Rebuild Past Continents - Middle School Earth and Space Science
- What is Pangaea in the context of past continental positions?
- A past supercontinent that included most landmasses. This supercontinent existed ~300-200 million years ago.
- Which seafloor feature is the long underwater mountain chain where new crust forms?
- Mid-ocean ridge. This volcanic chain marks where tectonic plates pull apart.
- Identify the strongest combined evidence set for reconstructing continents: fossils, rock belts, and what third clue?
- Continental shelf fit (geometric match of margins). Three independent data types confirm past positions.
- What is a plate in plate tectonics when reconstructing past continental positions?
- A rigid slab of lithosphere moving over the asthenosphere. Earth's outer shell divided into moving sections.
- What type of evidence uses matching rock layers and mountain belts across oceans to infer past positions?
- Geologic (rock and mountain) correlation evidence. Continuous rock formations and mountain chains split by oceans indicate past unity.
- Which seafloor age pattern best supports seafloor spreading for past plate positions?
- Youngest crust at ridges, older away from ridges. Dating confirms new crust forms at ridges and moves outward.
- What is the key magnetic property in rocks that records the direction to Earth's magnetic poles at formation?
- Remanent magnetization. Minerals align with Earth's magnetic field when rocks form.
- Which interpretation fits symmetric magnetic stripes on both sides of a ridge: seafloor spreading or erosion?
- Seafloor spreading. Symmetry proves new crust forms equally on both sides.
- What is the main reason mid-ocean ridges are key to reconstructing past plate motions?
- They create new crust and record spreading direction and rate. Spreading history preserved in magnetic stripes and age patterns.
- Which land reptile fossil is used to link South America, Africa, India, and Antarctica?
- Lystrosaurus. This land animal's fossils across four continents prove they were once connected.
- What is the key rock evidence type used to connect continents in past reconstructions?
- Matching rock layers and mountain belts. Continuous formations split by continental separation.
- Which option is the strongest match evidence: identical shoreline shapes alone, or matching rocks plus fossils?
- Matching rocks plus fossils. Multiple evidence types provide stronger proof than shape alone.
- What climate evidence indicates a continent was once near a pole?
- Glacial deposits and striations. Ice sheets leave scratches showing past polar locations.
- Which statement best describes why continent coastlines can be used to infer past positions?
- Continental shelves can fit like puzzle pieces. Underwater edges match better than coastlines for past positions.
- What seafloor pattern shows equal-age rocks arranged symmetrically on both sides of a ridge?
- Magnetic stripes (paleomagnetism symmetry). Earth's magnetic reversals create mirror-image patterns on both sides.
- Which type of evidence uses identical fossils on separated continents to infer past connections?
- Fossil correlation evidence (matching fossils across continents). Same species couldn't cross oceans, proving continents were joined.
- What is the best sequence for reconstructing past continents: fit margins, then check fossils/rocks/climate?
- Fit margins first, then verify with fossils, rocks, and paleoclimate. Physical fit provides framework; other data confirms connections.
- Which boundary type destroys ocean crust and complicates reconstructing older seafloor positions?
- Convergent boundary with subduction. Old oceanic crust recycled into mantle, erasing ancient seafloor records.
- Identify the likely past latitude if a continent contains widespread ancient glacial deposits and striations.
- High latitude, near a pole. Glaciers only form in polar regions with year-round cold.
- What seafloor feature is most directly associated with destruction of oceanic crust?
- Deep-ocean trench (subduction zone). Old oceanic crust sinks beneath other plates and melts.
- A basalt sample has reversed polarity and is far from the ridge. Which relative age is most likely?
- Older than basalt closer to the ridge. Distance from ridge indicates age; farther means older.
- What is paleomagnetism used for when reconstructing past continental positions?
- Inferring past latitude and rotation from magnetic minerals. Ancient magnetic fields recorded in rocks reveal past positions and orientations.
- Identify the best conclusion if Glossopteris fossils occur in South America, Africa, India, and Antarctica.
- Those continents were once connected. Seeds couldn't cross oceans, so fossils on multiple continents prove past connection.
- What is the term for the study of Earth's past climates using geologic evidence?
- Paleoclimatology. Reconstructs past climates from rocks, fossils, and ice cores.
- Which option best supports a past connection: A) Same climate today B) Same fossil species C) Same longitude today?
