Wizard Test Maker
... presence of fossils of the same species of organisms on continents that are separated by an ocean indicates A) this species was capable of swimming long distances. B) the continents must have been connected at some time in the past. C) a species can evolve separately on two different continents. D) ...
... presence of fossils of the same species of organisms on continents that are separated by an ocean indicates A) this species was capable of swimming long distances. B) the continents must have been connected at some time in the past. C) a species can evolve separately on two different continents. D) ...
PRE-POSTTESTwithANSWERS
... 5. The collision of two oceanic plates forms: a. a mountain; b. convection current; c. trench; d. volcano 6. The Earth’s crust is: a. thin; b. hard and brittle; c. broken into puzzle-like pieces; d. all of these 7. Plate Tectonics is: a. a popular theory; b. a known scientific law; c. a faulty hypot ...
... 5. The collision of two oceanic plates forms: a. a mountain; b. convection current; c. trench; d. volcano 6. The Earth’s crust is: a. thin; b. hard and brittle; c. broken into puzzle-like pieces; d. all of these 7. Plate Tectonics is: a. a popular theory; b. a known scientific law; c. a faulty hypot ...
process of forming new oceanic crust from magma rising to the
... Which process adds new crust to the surface? ______Sea Floor ...
... Which process adds new crust to the surface? ______Sea Floor ...
Chapter 9 WS #1
... PART A: TECTONIC FEATURES 1. Draw in the asthenosphere, lithosphere and an accretionary prism. 2. Color the diagram below using the figures on pages 192-194 as a guidelines. 3. Add missing labels as necessary. You should be able to identify and describe all of the following tectonic features. ...
... PART A: TECTONIC FEATURES 1. Draw in the asthenosphere, lithosphere and an accretionary prism. 2. Color the diagram below using the figures on pages 192-194 as a guidelines. 3. Add missing labels as necessary. You should be able to identify and describe all of the following tectonic features. ...
Chapter 8 Plate Tectonics
... • Location of Earthquakes and Volcanoes…. • Located along plate boundaries • Ring of Fire….ring of volcanoes & earthquakes around the Pacific Ocean ...
... • Location of Earthquakes and Volcanoes…. • Located along plate boundaries • Ring of Fire….ring of volcanoes & earthquakes around the Pacific Ocean ...
Subduction Zones
... or arc basement rocks covered by a thin veneer of sediments or both. • Where there is little sediment accumulation on the subducting plate, island arc or continental basement may extend all the way to the lower trench slope and little or no accretionary prism may occur. • Forearc basement may draped ...
... or arc basement rocks covered by a thin veneer of sediments or both. • Where there is little sediment accumulation on the subducting plate, island arc or continental basement may extend all the way to the lower trench slope and little or no accretionary prism may occur. • Forearc basement may draped ...
1 Lecture 24: Convergent boundaries November 22, 2006
... c. Cold slab drags the asthenosphere along with it setting up convection under the arc—promotes back-arc spreading. Seismicity 1. get shallow, extensional earthquakes near the trench where the slab bends into the subduction zone, 2. compressional faulting is associated with movement under the accret ...
... c. Cold slab drags the asthenosphere along with it setting up convection under the arc—promotes back-arc spreading. Seismicity 1. get shallow, extensional earthquakes near the trench where the slab bends into the subduction zone, 2. compressional faulting is associated with movement under the accret ...
Earthquake BINGO
... Select 12 words/phrases from this section to place in 12 different boxes. Colliding Ring of Fire Plate Boundary Divergent Rupture (crack) at surface People hurt Streams/rivers diverted Modified Mercalli Intensity Scale Richter Scale Mountain ridges line up Shapes of continents match Mid Atlantic Rid ...
... Select 12 words/phrases from this section to place in 12 different boxes. Colliding Ring of Fire Plate Boundary Divergent Rupture (crack) at surface People hurt Streams/rivers diverted Modified Mercalli Intensity Scale Richter Scale Mountain ridges line up Shapes of continents match Mid Atlantic Rid ...
9.2 – Sea Floor Spreading
... (80 km) per day. (average of 25 miles per year) •In the last 150 years, the pole has wandered a total of about 685 miles •The last time the poles switched was 780,000 years ago, and it's happened about 400 times in 330 million years ...
... (80 km) per day. (average of 25 miles per year) •In the last 150 years, the pole has wandered a total of about 685 miles •The last time the poles switched was 780,000 years ago, and it's happened about 400 times in 330 million years ...
Plate Boundaries Diagram Type of boundary and motion at
... Type of boundary and motion at boundary ...
... Type of boundary and motion at boundary ...
1.3 Japan and South-East Asia
... Describe the location of Indonesia and the Philippines in relation to plate boundaries. Now describe the spatial association between the location of these boundaries and the distribution of volcanoes. Is this a strong relationship? Explain. ...
... Describe the location of Indonesia and the Philippines in relation to plate boundaries. Now describe the spatial association between the location of these boundaries and the distribution of volcanoes. Is this a strong relationship? Explain. ...
