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WorksheetsEarth Sci 1 Grading Exam
Total questions: 90
Worksheet time: 45mins
is just another word for universe
COSMOS
BIG BANG THEORY
PROTOPLANET
COSMOLOGY
is the study of the origin, evolution and fate of
the universe
COSMOS
BIG BANG THEORY
PROTOPLANET
COSMOLOGY
Space and time spontaneously expanded from an infinitely
tiny and dense point called a singularity around 14 billion
years ago, and has been expanding ever since.
COSMOS
BIG BANG THEORY
PROTOPLANET
COSMOLOGY
As planets began to form, they grow in mass by accreting
planetesimals. Since force of gravity is proportional to
mass, the largest planetesimals are accreted first.
COSMOS
BIG BANG THEORY
PROTOPLANET
COSMOLOGY
Which among the statements are TRUE.
Earth is habitable because It has the right distance from the sun.
Earth is habitable because It is kept warm by insulating atmosphere.
Earth is habitable because it is a closed system for matter
All of the above
Contains all the solid, liquid, and gaseous water of the
planet.
HYDROSPHERE
BIOSPHERE
LITHOSPHERE
ATMOSPHERE
Contains all the planet’s living things, Includes all the microorganisms, plants, and animals of
earth. Living things from ecological communities (biomes) based
on the physical surroundings of an area.
HYDROSPHERE
BIOSPHERE
LITHOSPHERE
ATMOSPHERE
Contains all of the hard, solid land of the planet’s crust
(surface) up to the upper mantle.
HYDROSPHERE
BIOSPHERE
LITHOSPHERE
ATMOSPHERE
Contains the blanket of gases not only contains the air that we
breathe but also protects us from the blasts of heat and
radiation emanating from the sun.
HYDROSPHERE
BIOSPHERE
LITHOSPHERE
ATMOSPHERE
Layer closest to earth’s surface, Contains half of earth’s atmosphere, Clouds are found here
TROPOSPHERE
STRATOSPHERE
MESOSPHERE
THERMOSPHERE
EXOSPHERE
Starts above the troposphere and ends about 50km above
the ground, Ozone is abundant here, and This is where jet aircraft
and weather balloons fly
TROPOSPHERE
STRATOSPHERE
MESOSPHERE
THERMOSPHERE
EXOSPHERE
Starts at 50km and extends to 85km high, Meteors burn up in this layer
TROPOSPHERE
STRATOSPHERE
MESOSPHERE
THERMOSPHERE
EXOSPHERE
Extends from about 90km – 500km/1,000km
Air density is so low that most of this layer is what is
normally thought of as outer space (Karman Line, 100km) Auroras occur here
TROPOSPHERE
STRATOSPHERE
MESOSPHERE
THERMOSPHERE
EXOSPHERE
The highest layer, beyond the 500km - 1,000km boundary
Is extremely thin and is where the atmosphere merges into
outer space.
TROPOSPHERE
STRATOSPHERE
MESOSPHERE
THERMOSPHERE
EXOSPHERE
The top of the mesosphere, is the
coldest part of earth’s atmosphere.
TROPOSPHERE
MESOPAUSE
MESOSPHERE
THERMOSPHERE
EXOSPHERE
crust is where you and I live on and is by far the thinnest
of the layers of earth.
CRUST
MANTLE
CORE
OUTER CORE
INNER CORE
By far the largest layer, making up 84% of earth’s volume.
CRUST
MANTLE
CORE
OUTER CORE
INNER CORE
is the very hot, very dense center of our planet. Formed during the “iron catastrophe”
CRUST
MANTLE
CORE
OUTER CORE
INNER CORE
is fluid enough and low enough
in viscosity that it may spins faster than the entire earth.
Creates the electrical currents that drive the magnetic field.
CRUST
MANTLE
CORE
OUTER CORE
INNER CORE
Primarily iron and nickel, Enriched in unusual heavy elements, The pressures become high enough that despite very high temperatures, it is solid.
CRUST
MANTLE
CORE
OUTER CORE
INNER CORE
Crust-mantle boundary
Mohorovic Discontinuity
Gutenberg discontinuity
Mantle convection
Mantle-core boundary
Mohorovic Discontinuity
Gutenberg discontinuity
Mantle convection
describes the movement of the mantle
as it transfers heat from the white-hot core to the brittle
lithosphere.