- B) Same fossil species. Identical species prove past land connection.
- What seafloor pattern of magnetic stripes is expected on both sides of a mid-ocean ridge?
- Symmetric, alternating normal and reversed polarity bands. Mirror pattern forms as seafloor spreads during reversals.
- What is paleoclimate evidence in continental reconstructions?
- Climate clues (for example, glacial deposits) preserved in rocks. Ancient climate indicators reveal past continental latitudes.
- Which seafloor age pattern supports that plates move away from a mid-ocean ridge?
- Youngest crust at the ridge, older crust farther away. Age increases with distance, proving continuous spreading.
- What is the key shoreline evidence used when fitting continents back together?
- Jigsaw fit of continental shelves (not coastlines). Continental shelves show true continent edges, not erosion-altered coasts.
- Which option is the strongest single indicator of seafloor spreading: trenches, ridges, magnetic stripes, or volcano chains?
- Magnetic stripes. Only magnetic stripes directly record spreading history.
- What does the age pattern of ocean-floor basalt show as distance from a mid-ocean ridge increases?
- Rock ages increase with distance from the ridge. New crust forms at ridge; older crust moves outward.
- Identify the best conclusion: matching Appalachian and Caledonian mountain belts indicate what?
- North America and Europe were once connected. Same mountain chain split by Atlantic Ocean formation.
- Identify the correct conclusion: tropical coal deposits in Antarctica most strongly indicate what past position?
- Antarctica was once at a lower latitude (closer to the equator). Coal forms in warm, swampy conditions near equator.
- What type of evidence uses ancient climate indicators (coal, glacial deposits) to infer past positions?
- Paleoclimate evidence. Climate-specific deposits reveal past latitudes different from current positions.
- Which data source directly records the direction of Earth's magnetic field when basalt cools?
- Magnetic minerals in igneous rocks (paleomagnetism). Iron minerals align with Earth's field when lava solidifies.
- What is the name of the supercontinent that formed when most continents were joined?
- Pangaea. This supercontinent existed about 250 million years ago before breaking apart.
- What does the term "continental drift" describe?
- The idea that continents move over Earth's surface over time. Wegener's theory explaining matching features across oceans.
- Which statement best fits seafloor data: magnetic stripes mirror across a ridge and crust ages increase outward?
- The seafloor is spreading from the mid-ocean ridge. Symmetrical patterns and age gradients confirm spreading theory.
- Choose the correct method to reconstruct past positions using multiple sources: coastline fit, fossils, rocks, and paleoclimate.
- Overlay and align continents to maximize agreement among all datasets. Best reconstructions integrate all available evidence types.
- What is paleomagnetism in rocks used to determine when reconstructing past continental positions?
- Past magnetic field direction and latitude recorded in rocks. Magnetic minerals align with Earth's field when rocks form.
- Which conclusion best fits this data: Glossopteris fossils in South America, Africa, India, and Antarctica?
- These continents were once connected. This plant couldn't cross oceans; continents must have touched.
- Which evidence most directly indicates two continents were once joined: matching fossils or matching modern climates?
- Matching fossils. Modern climates change; fossils prove ancient connections.
- What is the term for Earth's magnetic field direction preserved in rocks as they form?
- Paleomagnetism. Iron minerals align with Earth's field when rocks cool.
- What type of evidence is provided when identical fossils are found on continents now separated by oceans?
- Fossil correlation indicating the continents were once connected. Same species couldn't cross oceans, proving land connection.
- What is the definition of continental drift as used in reconstructing past continental positions?
- Continents change position over geologic time. Wegener's theory explaining matching fossils and rocks across oceans.
- What is the definition of plate tectonics relevant to past continental positions?
- Lithospheric plates move and carry continents. Modern theory explaining continental drift through plate movement.
- What does a close fit of continental shelf edges (not modern shorelines) most directly support?
- Past continental connection and later separation by plate motion. Shelf edges show true continental boundaries before separation.
- What does a widespread layer of glacial till on now-tropical continents indicate about past positions?
- Those continents were once at high latitudes near a pole. Glaciers only form in polar regions, not tropical zones.
- Which paleoclimate clue suggests a continent was once near the poles?
- Glacial striations and till deposits. Ice sheets form at poles, leaving distinctive marks.
- Which fossil is classic evidence that South America and Africa were once connected?
- Mesosaurus. This freshwater reptile couldn't cross oceans, proving land connection.
