4. Earth: Adding circumstances๏
Time (when?) โ over long periods, during earthquakes
Place (where?) โ along active fault zones, at mid-ocean ridges
Manner (how?) โ by subduction, by erosion, by volcanism
Cause (why?) โ due to volcanism, as a result of erosion
4.1. Prepositional phrases as circumstances๏
4.2. Example mobility test๏
4.3. Igneous rock circumstances๏
Short Answer Questions
For each clause, write it twice: once with the circumstance at the end, and once at the front. Choose from:
along active fault zones
at convergent boundaries
beneath volcanic regions
during major seismic events
over long periods
Time. Water erodes weakened rock.
Place. Pressure fractures the crust.
Place. Subduction destroys oceanic crust.
Place. Heat weakens the crust.
Time. Strong building design reduces earthquake damage.
Reveal Answer Key
Water erodes weakened rock over long periods.
Over long periods, water erodes weakened rock.
Pressure fractures the crust along active fault zones.
Along active fault zones, presssure fractures the crust.
Subduction destroys oceanic crust at convergent boundaries.
At convergent boundaries, subduction destroys oceanic crust.
Heat weakens the crust beneath volcanic regions.
Beneath volcanic regions, heat weakens the crust.
Strong building design reduces earthquake damage during major seismic events.
During major seismic events, strong building design reduces earthquake damage.
Short Answer Questions
For each clause, write it twice: once with the circumstance at the end, and once at the front. Choose from:
at convergent boundaries
at mid-ocean ridges
during earthquakes
during seismic rupture
Time. Seismometers detect ground movement.
Place. Magma creates new oceanic crust.
Place. Plates compress the crust.
Time. Plates slip along faults.
Reveal Answer Key
Seismometers detect ground movement during earthquakes.
During earthquakes, seismometers detect ground movement.
Magma creates new oceanic crust at mid-ocean ridges.
At mid-ocean ridges, magma creates new oceanic crust.
Plates compress the crust at convergent boundaries.
At convergent boundaries, plates compress the crust.
Plates slip along faults during seismic rupture.
During seismic rupture, plates slip along faults.
4.4. Sedemetary Rock circumstances๏
Short Answer Questions
For each clause, write it twice: once with the circumstance at the end, and once at the front. Choose from:
in river deltas
in shallow seas
in the pore spaces
over millions of years
under great pressure
Time. Rivers transport sediment downstream.
Place. Sediment layers accumulate.
Place. Shell fragments and organic matter settle.
Manner. Compaction transforms loose sediment into rock.
Place. Minerals cement sediment grains together.
Reveal Answer Key
Rivers transport sediment downstream over millions of years.
Over millions of years, rivers transport sediment downstream.
Sediment layers accumulate in river deltas.
In river deltas, sediment layers accumulate.
Shell fragments and organic matter settle in shallow seas.
In shallow seas, shell fragments and organic matter settle.
Compaction transforms loose sediment into rock under great pressure.
Under great pressure, compaction transforms loose sediment into rock.
Minerals cement sediment grains together in the pore spaces.
In the pore spaces, minerals cement sediment grains together.
4.5. Metamorphic Rock circumstances๏
Short Answer Questions
For each clause, write it twice: once with the circumstance at the end, and once at the front. Choose from:
along tectonic plate boundaries
deep within the crust
through contact with magma
over millions of years
from limestone during metamorphism
Place. Slate forms.
Place. Schist develops.
Manner. Quartzite forms.
Matter (Origin). Marble forms.
Reveal Answer Key
Slate forms along tectonic plate boundaries.
Along tectonic plate boundaries, slate forms.
Schist develops deep within the crust.
Deep within the crust, schist develops.
Quartzite forms through contact with magma.
Through contact with magma, quartzite forms.
Marble forms from limestone during metamorphism.
From limestone during metamorphism, marble forms.