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Age of seafloor rock and sediment increases with distance from the oceanic ridges.
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Each band of color on the seafloor represents a different depth range or elevation. These color bands are used in bathymetric maps to visually depict the various underwater topographic features and gradients in depth.
they use sensors to measure the shallow depths of the ocean and can detect variations in sea surface height caused by the gravitational pull of the seafloor's features. This data is then used to create maps of the seafloor topography and to study ocean currents, tides, and marine habitats.
The age of rocks gets progressively younger as you move away from the mid-ocean ridges, where seafloor spreading occurs. This supports the theory of seafloor spreading, as new crust is being formed at the ridges and then moves away from them over time. This process leaves a record of older rocks further from the ridges and younger rocks closer to them.
Bathymetric maps are used to map seafloor topography. These maps are created using specialized sonar equipment to measure the depth of the ocean floor. The data collected is then used to generate detailed images and models of the underwater terrain.
Wave base is typically measured as the depth at which wave action is felt on the seafloor. This is commonly determined by the distance between the wave crest and the seafloor. One method is to analyze sediment samples to identify the depth at which there is a transition from well-sorted to poorly-sorted sediments, indicating the influence of wave energy.
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A fathometer measures the depth of water by using sound waves to calculate the distance between the sensor and the seafloor. It is commonly used on boats and ships for navigation and safety purposes.
The depth of the sea can be determined by measuring the time taken for sound waves to travel from a source to the seafloor and back to a receiver. By knowing the speed of sound in water, scientists can calculate the distance to the seafloor based on the time taken for the sound waves to return. This method is known as echo sounding or sonar.