- Identify the best reconstruction clue: A) Political borders B) Coastline shape C) Continental shelf fit.
- C) Continental shelf fit. True continental edges lie at underwater shelf boundary.
- Which option best supports a past tropical location: coal deposits in present-day Antarctica?
- Antarctica was once near the equator. Coal forms from tropical swamps, impossible at current polar location.
- Which fossil is classically used to link South America and Africa in reconstructions?
- Mesosaurus. This freshwater reptile fossil links these continents.
- What does the pattern of symmetric magnetic stripes on both sides of a ridge indicate?
- Seafloor spreading with periodic magnetic reversals. Earth's magnetic field flips periodically, recorded in cooling rock.
- Identify the most likely past position: glacial striations in S. America, Africa, India, Australia, Antarctica all point outward.
- These continents were joined near the South Pole (Gondwana). Radial glacial patterns indicate ice sheet centered at South Pole.
- What is the name of the supercontinent that included most landmasses about million years ago?
- Pangaea. All continents were joined in one landmass before breaking apart.
- Identify the plate-boundary type most directly associated with seafloor spreading.
- Divergent plate boundary. Plates separate at these boundaries, creating new oceanic crust.
- What is the process called when new ocean crust forms and moves away from a ridge?
- Seafloor spreading. Magma rises at ridges, solidifies, and pushes older crust outward.
- Which feature is the most direct evidence that new oceanic crust forms at mid-ocean ridges?
- Youngest seafloor rock located at the ridge crest. Active volcanism creates new basalt at spreading centers.
- What does evidence of ancient glaciers in present-day tropical regions most strongly imply?
- The continent moved to a different latitude in the past. Glaciers form in cold climates, not tropical zones.
- Which method best uses multiple data sources to test a reconstruction: rely on one clue or require agreement among clues?
- Require agreement among multiple independent clues. Multiple data types confirm or reject hypotheses.
- What is the main reason a single data source can be misleading when reconstructing past continental positions?
- One clue can have alternative causes; multiple lines reduce error. Convergent evidence from different sources increases reliability.
- What type of evidence uses coal, reef, or desert deposits to indicate past climate zones and latitude?
- Paleoclimate (climate-indicator deposits) evidence. Coal forms in tropics, reefs in warm seas, deserts at 30° latitude.
- Which boundary type creates new ocean crust that helps track past plate movements?
- Divergent plate boundary (mid-ocean ridge). Spreading centers create oceanic crust recording plate motion history.
- What type of evidence uses glacial striations and till deposits to infer a continent's past latitude?
- Paleoclimate (glacial) evidence. Glaciers form at high latitudes, revealing past polar positions.
- Identify the best reconstruction clue: a mountain belt on one continent aligns with one across an ocean. What does it imply?
- The continents were once joined along that belt. Split mountain chains prove continents rifted apart.
- Identify the best reconstruction choice: continents that align matching mountain belts across an ocean or those that do not.
- Choose the alignment that connects matching mountain belts. Continuous mountain chains indicate past physical connection.
- Identify the best evidence that two continents collided: matching mountain belts or matching beach sand color?
- Matching mountain belts. Collision creates linear belts; sand color is superficial.
- What is the definition of continental drift as used in reconstructing past continent positions?
- The idea that continents move slowly over geologic time. Wegener's theory explains matching fossils and rocks across oceans.
- Identify the best next step: fossil and rock matches conflict with coastline fit alone. What should you prioritize?
- Prioritize fossils and rock/mountain correlations. Geological evidence is more reliable than coastline shapes.
- What is the most reliable approach when different data sources disagree about past continental positions?
- Prioritize multiple independent lines of evidence together. Combining data reduces errors from any single method.
- What is the best definition of a supercontinent in plate tectonics?
- A single landmass formed when most continents are joined. All major continents merged into one giant landmass.
- What seafloor pattern provides evidence of plate motion away from mid-ocean ridges?
- Symmetric magnetic stripes on the seafloor. Alternating magnetic polarity bands record seafloor spreading history.
- Identify the data type: Mesosaurus fossils appear in both Brazil and South Africa. What does this support?
- South America and Africa were connected when Mesosaurus lived. Freshwater reptile couldn't swim across Atlantic Ocean.
- Which statement best explains symmetric magnetic stripes on both sides of a ridge?
