els prefinals Flashcards

1
Q
  • this is the earliest hypothesis on the origin of life. I know
    everyone is familiar with the creation. There is a Supreme Being that created
    everything for 6 days. This is a core belief in most of the religions but there is no
    found evidence to support this theory.
A

Special Creation

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2
Q
  • it is somewhat similar to creation theory in that
    it states that living organisms just unexpectedly came to life. According to this
    theory that living organism arise from non-living things. Aristotle believes that all
    things are full of soul so that, living or nonliving, everything can generate life. It is
    also called as ABIOGENESIS.
A
  1. Spontaneous Generation
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3
Q

-bio (life) and genesis (beginning). It is the theory that living
things come from other living things particularly of the same type. For example:
kitten came from cats.

A
  1. Biogenesis
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4
Q
  • “seeds everywhere”. This theory states that life had come to
    Earth from other planets in the universe in the form of bacterial spores.
A
  1. Panspermia
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5
Q
  • Life first arose from a collection of chemical
    substances by a progressive series of reactions that took place about 3.8 billion
    years ago. That time Earth is enduring heavy bombardment. Early Earth’s surface
    and atmosphere was hot and violent. Solar radiation and lightning must have
    been the chief energy source for these chemical reactions.
A
  1. Chemical Evolution
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6
Q

The biological levels of organization of living things follow a hierarchy
arranged from the simplest to most complex.

A

Levels of Organization

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7
Q

Moving, growing, reproducing and other activities of life require energy.
Without energy, life stops. Energy enters the ecosystem as sunlight. Plants, as a
producers convert light energy to chemical energy in the process called
photosynthesis.
Sugars, fats and other “fuel-like” molecules in the food serve as a fuel for
animals that eat them. From that there is already an interaction between
organisms and their environment.

A

The Flow of Energy

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8
Q

The theory of evolution explains how all kind of organisms came into
existence and their changes over long periods of time. I t also explains the
relationships among diverse groups of living organisms.

The only constant in this world is CHANGE. Life forms are slowly changing
and actually been changing. Adaptation allows life forms to acquire new
characteristics in response to their environment through the process of natural
selection. For example: some animals make their coats lightened to facilitate
hiding from predators.

A

Evolution

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9
Q

There is an interaction between living organisms and environment. A
living community is structured and interdependent, meaning all organisms in
ecosystem depend on each other. If one of them rises or fall, this can affect the
rest of the ecosystem. We call this interdependence.

For example: the coevolution (occurs when two or more species
reciprocally affect each other’s evolution) of flowering plants and insects has
been responsible for the diversity of both species.

A

Interacting System

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10
Q

The relationship between structure and function is evident in the entire
organism and the physiological systems that serve them. The structure determines
function, function reflects structure so technically, they are inseparable.
Within many kinds of organisms in the living world, body structures appear
to be carefully designed to bring out their purpose.

A

Structure and Function

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11
Q

It is branch of science that deals with the study of complex communities of
organisms in relation to their environment. No organism is completely secluded
from its surroundings. As part of the ecology, each organism continuously interacts
with the environment. For example: plants obtain water and nutrients from the
soil, carbon dioxide from the air and energy from sunlight. The key process in an
ecosystem is the transfer of chemicals between organisms and their
environment—breathing, drinking water, eating food and getting rid of wastes.

A

Ecology

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12
Q

Through science, humans learn about the solution to various problems. The
scientific method is able to give direction and pace for every inquiry and
technology produced machinery to lengthen the life of perishable goods.
Through the application of scientific discoveries provide comfort and
improvement to human life.

A

Science and Society

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13
Q

are landscape-changing processes that originates from inside or
beneath the surface of the Earth. These processes gets its energy from within the Earth in
the form of heat from radioactive decay from the core. This heat in turn, is transferred
upward to warm the mantle through convection currents.

A

Endogenic Processes

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14
Q

create
relief. It is defined as the difference in elevation
between the highest and the lowest points within a
specified area or on a particular surface feature.

A

In geology terms, endogenic processes

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15
Q

tend to increase the
amount of surface relief (that is, increase the
height/create a landform or increase the thickness
of the crust), while the exogenic processes work to
decrease relief.

A

Endogenic processes

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16
Q

In the early 20th century,— proposed that all of Earth’s continents were
once part of an enormous, single landmass called Pangaea

A

Alfred Wegener

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17
Q

These forces, which at the largest scale move the lithospheric plates, also cause bending,
warping, folding, and fracturing the Earth’s crust at continental, regional, and even local
scales.

A

Tectonic forces.

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18
Q

When two forces push towards each other from opposite sites, the rock layers will bend
into folds. The process by which folds are formed due to compressional forces is known as
folding.

A

FOLDING

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19
Q

An upward fold is called

an ,

A

anticline

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20
Q

a downward fold is called a . .

