed crystalline rock (metamorphic
rocks).
Shields
Other flat areas of the
stable interior in which highly deformed rocks,
like those found in the shields, are covered by
a relatively thin veneer of sedimentary rocks.
Stable Platforms
During the archean eon, hotspot volcanism and the subduction of the oceanic crusts led to the creation of _____________ -_______ __________.
Continent-size Landmasses