- Seafloor spreads outward as new basalt records polarity reversals. Each stripe forms when new crust records field direction.
- Which option best combines multiple data sources to reconstruct past positions: coastlines only, or fossils + rocks + paleoclimate?
- Fossils + rocks + paleoclimate (multiple independent lines of evidence). Multiple independent evidence types confirm past positions.
- Which modern measurement tool directly tracks present-day plate motion on Earth?
- GPS (Global Positioning System). Satellites measure precise positions, revealing plate movement rates.
- What is paleomagnetism as a data source for reconstructing past continental positions?
- Magnetic minerals record Earth's field at formation time. Iron minerals align with ancient magnetic fields when rocks form.
- What is the mountain range pair often matched to support a former Atlantic connection?
- Appalachians and Caledonians. These ranges form a continuous belt when continents are reassembled.
- Which direction did a continent likely move if its rocks show a shift from glacial deposits to desert deposits over time?
- From higher latitudes toward lower latitudes (toward the equator). Glaciers form at poles; deserts form near equator.
- Which direction did a plate move if ocean crust is at a ridge and far away on the same side?
- Away from the ridge toward the older crust. Older crust moved away as new crust formed at ridge.
- What is the relationship between seafloor age and distance from a mid-ocean ridge?
- Older seafloor is farther from the ridge. New crust forms at ridge, moves away over time.
- Which evidence type is shown by identical fossils found on now-separated continents?
- Fossil correlation evidence. Same species couldn't cross oceans, proving past connections.
- What does coal found in Antarctica indicate about Antarctica's past climate and location?
- It was once warmer and closer to the equator. Coal forms from tropical swamps, impossible in polar regions.
- Which option best supports a past polar location: widespread glacial striations in present-day India?
- India was once at high (polar) latitude. Glacial marks form only in cold climates near poles.
- Which data source best constrains past climate zone: glacial deposits or magnetic stripes on the seafloor?
- Glacial deposits. Till and striations directly indicate polar conditions.
- What is the most reasonable inference if tropical reef fossils are found in rock now located near a pole?
- The landmass was once nearer the equator. Reefs only form in warm tropical waters, not polar regions.
- What type of evidence uses the jigsaw-like match of continental margins to infer past positions?
- Continental fit (shape) evidence. Coastlines fit together like puzzle pieces when continents are reassembled.
- Identify the best inference if seafloor magnetic stripes are symmetric on both sides of a ridge.
- Seafloor spreading occurred from that ridge. Symmetric patterns prove new crust forms equally on both sides.
- Which reconstruction is more reliable: one based only on coastline fit or one using fossils, rocks, and climate together?
- The reconstruction using fossils, rocks, and climate together. Multiple evidence types provide stronger support than shape alone.
- Which seafloor feature is the main source of new oceanic crust?
- Mid-ocean ridge. Underwater mountain chain where new seafloor forms continuously.
- Which paleoclimate clue suggests a continent was once near the equator?
- Coal deposits from ancient tropical swamps. Swamps thrive in warm, wet equatorial climates.
- Which ocean-floor age pattern best supports seafloor spreading at a mid-ocean ridge?
- Youngest crust at the ridge, older crust farther away. New crust forms at ridge center, aging as it spreads outward.
- What type of evidence uses identical fossils on separated continents to infer past connections?
- Fossil correlation evidence. Same species couldn't cross oceans, proving land connection.
- Which fossil plant is classically used to link southern continents for past positions?
- Glossopteris. Seed fern found across all southern Gondwana continents.
- Which seafloor pattern provides strong evidence for plate motion used in reconstructions?
- Symmetric magnetic striping on both sides of ridges. Alternating polarity bands prove seafloor spreading from ridges.
- Which seed fern fossil is widely found across southern continents, supporting Gondwana connections?
- Glossopteris. This plant's seeds couldn't cross oceans, proving southern continents were joined.
- What is the key fossil evidence type used to match continents across oceans?
- Same land organism fossils on separated continents. Organisms couldn't cross oceans, proving past land connections.
- What is seafloor spreading as evidence for changing continental positions?
- New ocean crust forms at mid-ocean ridges and moves outward. This process pushes continents apart over time.
- What feature marks where new oceanic crust forms and plates move apart?
- Mid-ocean ridge (divergent boundary). New crust forms here as plates separate, pushing continents apart.