A

syncline

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21
Q

A plane drawn through the crest of a fold in a series of beds
is called the

A

axial plane of the fold.

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22
Q

The sloping beds on either side of an axial plane are

.

A

limbs

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23
Q

An anticline or syncline is described as — if the angles between each of
limb and the axial plane are generally similar, and asymmetrical if they are not.

A

symmetrical

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24
Q

If the
axial plane is sufficiently tilted that the beds on one side have been tilted past vertical, the
fold is known as an

A

overturned anticline or syncline

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25
Q

A break in rock along which a vertical or horizontal rock movement has occurred is
called a fault.

A

FAULTING

26
Q

is the fracturing (breaking) and displacement of more brittle rock
strata along a fault plane either caused by tension or compression.

A

Faulting

27
Q

The line of fault which
appears on land surface is known as —. These lines are often lines of weakness
which allow molten rock to rise up onto the earth surface when there is active volcanic
activity nearby.

A

fault line

28
Q

The three basic types of fault are

A

normal, reverse, and strike-slip.

29
Q

is one in which the rocks above the fault plane (hanging wall), move
down relative to the rocks below the fault plane (footwall).

A

Normal fault

30
Q

is one in which
the hanging wall moves up relative to the footwall. When rocks on either side of a nearly
vertical fault plane move horizontally, the movement is called strike-slip.

A

Reverse fault

31
Q

plays a very important role in our planet. It is one of the factors that
makes the Earth to be able to harbor life. I

A

Heat energy

32
Q

Sources of heat in our planet can be identified as

A

Primordial and Radioactive heat.

33
Q

During the early formation of the Earth, the internal heat energy that gradually gathered
together by means of dispersion in the planet during its few million years of evolution is
called —-. It is the heat from accretion and bombardment of the Earth during
the early stages of formation (Solar Nebular Theory). The heat was produced due to
friction. For example, if you hit a hammer on hard surface several times, the metal in the
hammer will heat up (kinetic energy is transformed into heat energy).

A

Primordial heat

34
Q

This heat is constantly lost to the outer
silicate layers of the mantle and crust of the
earth through convection and conduction. In
addition, the heat of the core takes tens of
thousands of years to reach the surface of
the earth.

A

Primordial heat

35
Q

On the other hand, the thermal energy released as a result of spontaneous nuclear
disintegration is called

A

Radioactive Heat.

36
Q

It involves the disintegration of natural
radioactive elements inside the earth like Uranium (U), Thorium (Th) and Potassium (K).
Uranium is a special kind of element because when it decays, radioactive heat is
produced. Estimated at 47 terawatts (TW), the flow of heat from Earth’s interior to the
surface and it comes from two main sources in equal amounts: the radioactive heat
produced by the radioactive decay of isotopes in the mantle and crust and the primordial
heat left over from the formation of the Earth.

A

Radioactive elements

37
Q

exist everywhere on
the earth in a fairly significant concentration. Without the process of radioactive decay,
there would be fewer volcanoes and earthquakes and less formation of earth’s vast
mountain ranges.

A

Radioactive elements

38
Q

Three

processes can transfer heat:

A

conduction, convection, and radiation.

39
Q

can be defined as the process by which heat energy is transmitted
through collisions between neighboring atoms or molecules. Heat from the Earth’s core
and radiation from the Sun is transferred to the surface of the Earth by conduction.
Contact of the atmosphere with these warm surfaces transfers thermal energy, which then
heats up the rest of the air through convection.

A

Conduction

40
Q

involves transfer of heat by the movement of mass, which is a more
efficient means of heat transport in the Earth compared to pure conduction. Convection
dominates the thermal conditions in the zones where large quantities of fluids (molten
rocks) exist, and thus governs the heat transport in the fluid outer core and the mantle. In
geological time scale, the mantle behaves as a viscous fluid due to the existence of high
temperatures. In convection current, the mantle of the earth moves slowly because of
transfer of heat from the interior of the earth up to the surface. This result to the movement
of tectonic plates.

A

Convection

41
Q

is the least important mode of heat transport in the Earth. The process
of heat exchange between the Sun and the Earth, through radiation, controls the
temperatures at the Earth’s surface. Inside the Earth, radiation is significant only in the
hottest parts of the core and the lower mantle.

A

Radiation

42
Q

(PHIVOLCS),

A

Philippine Institute of Volcanology and Seismology

43
Q

is composed of semi-liquid hot molten rocks located beneath the Earth,
specifically in the melted mantle rock and oceanic plate. This molten material, when cooled
and solidified, creates igneous rocks.

A

Magma

44
Q

. is

found in the magma chamber of the volcano

A

Magma

45
Q

while —- is found on the surface of earth

once the volcano erupts.

A

lava

46
Q

is a process under the earth’s crust where formation

and movement of magma occur.

