yes
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
The further away a point is from the mid-ocean ridge, the deeper the sediment layer should be. Because the ocean floor is relatively new nearer the ridge, sediments have had less time to accumulate.
The further from the delta, the finer the sediments deposited.
The three types of ocean floor sediments are Terrigenous, Biogenous, and Hydrogenous sediments.
False. Sea floor sediments do not gradually thicken away from a mid-ocean ridge. Instead, the thickness of sediments can vary significantly depending on factors such as proximity to sources of sediment input, ocean currents, and tectonic activity.
The three types of ocean floor sediments are Terrigenous, Biogenous, and Hydrogenous sediments.
The recommended plywood thickness for floor installation is typically 3/4 inch.
age increases
Basalt!
Meow
Seafloor spreading is supported by the observation that sediments are thinner and younger near mid-ocean ridges, where new crust is formed, and become progressively thicker and older as one moves away from the ridge. This pattern indicates that as new oceanic crust is created at the ridge, it pushes older crust outward, allowing sediment to accumulate over time. Additionally, the age of the sediments correlates with their distance from the ridge, providing strong evidence for the continuous process of seafloor spreading.
Origin