- Which supercontinent name refers to most landmasses joined about million years ago?
- Pangaea. Greek for "all Earth," existed during Permian-Triassic periods.
- Which data source provides symmetric magnetic stripe patterns used to infer seafloor spreading?
- Magnetic anomalies on the ocean floor. Alternating magnetic stripes record Earth's field reversals during spreading.
- Which option best indicates two continents were once adjacent: same-aged basalt flows or same modern rainfall totals?
- Same-aged basalt flows. Matching rock ages indicate formation when continents were joined.
- Identify the best reconstruction clue: identical trilobite fossils on two distant continents. What does it imply?
- The continents were once connected or much closer. Species couldn't evolve identically on separate continents.
- Which type of evidence uses ancient climate clues like coal beds and desert deposits?
- Paleoclimate indicators. Ancient climate features reveal past continental positions and latitudes.
- Identify the better coastline match for South America when reconstructing Pangaea: Africa or Australia?
- Africa. Their shelves fit like puzzle pieces from Pangaea breakup.
- Which data combination is strongest for reconstructing past continental positions: fossils, rocks, paleoclimate, or only coastlines?
- Multiple independent lines of evidence together. Single evidence types can be misleading; multiple sources confirm positions.
- Which conclusion best fits symmetric magnetic stripes on both sides of a mid-ocean ridge?
- New crust forms at the ridge and moves outward. Matching patterns prove seafloor spreads equally in both directions.
- What is the best-fit criterion that uses matching continental shelf edges to reconstruct past continents?
- Continental margin (shelf) fit. Continental shelves show true edge before rifting occurred.
- Which option best supports that a continent was once near the South Pole: coral reefs or glacial striations?
- Glacial striations. Glacial marks form only in polar regions with ice sheets.
- Identify the best interpretation: oceanic crust is youngest at ridges and older away from ridges.
- Seafloor spreading is occurring at ridges. Age pattern proves new crust continuously forms at ridges.
- What is the term for the study of Earth's past geographic positions and environments using rocks and fossils?
- Paleogeography. Reconstructs ancient geography from geological and fossil evidence.
- What is indicated when matching rock layers and mountain belts occur on opposite sides of an ocean?
- The landmasses were once joined and shared a geologic history. Continuous geology across oceans proves former connection.
- Which data source best constrains past latitude of a continent: paleomagnetism or coastline fit?
- Paleomagnetism. Magnetic inclination varies predictably with latitude.
- Which type of evidence compares rock type, age, and mountain belts across oceans?
- Rock and mountain belt correlation. Matching geology across oceans shows continents were once joined.
- What is the name of the supercontinent that included most landmasses about 300 million years ago?
- Pangaea. All continents joined before Atlantic Ocean opened.
- What magnetic pattern on the seafloor provides evidence for seafloor spreading?
- Symmetric magnetic stripes (reversal pattern). Mirror-image patterns form as field flips during spreading.
- Which evidence type uses ancient climate indicators (coal, glacial deposits) to infer past latitudes?
- Paleoclimate evidence. Climate indicators reveal past latitudes different from today.
- Identify the best conclusion if Mesosaurus fossils are found in both Brazil and western Africa.
- South America and Africa were once connected. This freshwater reptile couldn't cross the Atlantic Ocean.
- Which seafloor location is youngest: at a mid-ocean ridge or near a deep-ocean trench?
- At a mid-ocean ridge. New crust forms at ridges; old crust subducts at trenches.
- Which type of evidence uses matching fossil species on now-separated continents?
- Fossil correlation. Same species on different continents suggest they were once connected.
- Identify the best conclusion if matching mountain belts and rock ages occur in eastern North America and western Europe.
- North America and Europe were once joined. Continuous mountain chains now separated by ocean indicate past connection.
- Which paleoclimate evidence indicates a region was once near the equator and humid?
- Coal deposits. Coal forms in warm, swampy conditions typical of equatorial regions.
- Which option best indicates two continents were once connected: matching coastline shapes or matching fossils and rocks?
- Matching fossils and rocks. Coastlines change over time; geological evidence is more reliable.
- What seafloor feature is the main location where new ocean crust forms?
- Mid-ocean ridge. Divergent boundaries where plates separate and create crust.
- Which option best supports that a continent moved toward the equator: more glacial till or more coal deposits?
- More coal deposits. Coal forms in warm, swampy conditions near the equator.