Mohorovic Discontinuity
Gutenberg discontinuity
Mantle convection
Heat from when the planet formed, which has not
yet been lost. Frictional heating, caused by denser core material
sinking to the center of the planet; Heat from the decay of radioactive elements.
MAGMA
LAVA
IGNEOUS
METAMORPHIC
When magma is ejected by a volcano or other vent, the
material is called ____.
MAGMA
LAVA
IGNEOUS
METAMORPHIC
Magma that has cooled into a solid is called an _____ rock.
MAGMA
LAVA
IGNEOUS
METAMORPHIC
Involves the upward movement of earth’s mostly solid
mantle. This hot material rises to an area of lower pressure through
the process of convection. melts mantle
rock to form magma.
DECOMPRESSION MELTING
TRANSFER OF HEAT
INTRUSION
EXTRUSION
Magma can also be created when hot, liquid rock exits into
earth’s cold crust and is able to melt the surrounding rocks in
earth’s crust (the “ice cream”) into magma
DECOMPRESSION MELTING
TRANSFER OF HEAT
INTRUSION
EXTRUSION
is liquid rock that forms under earth’s surface. Magma from under the
surface is slowly pushed up from deep within the earth into
any cracks or spaces it can find, sometimes pushing existing rock out of the way.
DECOMPRESSION MELTING
TRANSFER OF HEAT
INTRUSION
EXTRUSION
Lava cools to form volcanic rock as well as volcanic glass. Magma can also
extrude into earth’s atmosphere as part of a violent volcanic explostion.
DECOMPRESSION MELTING
TRANSFER OF HEAT
INTRUSION
EXTRUSION
is a naturally occurring, inorganic solid with
a definite chemical composition and an ordered internal
structure.
MINERALS
ORE
ORE GENESIS
ORE DEPOSIT
Naturally occurring material from which a mineral or
minerals of economic value can be extracted. Extracted from the earth through mining; they are then refined (often vie smelting) to extract the valuable element,
or elements.
MINERALS
ORE
ORE GENESIS
ORE DEPOSIT
Process of ore formation
MINERALS
ORE
ORE GENESIS
ORE DEPOSIT
Occurrence of a particular ore type that has been tested and
known to be economically profitable to mine.
MINERALS
ORE
ORE GENESIS
ORE DEPOSIT
Valuable substances are concentrated within an igneous body through the
magmatic processes such as crystal fractionation,
partial melting, and crystal settling.
Magmatic Ore Deposits
Hydrothermal Ore Deposits
Sedimentary Ore Deposits
Placer Ore Deposits
Residual Ore Deposits
The concentration of valuable
substances by hot aqueous (water-rich
fluids flowing through fractures and pore
spaces in rocks.
Magmatic Ore Deposits
Hydrothermal Ore Deposits
Sedimentary Ore Deposits
Placer Ore Deposits
Residual Ore Deposits
Form evaporate deposits from
precipitation of saltwater and lake water.
Magmatic Ore Deposits
Hydrothermal Ore Deposits
Sedimentary Ore Deposits
Placer Ore Deposits
Residual Ore Deposits
Natural concentration of heavy materials
caused by effect of gravity on moving
particles.
Magmatic Ore Deposits
Hydrothermal Ore Deposits
Sedimentary Ore Deposits
Placer Ore Deposits
Residual Ore Deposits
Result from accumulation of valuable
materials through chemical weathering
process.
Magmatic Ore Deposits
Hydrothermal Ore Deposits
Sedimentary Ore Deposits
Placer Ore Deposits
Residual Ore Deposits
Reviewing of data working on gov’t requirements,
budget and organization proposals.
Field Project
Field Exploration
Pre-production Feasibility Study
Prospect Evaluation
Determines and validates the accuracy of all data
and information collected from the different
stages.
Field Project
Field Exploration
Pre-production Feasibility Study
Prospect Evaluation
Activities involve regional surface
investigation and interpretation.
