Which option gives the strongest set of evidence for seafloor spreading?
Seafloor spreading is supported by several independent evidences. Exam tip: identify the set of evidences rather than one clue.
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SubjectsGeography
महासागर तल का मानचित्रण
In this Class 11 Geography topic from “Distribution of Oceans and Continents,” students learn how the ocean floor is mapped and interpreted. They explore major features such as continental shelves, slopes, deep-sea plains, mid-ocean ridges, trenches and seamounts, and understand how soundings, sonar and bathymetric maps reveal underwater relief. The topic also helps connect ocean-floor patterns with plate boundaries, seafloor spreading and the changing distribution of continents and oceans.
TOPIC PRACTICE
Up to 25 questions from this page. Select your focus, then start.
Seafloor spreading is supported by several independent evidences. Exam tip: identify the set of evidences rather than one clue.
Rope sounding gave measurements only at limited points. Exam tip: link technological improvement with data coverage.
Seafloor spreading and subduction recycle oceanic crust. Exam tip: understand oceanic crust as temporary and dynamic.
Abyssal hills are small relief features of deep ocean floors. Exam tip: do not consider abyssal plains completely featureless.
A progressively aged seamount trail can record plate movement. Exam tip: read seamount chains as clues to motion direction.
Ridges trenches and seafloor spreading clarified the mechanism of plate motion. Exam tip: connect old theory with new discoveries.
Continental slope is identified by rapid depth change. Exam tip: remember the sudden increase in gradient after shelf.
Modern mapping revealed the diversity of the ocean floor. Exam tip: study seafloor as a group of complex landforms.
Both depth and position accuracy are necessary in mapping. Exam tip: do not view measurement only vertically.
Sediment movement on slopes indicates submarine landslides. Exam tip: connect high resolution maps with geohazard detection.
Crust near ridges is young and hot so less sediment accumulates. Exam tip: draw conclusions from combined evidence.
Seafloor spreading and subduction together form a cycle of oceanic crust. Exam tip: remember both creation and destruction.
Shelf areas are important for both resources and navigation. Exam tip: remember the economic and practical role of shelves.
Narrow deep features may be missed at small scale. Exam tip: pay attention to scale and level of detail.
Magma can form in subduction zones and create volcanic arcs. Exam tip: connect trenches and volcanism causally.
Closed isobaths with a shallow centre can show a submerged mountain. Exam tip: identify highs or lows from the direction of closed lines.
Trenches and earthquakes point toward active tectonics. Exam tip: do not call a deep linear feature quiet without context.
Map presentation can change visual interpretation of data. Exam tip: read values and isobaths before colours.
Without correct location even correct depth can make a wrong map. Exam tip: understand that both position and depth are essential.
A seamount is an isolated submerged mountain below sea level. Exam tip: distinguish it from an island because its summit remains submerged.
Continental rise forms by sediment accumulation at the base of the slope. Exam tip: place it between slope and abyssal plain.
Seafloor irregularity and geohazards affect infrastructure safety. Exam tip: connect bathymetry with modern infrastructure.
Sampling connects bathymetric form with rock and age evidence. Exam tip: understand the combination of direct and indirect data.
Seafloor relief explains the background of many marine hazards. Exam tip: link mapping with risk identification.
Accurate interpretation needs integration of many evidences. Exam tip: use combined analysis rather than one clue.
QUIZ COMPLETE