A

Magmatism

47
Q

So where does these formation and movement (MAGMA) take

place?

A

These happen in the lower part of the Earth’s crust and in the upper portion of the
mantle, known as asthenosphere.

48
Q

The magma present in the lower crust and upper mantle of the Earth is formed or
generated through the process of —- In this process, different minerals in
rock melt at different temperature and pressure. Another factor being considered in this
process is the addition of volatile materials such as water and carbon dioxide. This is the
reason why magma exhibits plasticity.

A

partial melting.

49
Q

Melting in the mantle requires one of three possible events to occur:

A
  1. An Increase in Temperature:
  2. A Decrease in Temperature:
  3. Addition of Volatiles:
50
Q

Conduction in mantle
happens when heat is transferred from hotter molten rocks
to the Earth’s cold crust. This process is known as heat
transfer. As magma rises, it is often hot enough to melt the
rock it touches. It happens at convergent boundaries,
where tectonic plates are crashing together. The
temperature of mantle is around 1200 degrees Celsius.
Rock minerals such as quartz and feldspar begin to partially
melt at around 650-850 degrees Celsius.

A
  1. An Increase in Temperature:
51
Q

: Mantle rocks remain
solid when exposed to high pressure. However, during
convection, these rocks tend to go upward (shallower level)
and the pressure is reduced. This triggers the melting of
magma. This is known as decompression melting. This
process occurs at the Mid-Ocean Ridge, an underwater
mountain system.

A
  1. A Decrease in Temperature
52
Q

When water or carbon dioxide
is added to hot rocks, flux melting occurs. The melting
points of minerals within the rocks decrease. If a rock is
already close to its melting point, the effect of adding these
volatiles can be enough to trigger partial melting. It occurs
around subduction zones.

A
  1. Addition of Volatiles:
53
Q

is an opening in the ground where molten rocks comes out from inside the
earth. Contrary to popular belief, a— is a not always cone-shaped like a mountain
or a hill. It can be just a simple opening in the ground, such as a fissure or a crack.
Volcanoes may be classified into three groups.

A

A volcano

54
Q

are
volcanoes constructed of pyroclasts (fragments
of rock formed by volcanic explosion ejected
from a central vent. These pyroclasts build up to
form steep slopes whose inclination may be as
much as 40° from the horizontal. The famous of
all cinder volcano is Mount Paricutin in Mexico.
Its formation was witnessed by geologists from
start to finish.

A

Cinder Cones (Pyroclastic Cones)

55
Q

may grow to be very large
volcanoes. That is because they undergo
repeated eruptions that add more and more
material to the slopes. Shield volcanoes are
built of very fluid basaltic lava. When the lave
reaches the earth’s surface, it spreads out the
ways liquid do. That is why shield volcanoes
have gentle slopes. The island of Hawaii is
composed of several shield volcanoes. The
largest is Mauna Loa, which is about 9 km high
when measured from the base at the bottom of
the Pacific Ocean up to the summit

A

Shield Cones

56
Q

are volcanoes which exhibit the classic volcano
shape that we are all familiar with. One of the
famous composite volcanoes is Mount Mayon in
Albay, in the Bicol region, with its nearly perfect
cone.

A

Composite Volcanoes (Stratovolcanoes)

57
Q
  • named after Vulcano Island near Stromboli, generally involves
    moderate explosions of gas laden with volcanic ash. This mixture forms dark, turbulent
    eruption clouds that rapidly ascend and expand in convoluted shapes.
A

Vulcanian type

58
Q
  • is associated with explosive outbursts that generate pyroclastic flows,
    dense mixtures of hot volcanic fragments and gas. This is named after the Mt. Pelee on
    the Carribean Islands. The fluidized slurries produced by these eruptions are heavier
    than air but are of low viscosity and pour down valleys and slopes at great velocities. As
    a result, they are extremely destructive.
A

Pelean type

59
Q
  • In this type of eruption, gases boiling out of gas-rich magma generate
    enormous and nearly continuous jetting blasts that core out the magma conduit and rip it
    apart. The uprushing gases and volcanic fragments resemble a gigantic rocket blast
    directed vertically upward. Plinian eruption clouds can rise into the stratosphere and are
    sometimes continuously produced for several hours.
A

Plinian type

60
Q
  • characterized by effusions of molten basaltic lava that flow
    from long, parallel fissures. Such outpourings often form lava plateaus.
A

Icelandic type eruption

61
Q
  • fluid lava flows from a volcano’s summit and radial fissures to
    form shield volcanoes, which are quite large and have gentler slopes.
A

Hawaiian type eruption

62
Q
  • involves moderate bursts of expanding gases that ejects clots of
    incandescent lava in cyclical or nearly continuous small eruptions. Named after
    Stromboli Volcano, in Italy.
A

Strombolian type