earth sci Flashcards
the study of the origin, history, and structure of the earth
GEOLOGY
the study of outer space and the physical bodies beyond the earth
ASTRONOMY
the study of everything in ocean environment, which covers about 70% of the earths surface
OCEANOGRAPHY
the science of the atmosphere and its phenomena (the study of the weather)includes the study of weather patterns, clouds, hurricanes, and tornadoes
METEOROLOGY
the concern of this theory is to solve problems about angular momentum of the sun
SOLAR NEBULAR HYPOTHESIS
this theory is proposed by Rene Descartes, its was formed into bodies with nearly circular orbits because of the whirlpool-like motion in the pre -solar materials
VORTEX THEORY
this theory is proposed by George Louis Leclerc, Comte de Buffon. the planets were formed by the collision of the sun with a giant comet
COLLISION THEORY
this is proposed by Immanuel Kant and Pierre Simon Laplace, nebula collapses because of gravitational force, and contracts as it spins more rapidly.
KANT-LAPLACE THEORY
this is proposed by Harold Jeffreys and James Jeans, and the planets were formed from the substance that was torn out f the sun
JEANS-JEFFREYS’ TIDAL THEORY
used to describe how light id reflected from the surface of a mineral
LUSTER
this is opaque and very reflective like gold and silver
METALLIC LUSTER
this is a dull, silky, greasy, and pearly like silicates
NON-METALLIC LUSTER
a measure of the resistance of a mineral to being scratched
HARDNESS
the least used property in determining what mineral is present in a rock
COLOR
this is a visible expression of a mineral’s internal arrangement of atoms
CRYSTALLINE STRUCTURE
three-dimensions of the mineral have about the same length, like that of a a cube or sphere
EQUANT
Forms prismatic or prism-like crystals that are thicker than needle as in a pencil
ELONGATE
looks like a flattened and thin crystal (like plate)
PLATY
the tendency of a mineral to cleave, or break, along flat, even surfaces.
CLEAVAGE
the uneven breakage of a mineral
FRACTURE
refers to the ability of some minerals to be attracted to a hand magnet
MAGNETISM
some mineral especially carbonate minerals, react visibly with acid
REACTION TO ACID
refers to the weight of that mineral divided by the weight of an equal volume of water
SPECIFIC GRAVITY
some minerals have distinctive taste (halite is salt, and tastes like it)
TASTE, ODOR, AND SMELL
this silicone-oxygen tetrahedron provides the framework of every silicate mineral
SILICATES
Mineral that contains the elements carbon, oxygen, and one more other silicate mineral
CARBONATES
minerals that contain oxygen or other elements, which usually metals
OXIDES
minerals that contain the element sulfur
SULFATES AND SULFIDES
minerals that contain a halogen ion plus one or more other elements
HALIDES
minerals that exist in relatively pure form. they naturally in an uncombined form with a distinct mineral structure
NATIVE ELEMENTS
they are often formed when other minerals are broken down by weathering, they are brightly colored
PHOSPHATES
it is the term used for hose substances that do not fit nearly into one of the eight classses
MINERALOID
it is the physical disintegration or chemical alteration of rocks or near the earths surface
WEATHERING
it is also known as physical weathering, caused by the change of temperature due to contraction and expansion rocks break up
MECHANICAL WEATHERING
Over millennia, tectonic
forces may raise the granite to
form a mountain range. As the
granite rises, the overlying
rock erodes and the pressure
decreases.
PRESSURE-RELEASE FRACTURING
Water
accumulates in a crack and then
freezes, the ice expands. Ice pushes
rock apart but at the same time
cements it together. When the ice
melts, rock fragments tumble from
a steep cliff.
FROST WEDGING
rocks, grains of sand,
and silt collide with one another when
currents or waves carry them along a
stream or beach. During these
collisions, their sharp edges and
corners wear away, and the particles
become eroded. The mechanical
wearing of rocks by friction and
impact is called abrasion.
ABRASION
if soil
collects in a crack in bedrock, a
seed may fall there and sprout.
The roots work their way into the
crack, expand, and may
eventually widen the crack.
ORGANIC ACTIVITY
Rocks at Earth’s
surface are exposed to daily and
yearly cycles of heating and cooling.
They expand when they are heated
and contract when they cool.
THERMAL EXPANSION AND CONTRACTION
Decomposes, dissolves, alters, or weakens the rock through
chemical processes to form residual materials.
CHEMICAL WEATHERING
we are all
familiar with the fact that
some minerals dissolve
readily in water while others
do not. If you put a crystal of
halite in water, the crystals
rapidly dissolve to form a
solution.
DISSOLUTON
water reacts
with a mineral to form a new
mineral with the water as part
of its crystal structure. Most
common minerals weather by
hydrolysis.
HYDROLYSIS
is the reaction of rock
minerals with oxygen. Iron rusts when
it reacts with water and oxygen.
OXIDATION
the process of rock
minerals reacts when carbon dioxide
and water combines forming carbonic acid.
CARBONATION
The process of transporting the weathered material,
eventually depositing it in new location or environment (Sills,
2010).
EROSION
when those sediments
are deposited, or dropped off, in a
different location. Deposition adds
sediment to a land form.
DEPOSITION
are the two types of weathering
CHEMICAL and MECHANICAL
is NOT interconnected with Exogenic Processes
GEOSPHERE
is described as the breakdown of a rock into unconnected grains or chunks without changes in its composition
MECHANICAL WEATHERING
Exfoliation, frost wedging, root wedging, salt wedging, and thermal expansion are under
MECHANICAL WEATHERING