Field Project
Detailed Exploration
Prospect Evaluation
Regional Reconnaissance
The objective of finding and delineating
targets or mineralized zones
Field Project
Detailed Exploration
Prospect Evaluation
Regional Reconnaissance
Assess market profitability by Extensive resources,
geotechnical, and engineering drilling; Metallurgical testing; and,
Environmental and societal costassessment
Field Project
Detailed Exploration
Prospect Evaluation
Regional Reconnaissance
Materials extracted or “mined” are rocks composed of both
ore and waste material (part of the rock which contains very
little or no element or mineral of economic value)
STEP 1: MINERAL EXPLORATION
STEP 2: MINE SITE DEVELOPMENTAL AND
OPERATION
STEP 4: LAND RECLAMATION
STEP 3: MILLING PROCESS
Here we can find the 2 Types of Mining
o Open Pit Mining
o Underground mining
STEP 1: MINERAL EXPLORATION
STEP 2: MINE SITE DEVELOPMENTAL AND
OPERATION
STEP 4: LAND RECLAMATION
STEP 3: MILLING PROCESS
Is a naturally occurring coherent aggregate of minerals
such as natural glass or organic matter. Found in the lithosphere
ROCK
ORE
TUFF
MINERALS
Formed from the cooling and solidification of magma or
lava. Also, can form at much higher temperature compared
to other types of rocks.
IGNEOUS ROCKS
SEDIMENTARY ROCKS
METAMORPHIC ROCKS
MESOMORPHIC ROCKS
Are the products of the lithification of particles produced by
the weathering of other preexisting rocks. can have parent material derived from
older igneous, metamorphic, and even sedimentary rocks. They may also
comprised of mineral fragments and organic material, or some cases.
IGNEOUS ROCKS
SEDIMENTARY ROCKS
METAMORPHIC ROCKS
MESOMORPHIC ROCKS
Form when preexisting or parent rocks (whether igneous,
sedimentary, or even metamorphic) are altered by heat,
pressure and chemical activity of fluids. This process is called
metamorphism, meaning change in form.
IGNEOUS ROCKS
SEDIMENTARY ROCKS
METAMORPHIC ROCKS
MESOMORPHIC ROCKS
Process in which rocks change in shape, size, location, tilt or break due to squeezing,
stretching, or shearing.
Tectonic forces operating inside the Earth causes rocks to undergo deformation.
DEFORMATION
STRESS
FAULT
THRUST
is the resulting change in rocks due to the different types of stress.
DEFORMATION
STRESS
STRAIN
THRUST
are the fractures in bedrock (Brittle Rocks) along
which movement has occurred.
FAULTS
STRESS
STRAIN
THRUST
Different kinds of strain can cause rock to stretch, shorten, and even change temporarily
called an _____.
DEFORMATION
STRESS
STRAIN
ELASTIC STRAIN
is a fracture along which no movement has taken place, usually caused by
tensional forces.
DEFORMATION
STRESS
JOINTS
ELASTIC STRAIN
If the forces act uniformly from all directions, also known as
pressure
Uniform stress
Confining stress
Differential stress
Shear Stress
when the weight of the overlying rocks exerts pressure
Uniform stress
Confining stress
Differential stress
Shear Stress
if the force is not equal from all directions
Uniform stress
Confining stress
Differential stress
Shear Stress
dominant force is directed away from each other.
Tensional stress
Compressional stress
Shear stress
dominant force is directed towards each other.
Tensional stress
Compressional stress
Shear stress
two dominant force are directed towards each
other but not along the same axis
Tensional stress
Compressional stress
Shear stress
A stage of Deformation that is characterized by
reversible strain
Elastic Deformation
Ductile Deformation
Permanently Deformed
A stage of Deformation that is irreversable
Elastic Deformation
Ductile Deformation
Permanently Deformed
A stage of Deformation that once it reaches
the elastic limit, it would result to
permanent deformation or fracture.
