ocean mapping is made possible through indirect methods. Oceanographers use echo sounding, sonar, radar, and seismographic surveys. Vibrations such as sounds are set down from the ocean surface. The vibrations are then reflected from the ocean bottom at the same angle that they are received and are recorded at the surface. To calculate the distance to the bottom, the following equation is used
d= 1/2 t x v
These photographic technologies made possible the complete mapping of the ice sheet that covers 98% of the continent. Mapping the physical attributes of the continent uses other technologies, including geo-mapping technologies.
Sonar mapping is needed for ocean research patterns.
like mountain
the echolaocation for measurnig the bottom of the ocean is the Doppler effect
I think that Henry Hess invented echo-sounding devices for mapping the ocean floor. But I am not 100% sure that is the correct answer. LOL <3
Developments in sonar, both depth-profiling and side-scan, and in sea-bed mapping generally for the overall topography, and in remotely-controlled submersibles for studying details. The adjective "underwater" isn't needed, BTW! :-)
SONAR, which was developed by the military to detect submarines.
Bathyscapes and submersibles have.
no
Yes, it is possible that there are deeper parts of the ocean that have not yet been discovered. Scientists continue to explore and map the ocean floor, and new discoveries are still being made.
The invention of the Portuguese ship, the caravel, made travel across the open tropical ocean and against the wind possible in 1492.
advances in sailing and shipbuilding techniques(study Island)