Whopper Day 3 Flashcards
Please just end this suffering already
Dense ball of solid metal
Inner Core
Layer of molten metal that surrounds inner core
Outer Core
Solid material extending all the way to the Earth’s cpre
Lower Mantle
Uppermost part of the mantle and the crust for a ridge layer about 100 kilometers thick. (Asthenosphere)- Softer part part below this part, which is hotter, and under increased pressure
Upper Mantle (Lithosphere)
Layer of solid rock that forms the Earth’s outer “skin”
*Includes both dry land and ocean floor . Oceanic ____ consists of basalt. Continental _____ is mainly granite
Crust
Lithosphere is broken into separate sections called _____
Plates
Explains the formation, movement and subduction (Sideways or downward movement) of Earth’s plates
Plate Techtonics
The transfer of energy through empty space has no direct contact between heat source and object
(Sun, heat lamp, microwave, or fire place)
Radiation
Heat transfer by direct contact of particles of matter.
(Metal spoon in soup,
Conduction
Transfer of heat by the movement of hot fluid (Includes liquid and gasses) caused by differences in temperature and density within the fluid
(Heating water on stove)
Convection
A slow movement of Earth’s continents moving away from each other. They have been doing this for billions of years
Continental Drift
Sea floor spreads apart along both dies of a mid-ocean ridge as new crust is added. Ocean floors move like a conveyor belt, carrying continents along with them
Sea Floor spreading
3 Plate Boundaries
Transform boundary- Place where 2 plates slip past each other, moving in opposite directions (Frequent earthquakes)
Divergent boundary- 2 plates move apart, or diverge usually occur at the mid-ocean ridge
Convergent boundary- Place where 2 plates come together causing a collision.
3 Scientists That Contributed to Plate Tectonics Theory and What They Each Discovered
J. Tuzo Wilson, Harry Hess, and Alfred Wegner
J. Tuzo Wilson was a Canadian scientist that proposed the lithosphere was broken into separate sections called plates. He also combined information from continental drift, sea floor spreading and Earth’s plates which is the theory of “Plate Tectonics”
Harry Hess had a theory of Seafloor spreading
Alfred Wegner had the theory of Continental Drift
(Evidence from land features such as mountain ranges lining up on a continent when pieced together)
Convection in Mantle
Convection currents flow in the mantle-heat source is the Earth’s core and mantle. the convection currents act like a conveyor belt moving the lithosphere above
If new crust is added to the Earth through Seafloor spreading, why doesn’t the Earth continue to get bigger
Seafloor spreads apart along both sides of a mid-ocean ridge as new crust is added. The ocean floors move like a conveyor belt , carrying continents along with them . Eventually, the ocean floor sinks into deep trenches
What are two (THREE) pieces of evidence that shows that continents were once all together in one landmass
There are three 3 pieces of evidence that shows that there was something called Pangaea. First, the land features lined up with different parts of the world. Secondly, Climate change, showed scratches on rocks made from glaciers in places with much more mild climate today. And LASTLY, the remaining bones from dinosaurs in different parts of the world
Constantly changes over time due to plate tectonics. Forces at plate boundaries are strong enough to break rocks or change their shape
Continental Crust
Physical force that acts on rocks to change its shape or volume
Stress
Pulls on the crust, stretching rocks so it becomes thinner in the middle
(Mid-ocean ridge, continental rifts)
Tension
Squeezes rocks until it folds or breaks
Mountain ranges, ocean trenches, and volcanic arc
Compression
Pushes a mass of rocks in two opposite directions
Fault zones
Shearing
A change of rock caused by two types of stress
Strain
Change in rock that is not permanent
Elastic Strain
Creates a permanent change in the shape of a rock; usually occurs when rocks are weak and hot
Plastic Strain
Vibrations in the ground that result from movement along the faults breaks in Earth lithosphere
Earthquakes
Forms when forces pull rocks apart along divergent plate boundary; block above fault moves down
Normal Fault
Two blocks of rock slide horizontally in opposite direction
Strike Slip Fault
Force pushes two blocks of rock together with the rock above the fault moving
Reverse Fault
Point beneath Earth’s surface where rocks under stress break and causes an earthquake
Focus
Point on the surface directly above the focus
Epicenter
Waves that carry energy of an earthquake away from the focus. There are 3 different waves, the Primary waves, Secondary waves, and Surface waves
Seismic waves
Compression waves travel through solid and liquids compressing and expanding the material they pass through, temporarily changing volume (Fastest)
Primary Waves (Push and pull)
Only travel through solids and temporally change shape, but not the volume of the material they pass through
Secondary Waves (Comes second/Side to side)
Move slower than the other waves but can produce severe ground movement with wave like motion (up above the surface)
Surface waves (Slowest)
Weak spots in the Earth’s crust where molten material or magma, comes to the surface
Volcano