In ocean-floor mapping, the use of sound waves to measure depth is based on which principle?
The sound wave returns after striking the sea floor and depth is calculated from time. Exam tip: remember the relation between time and velocity.
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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.
The sound wave returns after striking the sea floor and depth is calculated from time. Exam tip: remember the relation between time and velocity.
Bathymetry measures the topography of the sea floor. Exam tip: connect it with underwater relief.
Echo sounding allowed a moving ship to record depth. Exam tip: link technology with faster mapping.
A continental shelf is the submerged edge of a continent. It remains relatively shallow because it is a continuation of the land surface beneath the sea. On an ocean-floor map, it appears beside the coastline as a broad zone with a gentle gradient, before the seabed drops more sharply toward the continental slope.
Therefore, option A is correct: a shallow, gently sloping part near the coast identifies the shelf. A deep narrow trench is a different feature associated with very great depth, while a mid-ocean volcanic peak and a steep rise in an abyssal plain do not mark the continental margin. The indicator is both its coastal position and its low relief.
The slope is a steep descent linking shallow and deep parts. Exam tip: remember it as a boundary zone.
Trenches are long narrow and extremely deep. Exam tip: also link them with convergent plate boundaries.
Mid-oceanic ridges are linked with formation of new oceanic crust. Exam tip: connect ridges with spreading centres.
Symmetrical magnetic stripes show crust formation on both sides of ridges. Exam tip: remember magnetic stripes as evidence of spreading.
The direct answer is A, Isobath. An isobath is a line joining places having the same depth below sea level. Ocean-floor maps use depth measurements, just as land maps use height measurements. The idea is simple: if several points are 2,000 metres deep, one line may join them; that line is an isobath. Option A is correct because “iso” means equal and “bath” relates to depth. Option B, Isohyet, joins places receiving equal rainfall, not equal depth. Option C, Isobar, joins places having equal atmospheric pressure. Option D, Isotherm, joins places having equal temperature. Thus, depth means isobath. Remember: bath sounds like bathymetry, the measurement of underwater depth.
Raised sea-floor features cause small gravity and surface-height variations. Exam tip: treat it as an indirect mapping method.
A seamount is pointed while a guyot has a flat top. Exam tip: link guyot with a truncated volcanic summit.
Abyssal plains are among the flattest large areas on Earth. Exam tip: connect them with sediment deposition.
Submarine canyons can help carry sediments from coast to deep areas. Exam tip: link them with slope and sediment flow.
The sea floor is hidden so depth-based maps are needed. Exam tip: remember the difference between navigation and bathymetry.
Crust becomes older away from the ridge and gets more time for sediment deposition. Exam tip: understand distance-age relation.
Multibeam sonar gives high detail over a broad swath. Exam tip: connect it with modern detailed mapping.
New crust forms at ridges and crust may sink at trenches. Exam tip: understand both as parts of the plate cycle.
Symmetrical age pattern is strong evidence of sea-floor spreading. Exam tip: study age and magnetic stripes together.
Due to depth the real relief remained hidden for long. Exam tip: connect technological development with change in knowledge.
Transform faults cut ridge segments and show horizontal movement. Exam tip: connect them with direction of plate motion.
Earthquakes and volcanoes are often linked with active boundaries. Exam tip: study structures and hazard zones together.
Colours make shallow and deep parts easy to distinguish. Exam tip: pay attention to the visual language of maps.
Single-beam gives depth only along a narrow line. Exam tip: remember the relation between sampling distance and map detail.
Mapping proved the sea floor to be an active geological region. Exam tip: connect different evidences in answers.
Oceanic trenches are the deepest linear features. Exam tip: identify them immediately from the word trench.
QUIZ COMPLETE