TECTONICS Flashcards

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1
Q

TECTONIC HAZARDS - WHAT ARE THEY ???

A

EARTHQUAKES AND VOLCANIC ERUPTIONS
PLUS SECONDARY HAZARDS
SUCH AS TSUNAMI

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2
Q

CAN BE CLASSIFIED AS EITHER ??

A

SEISMIC OR VOLCANIC

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3
Q

GLOBAL DISTRIBUITON OF TECTONIC HAZARDS - EARTHQUAKES

A

FAR FROM RANDOM !

MAIN EARTHQUAKE ZONES FOUND ALONG PLATE BOUNDARIES.

ABOUT 70% OF ALL EARTHQUAKES ARE FOUND IN THE “RING OF FIRE” IN THE PACIFIC OCEAN

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4
Q

SEISMIC HAZARDS - DESCRIBE ??

A

GENERATED WHEN ROCKS WITHIN 700 KM OF THE EARTHS SURFACE COME UNDER SUCH STRESS THAT THEY BREAK AND BECOME DISPLACED

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5
Q

VOLCANIC HAZARDS - DESCRIBE ??

A

ASSOCIATED WITH THE ACTUAL ERUPTION EVENTS

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6
Q

VOLCANO - WHAT IS THIS ??

A

A LANDFORD THAT DEVELOPS AROUND A WEAKNESS IN THE EARTH’S CRUST FROM WHICH MOLTEN MAGMA, DISRUPTED FROM PRE-EXISTING VOLCANIC ROCK AND GASES ARE EJECTED OR EXTRUDED

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7
Q

INTRA PLATE EARTHQUAKES

A

OCCUR IN THE MIDDLE OR INTERIOR OF TECTONIC PLATES AND ARE MUCH RARER THAN BOUNDARY EARTHQUAKES

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8
Q

GLOBAL DISTRIBUTION OF TECTONICS HAZARDS : VOLCANOES

A

THE VIOLENCE OF A VOLCANIC ERUPTION IS DETERMINED BY

THE AMOUNT OF DISSOLVED GASES IN THE MAGMA AND HOW EASILY THE GASES CAN ESCAPE

ABOUT 500 ACTIVE VOLCANOES THROUOUT THE WORLD

ON AVERAGE AROUND 50 ERUPT EACH YEAR

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9
Q

PLATE BOUNDARY - 3 TYPES

A

DIVERGENT
CONVERGENT
CONSERVATIVE

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10
Q

PLATE TECTONICS - WHAT IS THIS ??

A

A THEORY DEVELOPED > 60 YEARS AGO TO EXPLAIN THE LARGE-SCALE MOVEMENTS OF THE LITHOSPHERE (OUTERMOST LAYER OF THE EARTH)

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11
Q

LITHOSPHERE - WHAT IS THIS ??

A

OUTERMOST LAYER OF THE EARTH

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12
Q

DIVERGENT PLATE BOUNDARY - DESCRIBE

A

CONSTRUCTIVE MARGINS

MOST CLEARLY DISPLAYED AT MID-OCEAN RIDGES.

LARGE NUMBERS OF SHALLOW FORCES

GENERALLY LOW MAGNITUDE

MOST ARE SUBMARINE(UNDER THE SEA)

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13
Q

CONVERGENT PLATES - DESCRIBE

A

PLATES MOVE TOGETHER

ACTIVELY DEFORMING COLLISION LOCATIONS WITH PLATE MATERIAL MELTING THE MANTLE,

CAUSING FREQUENT EARTHQUAKES AND VOLCANOES

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14
Q

CONSERVATIVE PLATES - DESCRIBE

A

OBLIQUE-SLIP,SLIDING OR TRANSFORM

MARGINS WHERE ONE PLATE SLIDES AGAINST ANOTHER

RELATIVE MOVEMENT IS HORIZONTAL AND CLASSIFIED AS EITHER
SINISTRAL (TO THE LEFT)
OR
DEXTRAL (TO THE RIGHT)

