What forms at each kind of plate boundary
Grade 9 Science Worksheet - Challenge Me
Circle the best answer.
Read this first
Card (USGS)
The vast majority of volcanoes occur near plate boundaries. Hawaii formed more than 3,200 km from the nearest boundary, over a hotspot.
A student tells Esme that every volcano sits on a plate boundary. Which reply fits the card?
- Not supported; Hawaii is more than 3,200 km from a boundary, and a hotspot feeds its volcanoes
- Supported; Hawaii is a divergent boundary in the middle of the Pacific, so the claim holds
- Supported; hotspots count as plate boundaries, so Hawaii sits on one in the Pacific plate
- Not supported; most volcanoes are far from boundaries, and Hawaii is a typical example of that
India and Asia are continental plates. When two continents meet, neither subducts, and the light crust buckles upward. A student tells Jun that the Himalayas formed when India's oceanic plate sank beneath Asia. Which reply fits the card?
- Not supported; both plates are continental, so neither sinks and the crust buckles upward
- Supported; the oceanic plate sinks and builds the range with volcanoes above it, as at a trench arc
- Not supported; the plates part, and the range is a rift valley formed between two continents
- Supported; India is an oceanic plate, so it sinks and the Himalayas are a chain of volcanoes
Card (example data)
Plate N lies north of the boundary and moves 3 cm a year east and 2 cm a year north. Plate S lies south of it and moves 3 cm a year west and does not move north or south.
A boundary runs east to west. Which description fits the motion, by Luz's reading?
- Mostly sliding past at 6 cm a year, with some opening at 2 cm a year
- Opening at 6 cm a year, with some sliding at 2 cm a year
- Mostly closing at 2 cm a year, with some sliding at 6 cm a year
- Sliding past at 3 cm a year, with some opening at 2 cm a year
Card (example data)
The slab moves 7 cm a year along its dip. Depth rate = speed × sin(dip). sin 60° is about 0.87.
A slab dips 60° and sinks along its dip at 7 cm a year. About how long to reach 600 km depth, by Milo's math? (1 km = 100,000 cm.)
- About 10 million years
- About 8.6 million years
- About 100 million years
- About 1 million years
Four boundary sites (example data)
Site Quake depths Volcanoes Crust ages Site W to 20 km none youngest at the center Site X to 600 km a curved chain oldest next to a deep trench Site Y to 20 km none ridge offset sideways Site Z to 100 km none continental crust on both sides Which site is a continent–continent collision, and what separates it from Site X, by Noah's reading?
- Site Z: quakes stop near 100 km and there is no volcanic chain, unlike Site X
- Site Y: quakes stop near 20 km and its ridge is offset sideways, unlike Site X
- Site X: quakes reach 600 km and it has a curved chain of volcanoes
- Site W: quakes stop near 20 km and its crust is youngest at the center, unlike Site X
Three groups of volcanoes (example data)
Group Distance from nearest boundary Quake depths below Group A 60 km to 300 km Group B 3,200 km to 20 km Group C 80 km to 20 km Which group is best explained by a hotspot, and why, by Pia's reading?
- Group C: it lies near a boundary, which is where hotspots form, with shallow quakes below
- Group B: it lies 3,200 km from a boundary, with only shallow quakes below it
- Group A: its deep quakes below it show a hot region under the plate, so a plume is likely
- Group A: it lies close to a boundary and has deep quakes below it, so a plume is likely
Quakes 200 km inland of four trenches (example data)
Zone Depth of quakes Zone 1 168 km Zone 2 200 km Zone 3 280 km Zone 4 346 km Which conclusion does the table support, by Ren's reading? (Dip = angle whose tangent is depth ÷ 200 km.)
- Zone 4 has the shallowest dip, since its quakes are the deepest
- The four zones share one dip of 45°, since depth rises with distance in each
- Dip falls from 60° to 40° from Zone 1 to Zone 4, as depth rises
- Slab dip varies from about 40° to 60°, so no single dip fits every zone
Card (USGS)
Divergent boundaries make ridges and rifts. Convergent boundaries make trenches, volcanic arcs and mountains. Transform boundaries slide plates past. Hotspots lie inside plates.
Which summary links boundaries to features, by Zee's reading?
- Divergent: ridges and rifts. Convergent: trenches, arcs, mountains. Transform: sliding. Hotspots: volcanoes inside plates
- Divergent: trenches and arcs. Convergent: ridges and rifts. Transform: sliding. Hotspots: volcanoes inside plates
- Divergent: ridges and rifts. Convergent: sliding. Transform: trenches and arcs. Hotspots: volcanoes on boundaries
- Divergent: ridges and rifts. Convergent: trenches, arcs, mountains. Transform: new crust. Hotspots: volcanoes on boundaries
The Marianas are ocean–ocean convergence. The Andes are ocean–continent convergence. The Himalayas are continent–continent convergence. Which summary pairs each place with its plates and features, by Ari's reading?
- Marianas: trench and island arc. Andes: mountains with no trench. Himalayas: trench and volcanic range
- Marianas: trench and island arc. Andes: trench and volcanic range. Himalayas: a rift valley
- Marianas: trench and island arc. Andes: trench and volcanic range. Himalayas: mountains with no trench
- Marianas: mountains with no trench. Andes: trench and island arc. Himalayas: trench and volcanic range
Card (USGS)
At subduction zones, earthquakes lie in a zone sloping 40 to 60° down under the overriding plate and reaching several hundred km.
Which summary of earthquakes at subduction zones fits the cards, by Bo's reading?
- Quakes deepen inland along a slab dipping 40 to 60°, reaching several hundred km
- Quakes deepen inland along a slab dipping 4 to 6°, reaching several hundred km
- Quakes deepen toward the sea along a slab dipping 40 to 60°, reaching several hundred km
- Quakes stay shallow along a slab dipping 40 to 60°, reaching just a few km