Elastic Deformation
Ductile Deformation
Permanently Deformed
movement is parallel to the dip of the fault
plane
Dip-Slip Fault
Strike-slip Fault
Normal Fault
Reverse Fault-
the hanging-wall block has moved down
(Tensional stress)
Dip-Slip Fault
Strike-slip Fault
Normal Fault
Reverse Fault-
the hanging-wall block has moved up
(Compressional stress)
Dip-Slip Fault
Strike-slip Fault
Normal Fault
Reverse Fault
the movement is predominantly
horizontal and parallel (Shear stress)
Dip-Slip Fault
Strike-slip Fault
Strike-slip Fault
Oblique-slip Fault
the movement is both vertical and horizontal
Dip-Slip Fault
Strike-slip Fault
Strike-slip Fault
Oblique-slip Fault
a special case of a reverse
fault where the dip of the fault is less
than 45o
Thrust Fault
Left-Lateral Strike-slip Fault
Right Lateral Strike-slip Fault
Folds
Fault: if the block on
the other side has moved to the left, we say
that the fault is a ____.
Thrust Fault
Left-Lateral Strike-slip Fault
Right Lateral Strike-slip Fault
Folds
Fault: if the block on
the other side has moved to the RIGHT, we say
that the fault is a ____.
Thrust Fault
Left-Lateral Strike-slip Fault
Right Lateral Strike-slip Fault
Folds
result from compressional stresses or shear stresses acting over considerable time.
Thrust Fault
Left-Lateral Strike-slip Fault
Right Lateral Strike-slip Fault
Folds
drives plate tectonics. Hot material rises at mid-
ocean ridges and sinks at deep sea trenches, which keeps the plates
moving along the Earth’s surface.
Thrust Fault
Left-Lateral Strike-slip Fault
Right Lateral Strike-slip Fault
Mantle convection
arch-like shape, upward folds.
Anticline
Syncline
Monoclines
trough-like shape, downward folds.
Anticline
Syncline
Monoclines
are the simplest types of folds, gently dipping bends in horizontal rock layers.
Anticline
Syncline
Monoclines
explained that continents had once been joined
together and have slowly drifted apart by some unknown
mechanism
Continental Drift Theory
Big Bang Theory
The flat Earth Theory
The geocentric model theory
explained that continents had once been joined
together and have slowly drifted apart by some unknown
mechanism
Continental Drift Theory
Big Bang Theory
Sea-floor spreading theory
The geocentric model theory
It is a process that occurs at mid-ocean ridges,
where new oceanic crust is formed through volcanic
activity and then gradually moves away from the ridge.
Evidences This means that the sediments are gradually
becoming thicker and older, with increasing distance
away from the center of the ridges.
Continental Drift Theory
Big Bang Theory
Sea-floor spreading theory
The geocentric model theory
Type of plate boundaries that Collide/Move toward.
Convergent Boundaries
Divergent Boundaries
Transform Boundaries
Type of plate boundaries that Move away from/Move apart.
Convergent Boundaries
Divergent Boundaries
Transform Boundaries
Type of plate boundaries that Slide past/Slip away.
Convergent Boundaries
Divergent Boundaries
Transform Boundaries
Where oceanic crust meets ocean
crust. When the interacting plates are
both oceanic, the denser plate
sinks beneath the lighter one
and heads back to the mantle.
Oceanic
-Oceanic Collision
Oceanic
-Continental Collision
Continental
-Continental Collision
Where oceanic crust meets continental crust Oceanic
-continental convergence occurs when
leading edge of one plate is composed of continental rocks
(granitic) and the other is oceanic (basaltic).
Oceanic
-Oceanic Collision
Oceanic
-Continental Collision
Continental
-Continental Collision
Where continental crust meets
continental crust. When colliding plates are both
continental, neither subducts because continental crust are
so buoyant. Instead of subduction zone, what forms
is a collision mountain belt.
Oceanic
-Oceanic Collision
Oceanic
-Continental Collision
Continental
-Continental Collision
Chain of volcanoes are also known as _____.
Volcanic Arc
island arc
Continental volcanic arc
Volcanic Trench
is formed from the
subduction of an oceanic plate beneath another
oceanic plate.
Volcanic Arc
island arc
Continental volcanic arc
Volcanic Trench
is formed from the subduction of oceanic plate beneath continental plate.
Volcanic Arc
island arc
Continental volcanic arc
Volcanic Trench
in the South Pacific Ocean, is formed as the mighty
Pacific plate subducts beneath the smaller, less-dense Philippine plate.
Volcanic Arc
island arc
Continental volcanic arc
Mariana Trench
