The oldest oceanic crust is generally found at the largest distance from the spreading centre where it was generated. the best place to go at the moment would be the Pacific Ocean south east of Japan, where there is Jurassic ocean crust preserved. Oceanic crust of the same age can be found East of the United States of America and west of Africa as well but there one finds much less because of slower spreading rates.
These rocks are usually buried by hundreds of meters of sediments and are thus mostly not directly accessible. Very old rocks can be found on the ocean floor, when icebergs carry gravel and stones derived from old continental crust (like large parts of Skandinavia) onto the ocean and drop them as they melt (drop stones).
If one was measuring the temperatures of rocks on the seafloor, the hottest rocks would be located nearest to a mid ocean ridge. This is the location where the hot magma from the asthenosphere rises and is situated on either side of the ridge. The farther away the seafloor is from the central area of heat, the colder it is. This pattern is identical on both sides of a mid ocean ridge. However, if rocks are located near subduction zones or hot spots, they too would be hotter than the majority of the seafloor.
Near volcano and earthquake areas on the ocean floor, you would expect to find features like mid-ocean ridges, deep-sea trenches, seamounts, and hydrothermal vents. These features are associated with tectonic plate boundaries and geological activity, such as volcanic eruptions and seismic events, that occur in these areas.
They are formed over millions of years of sand being packed down by the ocean.....And you can find them where oceans are located or were located like hoodoos and coulies.
You would find extrusive igneous rocks. Beyond that it depends on the volcano.
Yes, you can find fossils in sedimentary rocks.
sand,rocks
The ocean floor is mainly basalt. Closer to the poles you would occassionally find a glacial erratic, dropped from a melting iceberg.
The youngest rocks on the ocean floor are typically found along mid-ocean ridges. These areas are where new oceanic crust is formed through volcanic activity and the process of seafloor spreading. As the magma cools and solidifies, it creates new rocks that are relatively young compared to rocks found in other parts of the ocean floor.
The oldest rock on the ocean floor can be found in the central parts of the ocean basins, particularly in regions known as abyssal plains. These rocks are generally around 200 million years old or older.
Somewhere at the bottom of the Marianas Trench you would find the oldest rock of the oceanic crust. Somewhere else, however, there are older rocks on the ocean floor--those deposited by icebergs that have broken off of glaciers. Those erratic rocks could be much older than the oldest oceanic crust.
Somewhere at the bottom of the Marianas Trench you would find the oldest rock of the oceanic crust. Somewhere else, however, there are older rocks on the ocean floor--those deposited by icebergs that have broken off of glaciers. Those erratic rocks could be much older than the oldest oceanic crust.
Somewhere at the bottom of the Marianas Trench you would find the oldest rock of the oceanic crust. Somewhere else, however, there are older rocks on the ocean floor--those deposited by icebergs that have broken off of glaciers. Those erratic rocks could be much older than the oldest oceanic crust.
in the deep oceon floor
pacific ocean st pats rocks
If one was measuring the temperatures of rocks on the seafloor, the hottest rocks would be located nearest to a mid ocean ridge. This is the location where the hot magma from the asthenosphere rises and is situated on either side of the ridge. The farther away the seafloor is from the central area of heat, the colder it is. This pattern is identical on both sides of a mid ocean ridge. However, if rocks are located near subduction zones or hot spots, they too would be hotter than the majority of the seafloor.
At the Mid-ocean ridge, because those rocks will have just been produced by the diverging boundary.
Abyssal hills are small hills that rise from the abyssal plain, which is the floor of the ocean.