- Identify the best interpretation: magnetic stripes are parallel to a mid-ocean ridge and mirror each side.
- New crust forms at the ridge and spreads outward. Symmetrical patterns prove continuous spreading from center.
- Which evidence type matches rock layers and mountain belts across oceans to reconstruct past positions?
- Geologic correlation (matching rocks and mountain ranges). Continuous formations split by oceans prove past connections.
- Which fossil is classically used to connect South America and Africa in continental drift evidence?
- Mesosaurus. This freshwater reptile couldn't swim oceans, proving land connection.
- What is the name of the supercontinent that included most modern continents about million years ago?
- Pangaea. All continents formed one landmass before breaking apart.
- What is the name of the supercontinent that formed about million years ago?
- Pangaea. All continents joined before breaking apart into today's configuration.
- Which evidence type is strongest for reconstructing past continent positions: fossils, rocks, climate, or coastline shape?
- Multiple independent lines of evidence combined. Single evidence types can be misleading; multiple types confirm reconstructions.
- Which conclusion is best if two continents share the same land fossil species and matching rock layers?
- They were once connected or much closer together. Shared fossils and geology prove past continental unity.
- What type of evidence uses matching rock layers and mountain belts across oceans to reconstruct past positions?
- Geologic (rock and mountain) correlation evidence. Continuous formations split by seafloor spreading show past unity.
- What climate evidence indicates a continent was once near the equator?
- Coal deposits from warm, wet swamp environments. Coal forms in tropical swamps, indicating past equatorial position.
- Identify the best reconstruction clue: coastlines fit, but fossils and rocks do not match. Which evidence should dominate?
- Fossil and rock correlation evidence. Coastline shapes alone can be misleading without other evidence.
- What is the best overall term for evidence types used to rebuild past continental positions?
- Multiple data sources (fossils, rocks, paleoclimate, seafloor, GPS). Scientists combine different evidence types to reconstruct ancient geography.
- What type of evidence uses identical fossils on separated continents to infer past positions?
- Fossil correlation evidence. Same species couldn't cross oceans, so presence on multiple continents shows past connection.
- Which interpretation is most valid: matching Appalachian and Caledonian mountains indicate what past condition?
- North America and Europe were once connected. Mountain chains were continuous before Atlantic opened.
- Which seafloor observation best supports seafloor spreading at mid-ocean ridges?
- Youngest ocean crust is at the ridge; older crust is farther away. Age increases with distance from ridge, proving continuous crust formation.
- Which paleoclimate evidence indicates a region was once dry, like a desert belt?
- Evaporite deposits (salt, gypsum). These minerals form when seawater evaporates in hot, arid climates.
- Identify the best match: Mesosaurus fossils on South America and Africa imply what past relationship?
- South America and Africa were once joined. Freshwater reptile fossils on both continents prove direct connection.
- Identify the best data source to determine a continent's past latitude: fossils, paleomagnetism, or coastlines.
- Paleomagnetism. Magnetic inclination varies with latitude when rocks formed.
- Which plant fossil found across several southern continents supports past connection?
- Glossopteris. This seed fern spread across Gondwana before continents separated.
- Which supercontinent is commonly reconstructed from fossil, rock, and fit evidence in middle school geology?
- Pangaea. The supercontinent that existed 250 million years ago.
- Which conclusion is supported if the same land reptile fossil is found in South America and Africa?
- South America and Africa were once connected. Land animals couldn't swim across ocean barriers.
- What type of evidence is indicated by matching rock layers and mountain belts across oceans?
- Rock and mountain correlation evidence. Continuous geological features prove past continental connections.
- Find the best fit rule: should you match modern coastlines or continental shelves when rebuilding past continents?
- Match continental shelves. Shelves show true continent edges before erosion changed coastlines.
- Which paleoclimate feature on bedrock indicates glaciers once covered the area?
- Glacial striations (scratches) and till. Glaciers carve distinctive marks as they move over bedrock.
- What pattern of magnetic stripes on the seafloor supports seafloor spreading?
- Symmetrical magnetic reversals on both sides of a ridge. Mirror patterns prove crust forms at ridge and spreads equally.
- Which conclusion best fits this data: identical-aged basalt and symmetric magnetic stripes across an ocean ridge?
- New crust formed at the ridge and spread outward. Symmetry and age patterns prove seafloor spreading from the ridge.