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crustal extension ( below(passive) caused bya normal fault
( ex)tensional stress(passive) created byNormal fault
tensional forces where plates diverge(passive) is caused byNormal fault
when tension in the crust tears the rock apartthus creatinga normal fault
The type of stresscausesa normal fault
crust pulls rocks apartcausingnormal fault
normal faults- Tensioncausesa normal fault
tension , which is common in the region(passive) caused bya normal fault
Tension Reverse Fault(passive) Caused by Normal Fault –
Tensional stress , meaning rocks pulling apart from each othercreatesa normal fault
a pulling motioncausesa normal fault
continued ) Tension forces in earths crustcausednormal fault
tensional force within the earth crust(passive) is caused byA normal fault
three main types of faults : Normal faults , reverse faults , & strike - slip faults Tensioncausesa normal fault
rock above the fault moving downward in relation to the rock below the fault 2(passive) caused bynormal fault
tension forces o Reverse fault caused by compression forces o Strike - slip fault caused by shearing forces(passive) caused byNormal fault
tensional crustal forces(passive) caused byNormal fault trough
Faulting(passive) is caused byhighly Normal fault
pulling strength and downward slip(passive) is caused byA normal fault
individuals(passive) created bya normal fault
What type of forcescould causea normal fault
one plate sliding below another(passive) is caused byA normal fault
when there is a fracture in the surface of the earth and the surface moves down(passive) is causedA normal fault
Stress that pulls rock apartcausesa normal fault
students(passive) created bya normal fault
extensional stresses within the upper portion of the Pacific Plate(passive) caused bya normal fault
the stretching of the Earth(passive) caused bya “ normal fault ”
an earthquake(passive) created bya normal fault
Hanging wall moves downcreatinga normal fault
subsidence that compensates for the removed sediment(passive) caused bya normal fault
unroofing(passive) caused bya normal fault
the flexural bending of the European plate in response to the load exerted by the Alps(passive) created bya normal fault
an oblique slip at depth and c shear stress change for left - lateral strike - slip movement on NW - dipping fault due to a combination of blind oblique slip and surface right - lateral slip(passive) caused bya normal fault
This high - angleresultednormal fault
the breakdown of Gondwana(passive) created bya normal fault
post - deposition Pabdeh - Gurpi Formations in Paleocene - Oligocene time that causedto createnormal fault
The earthquake in Chile(passive) was caused byThe earthquake in Chile
from vertical motion of two adjacent blocks under horizontal tensioncan resultfrom vertical motion of two adjacent blocks under horizontal tension
the 1556 Shaanxi earthquakecausedthe 1556 Shaanxi earthquake
the hanging wall to move down to the foot wall Vertical fault 10causesthe hanging wall to move down to the foot wall Vertical fault 10
The study of the mining effect(passive) influenced byThe study of the mining effect
By Earthquake Weekender Tote Bag for Sale by Photo ResearchersCreatedBy Earthquake Weekender Tote Bag for Sale by Photo Researchers
from deformation by tectonic processesresultingfrom deformation by tectonic processes
the fuse in the plug to operate as it is designed to dowould simply causethe fuse in the plug to operate as it is designed to do
a strike - slip faultwill someday causea strike - slip fault
the gap in well 3(passive) is ... caused bythe gap in well 3
Tsunamican also causeTsunami
a sector failure of volcanic edificetriggeringa sector failure of volcanic edifice
The destruction(passive) caused byThe destruction
The L’Aquila event(passive) was caused byThe L’Aquila event
in an elastic half‐spacesetin an elastic half‐space
rocks to bend and then fracture , with each block of rock sliding down the fault planescausesrocks to bend and then fracture , with each block of rock sliding down the fault planes
from extending or depressing the crustresultsfrom extending or depressing the crust
all stations near the downthrown side of the fault to record downward first motionswill causeall stations near the downthrown side of the fault to record downward first motions
70setting70
sedimentary mountains(passive) caused bysedimentary mountains
a Horst and Graben structure ( high and low ) solid breaks from applied stresscreatesa Horst and Graben structure ( high and low ) solid breaks from applied stress
a change in the shape of an object that disappears when stress is removedis createda change in the shape of an object that disappears when stress is removed
through extensioncreatedthrough extension
features like scarps , horsts and grabens , and fault - block mountainscan createfeatures like scarps , horsts and grabens , and fault - block mountains
in the Miocene during the Japan openingcreatedin the Miocene during the Japan opening
huge blocks of rock to tilt upcauseshuge blocks of rock to tilt up
in the Aegean regionsettingin the Aegean region
near the setup roomwas discoverednear the setup room
from Tension as the here three platesResultingfrom Tension as the here three plates
the valley just a few million years agocreatedthe valley just a few million years ago
the Carson Range to the east and the Sierra Nevada to the westcreatedthe Carson Range to the east and the Sierra Nevada to the west
the maximum joint rotation angle(passive) caused bythe maximum joint rotation angle
the northeast - facing front of the Sierra Madrethus creatingthe northeast - facing front of the Sierra Madre