Abeka 8th grade Science Test 2
Circum-Pacific Belt
80% of all earthquakes occur here
shallow focus
85% of earthquakes are this type
Geographic Information System (GIS)
A computer system that stores and processes geographic data from various sources
anticline
A fold in rock that bends upward into an arch
The rocks were polished by rapid motion of the fault
A slickenside is a short cliff along a fault that has been polished smooth. How do slickensides prove evidence for the elastic rebound theory?
seismometer, to detect earthquakes caused by underground pressure
A volcanologist is placing a volcano to help predict when a volcano little rat. What instrument is he most likely to choose?
Modified Mercalli scale, because each location has its own value
After an earthquake, the U.S. Geological Survey often publishes a ShakeMap. The ShakeMap shows how the strength of an earthquake varies throughout the affected area. Which earthquake strength scale is used and why?
True
Among rock beneath the surface of the world is called magma
Molten rock pushes up overlaying rock layers without reaching the surface.
Describe how tall mountains form.
Fixed-base system- base of building is directly on the bed rock. Allows the buildings beams and joints to absorb the seismic energy. The downside to this construction is that the building can be deformed. Base-isolated system- The building rests on isolators that absorb the seismic energy. The isolators act as a movable "skills" that separate the building from the foundation. The building rests on isolators that absorb the seismic energy. The isolators act as movable "stilts" that separates the building from the foundation. Energy-dissipating device- Device is added to structures to absorb some of the seismic energy. This lesson is the stress on the building, minimizing the formation.
ESSEY: An engineer is designing a new steel skyscraper that will be built in an area that receives frequent earthquakes. He needs to choose one technique to use to reduce the damage the building will receive in an earthquake. Compare two different techniques that he could used to reduce earthquake damage. Recommend one of the techniques; give reasons why you chose that technique instead of the other one.
p waves
Faster type of earthquake waves are S waves
aa
Harden lava that form is rough, jagged rocks with a crumbly texture
Most volcanoes the peer to be located along a subduction zones
How does the existence of the ring of fire proof evidence for plate to tonics?
volcanic blocks
Large, irregular shaped lump made of lava that harden before being thrown out of a volcano
pillow lava
Lava and water solidifies almost instantly, forming rounded structures
Point IV is 60 feet higher
Point IV is 60 feet higherWhat is the approximate difference in elevation between point I and IV?
true
Small earthquakes that often thought of a large earthquake at circle intervals are called aftershocks
lapilli
Solid eject a larger than 2mm but less than 64 mm in diameter
geology
Study of the earth
pyroclastic flow
Superheated cloud of gas and small particles that travel as an avalanche
core
The central part of the earth below the mantle
igneous intrusion
The general name for a massive underground volcanic rock is a caldera
Solid
The inner core of the earth is thought to be what?
Volcanic Explosivity Index (VEI)
The strength of a volcano eruption is measured using a scale called the what?
seismology
The study of earthquakes
magma chamber
The underground lava tunnel is the actual source of a volcanic eruption.
A dike is vertical; a sill is horizontal
What is the main difference between a dike and a sill?
Point II
Which point has the steeper slope?
Modified Mercalli Scale
a 12 point scale developed to evaluate earthquake intensity based on the amount of damage to various structures
volcanic mountian
a type of mountain formed when molten rock erupts from a whole in the earth's crust
dormant volcano
an inactive volcano that could erupt again
volcano
an opening in the earth's surface through which hot gases, ash, and molten rock are ejected from the earth's interior
Moho
boundary between crust and mantle
A low-viscosity magma most likely...
causes a volcanic eruption to be violent
moment magnitude scale
considered the most reliable method for measuring an earthquake's magnitude
sediments
deposits of sand, mineral fragments, or organic materials usually left by wind or water
Earth's interior
earthquake waves can provide us with information about
Alpide belt
earthquake zone stretching from southern Europe to Indonesia
tectonic earthquakes
earthquakes that result from sudden movements of rock beneath the earth's surface
lava tunnels
form when the surface of a large lava flow hardens but the lava beneath remains molten and continues to flow
composite volcano
forms partly through explosive eruptions of cinders from the crater and partly through mild lava flows that pour out of cracks on the cone's flanks
pahoehoe
hardened lava with a surface that is either smooth or ropy
measuring travel time of seismic waves
how scientists determine the point where an earthquake begins
calderas
huge bowl shaped craters thought to form when the magma chamber beneath a volcano is emptied of magma causing it to collapse under its own weight
catastrophic plate tectonics
idea that rapid movement of tectonic plates during the Flood is responsible for most of Earth's features
volcanic bombs
large almond or teardrop shaped pieces of ejecta formed when lava solidifies after being thrown high into the air
true
mass of underground volcanic rock that is similar to a laccolith but much larger is a batholiths
oxygen
most abundant element in the earth's crust
pyroclast
particles or blocks of solid volcanic ejecta
Asthenosphere
plastic rock on which the tectonic plates float is called the lithosphere
hypocenter (or focus)
point below the surface where earthquake begins
epicenter
point on Earth's surface directly above an earthquake's focus
thrust fault
results when rocks on one side of a fault are shoved on top of the rocks on the other side
elastic rebound theory
rocks on either side of a fault spring back to a position of little or no strain at the moment of an earthquake, triggering vibrations in the earth's crust
volcanic ash
solid particles less than 2mm in diameter
transition zone
the area between the upper mantle and the lower mantle
core-mantle boundary
the bottom of the mantle
vent
the channel in a volcano through which gases, ash, and molten rock are ejected from the earth's interior
crust
the earth's outer layer made of solid rock
fault
the fracture zone between stationary and moving rocks
mantle
the middle of the earth's three main layers
folded mountains
these are thought to have formed when the edges of two adjacent tectonic plates were pushed together, causing the layers to buckle like a wrinkled rug
Seismograph
used to record the vibrations caused by earthquakes
extinct volcano
volcano that is unlikely to erupt again
cinder-cone volcanoes
volcanoes that consist primarily of erupted volcanic ash and rock fragments called cinders