LITHOSPHERE IS NEITHER CREATED NOR SUBDUCTED

DO NOT RESULT IN VOLCANIC ACTIVIITY

THEY ARE THE SITES OF EXTENSIVE SHALLOW FOCUS EARTHQUAKES
OCCASIONALLY OF CONSIDERABLE MAGNITUDE

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15
Q

CONTINENTAL INTERIORS

A

SCATTERED EARTHQUAKES

ALONG OLD FAULT LINES AND IS ASSOCIATED WITH THE REACTIVATION OF THIS WEAKNESS EG CHURCH STRETTON FAULT IN SHROPSHIRE

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16
Q

EARTHQUAKES -

A

ARE A COMMON HAZARD

PRIMARY HAZARDS (GROUND MOVEMENT AND GROUND SHAKING)

SECONDARY HAZARDS LIKE LANDSLIDES AND TSUNAMIS CAN BE DEVELOP FROM THE EARTHQUAKE

CAN DEVELOP INTO A DISASTER ESPECIALLY WHEN THE EARTHQUAKES HAVE BOTH -

HIGH MAGNITUDE AND
OCCUR IN DENSELY POPULATED AREAS

17
Q

WAYS OF PLATES MOVEMENT - X3

A

PULL AWAY FROM EACH OTHER

SLIDE PAST EACH OTHER

CRUNCH INTO EACH OTHER

18
Q

PLATE MOVEMENT AND EARTHQUAKE TYPE

WAYS OF MOVEMENT - X3

A

PULL AWAY FROM EACH OTHER

SLIDE PAST EACH OTHER

CRUNCH INTO EACH OTHER

19
Q

PLATE MOVEMENT AND EARTHQUAKE TYPE

WAYS OF MOVEMENT - X3

A

PULL AWAY FROM EACH OTHER ( DIVERGENT)

SLIDE PAST EACH OTHER (COVERGENT)

CRUNCH INTO EACH OTHER (CONSERVATIVE)

20
Q

DIVERGENT PLATES (MOVE AWAY FROM EACH OTHER )

IMPACTS ??

A

DIVERGENT “SPREADING RIDGES” IN THE OCEANS

NEW OCEANIC CRUST = THINNER AND DENSER THAN THE CONTINENTAL CRUST IS CREATED.

FREQUENT SMALL EARTHQUAKES

TYPICALLY LOW HAZARD RISK, AS OCEAN BASED

DO NOT TYPICALLY TRIGGER TSUNAMIS

21
Q

SLIDE PAST EACH OTHER

A
PRESENTS MORE RISK
SAN ANDREAS FAULT, CALIFORNIA
PACIFIC PLATE (MOVING NORTH)
ZONE OF FRICTION
AGAINST THE NORTH ATLANTIC PLATE  (MOVING NORTH ALSO BUT AT A DIFFERENT SPEED )
22
Q

CRUNCH INTO EACH OTHER OR MOVING TOWARDS EACH OTHER (SUBDUCTION)

A

GENERATES THE LARGEST AND MOST DAMAGING EARTHQUAKES AND CAUSES THE EMERGENCE OF MOUNTAINS/MOUNTAIN RANGES LIKE THE HIMALAYAS AND

The friction of the movement can also melt rocks and produce volcanoes.
This is also part of the rock cycle, because the plate that dives under the other one becomes part of the mantle and emerges much later from volcanoes and in seafloor spreading.

sometimes bends the other down into a deep seafloor trench.

23
Q

DESTRUCTIVE PLATE BOUNDARIES - WHAT HAPPENS HERE ??

A

Sometimes called convergent or tensional plate margin.

Occurs when oceanic and continental plates move together.

The oceanic plate is forced under the lighter continental plate.

Friction causes melting of the oceanic plate and may trigger earthquakes.

24
Q

CONSTRUCTIVE PLATE BOUNDARIES - WHAT HAPPENS HERE ??

A

SOMETIMES CALLED DIVERGENT PLATE MARGIN

AT OCEANIC RIDGES AND FORMS young fold mountains, rift valleys, ocean ridges, deep sea trenches and island arcs