PP.1 Mid-Unit Content Assessment
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Last updated almost 3 years ago
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| Draggable item | arrow_right_alt | Corresponding Item |
|---|---|---|
mantle | arrow_right_alt | Earth’s largest and thickest layer; consists of very hot, very dense rock |
crust | arrow_right_alt | solid; made of very hot metal; may be nearly as hot as the sun’s surface; innermost layer |
outer core | arrow_right_alt | thin; rocky; outermost layer; two types: oceanic and continental |
inner core | arrow_right_alt | liquid; made of very hot metal |
Yes | No | |
|---|---|---|
Tsunamis form when earthquakes occur in oceanic crust, causing the seafloor to shift. | ||
Tsunamis travel fast—as much as 500 miles per hour. | ||
Tsunamis are easy to stop as long as scientists have enough warning when they begin to form. | ||
Tsunamis can grow to become as tall as a three- or four-story building. |
active | dormant | extinct | |
|---|---|---|---|
a volcano that has not erupted for at least 10,000 years and is not likely to erupt again | |||
a volcano that has erupted in the past 10,000 years and is likely to erupt again | |||
a volcano that hasn’t erupted for a long time but could erupt again |
Yes | No | |
|---|---|---|
long ago, Earth had one huge landmass called Pangaea | ||
as continents moved apart, their climates changed | ||
drifting continents actually moved due to tectonic plates | ||
groups of plants and animals that once lived together were separated as the continents moved apart |
| Draggable item | arrow_right_alt | Corresponding Item |
|---|---|---|
Richter scale | arrow_right_alt | Numbers describe the intensity of earthquakes based on the largest seismic wave recorded. |
Seismograph | arrow_right_alt | Jagged up-and-down lines show the energy of seismic waves. |