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SCI LT REVIEW

1ST QUARTER, 10-DOCILITY

QuestionAnswer
Earth's Layers, there are 2 types we can refer to COMPOSITIONAL AND MECHANICAl.
consists of crust, mantle, and core. COMPOSITIONAL
It is the outmost layer of the earth, the least dense of all the layers, and is divided into 2 types; continental crust and oceanic crust. CRUST
is thicker than the other but it is less dense Continental crust
is less thicker than Continental crust, yet it is denser than the other. Oceanic crust
Thickest layer, and is denser than the crust. It also consists of semisolid, rocky, and very hot layer MANTLE
The densest layer of the Earth, and is the innermost part of it. CORE
Consists of Lithosphere, Asthenosphere, Mesosphere, Outer core, and Inner core. MECHANICAL
a combination of the lower part of the crust and the uppermost part of the mantle, it also has what we call plates or tectonic plates. LITHOSPHERE
Located below the mantle ASTHENOSPHERE
Located within a portion of the mantle, right below the Asthenosphere. MESOSPHERE
It is a liquid that is made of molten rocks. OUTER CORE
unlike the outer core, is not liquid or molten. Due to the temperature, it makes the pressure intense which prevents melting INNER CORE
are created by Earthquakes, Volcanic Eruptions, and other tectonic process. SEISMIC WAVES
are instruments used to record the motion of the ground during an earthquake. SEISMOGRAPH AND SEISMOMETER
TWO TYPES OF SEISMIC WAVE BODY WAVES AND SURFACE WAVES
waves that travel through the inner layers BODY WAVES
2 TYPES OF BODY WAVES P WAVES AND S WAVES
waves that travel through on the surface of the earth SURFACE WAVES
Slippage along the fault or the plate boundary releases a tremendous amount of energy which causes vibration EARTHQUAKE
formed along convergent boundaries wherein when two plates collide VOLCANISM
formed between between the collision of continental-to continental convergence. MOUNTAIN RANGES
derived from the word ‘Tekton’ which means carpenter or builder. The word tectonic used to describe the movement of plates TECTONIC PLATES
the Lithosphere is divided into several plates that glide over the Earth's the rocky inner layer above the softcore PLATE TECTONIC THEORY
7 MAJOR PLATES PACIFIC PLATE, NORTH-AMERICAN PLATE, EURASIAN PLATE, AFRICAN PLATE, ANTARCTIC PLATE, INDIO-AUSTRALIAN PLATE, AND SOUTH-AMERICAN PLATE
8 MINOR PLATES JUAN DE FUCA, COCOSPLATE, PHILIPPINE-SEA PLATE, INDIAN PLATE, NAZCA PLATE, CARRIBEAN PLATE, ARABIAN PLATE, AND SCOTIA PLATE
Earth has been affected by sudden, short-lived, violent events, that were sometimes worldwide in scope. Due to the great flood interpreted from the bible (really happened during the bronze age) CATATROPHISM
is the assumption that the natural processes operating in the past are the same as those that can be observed operating in the present. UNIFORMITARIANISM
Theorized that the Earth is contracting because it is cooling JAMES DWIGHT DANA
Earth cooled after its formation. Heavier materials such as iron sank and formed the core, while lighter materials such as aluminum stayed up in the crust. CONTRACTION THEORY
was a German Geophysicist and meteorologist ALFRED WEGENER
Continents gradually drifted apart to where they are today CONTINENTAL DRIFT THEORY
The idea was first presented in 1596, by the man who built the first atlas known as “Theatrum Orbis Terrarum” ABRAHAM ORTELIUS
Wegener noticed the continents resemble jigsaw puzzle pieces CONTINENTAL JIGSAW PUZZLE
a single landmass disintegrated, though he ascribed the cause to the Biblical Great flood ANTONIO SNIDER-PELLEGRINI
Australian Geographer, Glossopteris could be found in 3 different continents EDWARD SUESS
when a leaf, shell, skin, or foot leaves an imprint on soft earth. IMPRESSION
a fossil that has been crushed or flattened but regains some organic material, although it has been Chemically altered COMPRESSION
which does not have specific dates, allows one to determine if it is older than another artifact or fossil RELATIVE DATING
provides more specific origin dates and time ranges, such as age range in years ABSOLUTE DATING
is the study of climatic conditions of past geological ages PALEOCLIMATOLOGY
the study of ancient magnetic field (magnetometer), Earth’s past magnetic field showed that the magnetic north pole seemingly wandered all over the globe. PALEOMAGNETISM
was a geologist and navy submarine commander during World War II, Part of his mission had been to study the deepest part of the ocean floor HARRY HAMMOND HESS
a device that bounces sound waves off underwater objects and then records the echoes of these sound waves. SONAR
The process that continually adds new material to the ocean floor while pushing rocks away from the ridge SEAFLOOR SPREADING
edges where two plates meet. PLATE BOUNDARIES
are massive, rigid slabs of rock that form the Earth’s continents. They are the thicker and less dense type of tectonic plate. CONTINENTAL PLATES
are large, rigid slabs of rock that form the ocean floor. They are thinner and denser than the other. OCEANIC PLATES
3 TYPES OF PLATE BOUNDARIES CONVERGENT, DIVERGENT, AND TRANFORM
Plates move toward each other. Whereas tectonic plates collide or come together, they contribute to the formation of mountains, volcanic activity, and earthquakes CONVERGENT
Plates move away from one another. This movement resulted in the creation of a new crust as magma rises from the mantle, it solidifies and forms a new oceanic crust DIVERGENT
; Plates slide past each other. These boundaries can cause earthquakes, as the plate grind against each other. TRANSFORM
Created by: MEOWIE
 

 



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