Chapter 17 Study Guide Answers
... • 4. Climate clues (glaciers) • 5. Rock clues (similar mountains) ...
... • 4. Climate clues (glaciers) • 5. Rock clues (similar mountains) ...
Chapter 1—Plate Tectonics and California
... sketch, label the following: oceanic trench, volcanic arc, where magma is forming, a batholith and the accretionary wedge. Describe what each one is. Use several “X’s” to show where earthquakes would occur. Use arrows to show how the plates are moving with respect to one another. 5. Draw a sketch of ...
... sketch, label the following: oceanic trench, volcanic arc, where magma is forming, a batholith and the accretionary wedge. Describe what each one is. Use several “X’s” to show where earthquakes would occur. Use arrows to show how the plates are moving with respect to one another. 5. Draw a sketch of ...
Chapter Questions
... volcanic settings like seafloor spreading centers and ocean hotspots. Example: Basalt. FELSIC – igneous rocks whose composition is high in Si and low in Fe, Mg, and Ca – usually found in continental volcanic settings like subduction zone volcanic arcs, continental hotpots, or continental rifting. Ex ...
... volcanic settings like seafloor spreading centers and ocean hotspots. Example: Basalt. FELSIC – igneous rocks whose composition is high in Si and low in Fe, Mg, and Ca – usually found in continental volcanic settings like subduction zone volcanic arcs, continental hotpots, or continental rifting. Ex ...
Plate Tectonics Review Worksheet
... Plate Tectonics Worksheet (Some answers may have to be researched) 1. Define Continental Drift: ...
... Plate Tectonics Worksheet (Some answers may have to be researched) 1. Define Continental Drift: ...
Lecture 6 Review Sheet
... boundary, mid-ocean ridge, continental rift, rift valley, rift volcano, rift range or rift mountain, island arc, subduction, magma, volcano, collision zone, orogenic belt, volcanic arc, accretionary wedge, forearc basin, terrigenous/terrestrial sediment, subduction trench, magmatic arc, mountain cha ...
... boundary, mid-ocean ridge, continental rift, rift valley, rift volcano, rift range or rift mountain, island arc, subduction, magma, volcano, collision zone, orogenic belt, volcanic arc, accretionary wedge, forearc basin, terrigenous/terrestrial sediment, subduction trench, magmatic arc, mountain cha ...
Tectonic Landforms
... convergence of two plates. • Either at collision (Himalayas) or destructive (Andes) margins. • Anomaly = The Urals Outcome of crustal crumpling due to compressional forces exerted at the plate ...
... convergence of two plates. • Either at collision (Himalayas) or destructive (Andes) margins. • Anomaly = The Urals Outcome of crustal crumpling due to compressional forces exerted at the plate ...
Type of Boundary - Ms Dudek`s Website
... TECTONIC PLATE BOUNDARIES (remember that oceanic crust is denser than continental crust) ...
... TECTONIC PLATE BOUNDARIES (remember that oceanic crust is denser than continental crust) ...
Converging Plate Boundaries
... lithospheric slabs, thereby producing an inclined zone of earthquakes that dips into the Earth’s upper mantle typically at angles of 40°– 60° from the horizontal. Earthquakes can occur at any depth within the sinking slab, from shallow (0 - 60 km) to as great as 700 km. Over three-quarters of the wo ...
... lithospheric slabs, thereby producing an inclined zone of earthquakes that dips into the Earth’s upper mantle typically at angles of 40°– 60° from the horizontal. Earthquakes can occur at any depth within the sinking slab, from shallow (0 - 60 km) to as great as 700 km. Over three-quarters of the wo ...
Convergent Boundaries: Here crust is destroyed and recycled back
... as a whole sinks smoothly and continuously into the subduction trench. ...
... as a whole sinks smoothly and continuously into the subduction trench. ...
Aim: How do the different types of plate boundaries differ?
... Put your name, period and date on it.. The students who gets this question correct will ...
... Put your name, period and date on it.. The students who gets this question correct will ...
Oceanic trench
The oceanic trenches are hemispheric-scale long but narrow topographic depressions of the sea floor. They are also the deepest parts of the ocean floor. Oceanic trenches are a distinctive morphological feature of convergent plate boundaries, along which lithospheric plates move towards each other at rates that vary from a few mm to over ten cm per year. A trench marks the position at which the flexed, subducting slab begins to descend beneath another lithospheric slab. Trenches are generally parallel to a volcanic island arc, and about 200 km (120 mi) from a volcanic arc. Oceanic trenches typically extend 3 to 4 km (1.9 to 2.5 mi) below the level of the surrounding oceanic floor. The greatest ocean depth to be sounded is in the Challenger Deep of the Mariana Trench, at a depth of 11,034 m (36,201 ft) below sea level. Oceanic lithosphere moves into trenches at a global rate of about 3 km2/yr.