Not really but sea floor sediments thickness increase with increased distance from spreading centers which is good evidence. Other evidence such as magnetic reversals, temperature, dating methods provide the best evidence of seafloor spreading
Lithogenous sediment is made up of fragments of rocks and minerals that have been eroded and transported by various geological processes before settling on the ocean floor. These sediments typically originate from continental sources and can include materials such as quartz, feldspar, and clay minerals. Lithogenous sediment forms a significant component of marine sedimentary deposits.
Sediments become thicker away from the mid ocean ridge. This is because the oceanic crust away from the mid ocean ridge is older than the crust close to it, so sediment has had more time to accumulate.
Fine sediments can reach the ocean floor through various ways, such as river runoff carrying sediment from land, currents transporting sediments offshore, and particles settling from the water column. Once these fine sediments reach the ocean floor, they can accumulate over time to form sediment layers.
Lithogenous sediments come from the land They result primarily from erosion by water, wind, and ice Biogenous sediments originate from organisms The particles in these sediments come from shells and hard skeletons. Although lithogenous sediments represent the largest total volume, biogenous sediments cover a greater area of sea floor
The three types of ocean floor sediments are Terrigenous, Biogenous, and Hydrogenous sediments.
The three types of ocean floor sediments are Terrigenous, Biogenous, and Hydrogenous sediments.
Not really but sea floor sediments thickness increase with increased distance from spreading centers which is good evidence. Other evidence such as magnetic reversals, temperature, dating methods provide the best evidence of seafloor spreading
Basalt!
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Here is an example sentence with the word 'fragments':The once-beautiful photo frame slipped from her hands, and in no time it became mere shimmering fragments on the floor.
Lithogenous sediment is made up of fragments of rocks and minerals that have been eroded and transported by various geological processes before settling on the ocean floor. These sediments typically originate from continental sources and can include materials such as quartz, feldspar, and clay minerals. Lithogenous sediment forms a significant component of marine sedimentary deposits.
Origin
terrigeneous, biogeneous, and hydrogeneous
Sediments become thicker away from the mid ocean ridge. This is because the oceanic crust away from the mid ocean ridge is older than the crust close to it, so sediment has had more time to accumulate.
The sediments build up on the floor of the stream, ocean, river, or lake and causes the water to lower.
The further from the delta, the finer the sediments deposited.