These Samples are reviewed for consistency and deposits: the "age" of samples are determined as closely as practical , by the Carbon Dating of the tiny shells normally found inside most sediment samples.
While it is True that the Average Research will only Sample and "date" to a particular point in Earth's History due to the Fact that Sample Core Tools and the Power systems to drive those into the seafloor is limited in it's size and strength.
Should we obtain a mile long tube with the power to drive it into the seafloor: We will find great a wealth of Data: and eventually, as it is believed , come to a point where our Dating system has found it's limit or a complete lack of fossils to date with.
When scientists were able to widely sample sea floor rocks, they were surprised to find that the oldest were only about 160 million years old. Soon after, the mid-ocean ridges were discovered, where new crustal rocks are being continuously created. And Plate Tectonics followed.
As to how is the rock dated, there are a number of radioactive transforms that are used. The Potassium - Argon decay is probably the simplest one. 40K has a half life of about 1.95 x 109 years before it decays into 40Argon (11%), and 40Calcium (89%).
Micas in the rock will have crystallized last, and these are commonly the mineral chosen to give the date.
The layer that is on top that rock is the newest , the one underneath is the oldest rock.
By existing catalogs developed over many years of what types of fossils are most commonly expected in sediment layers of what epochs.
by the age of rock samples
by diging it out
It helps them determine the frequency of shifts in the magnetic orientation of the Earth, and initially led to the confirmation of seafloor spreading at the mid-ocean ridges.
The age of rocks in the ocean crust depends on where the rocks are collected. Scientists collected rock samples from the sea floor. They found out that rock samples that were closer to mid-ocean ridges were younger than the samples farther away from the ridges. So pretty much you could get rocks that are thousands of years old to over millions of year old.
Scientists who study rocks are called petrologists.
Forms by lava from volcanoes on the sea floor
On each side of the mid-ocean ridge is a mirror of the striped pattern on the other side. When drawn, these patterns show alternating bands of normal and reverse polarity that match the geomagnetic reversal time scale, scientists can assign ages to the sea-floor rocks. The youngest rocks were at the center, and the older rocks father away. The ages of the sea floor rocks are symmetrical. The only place on the ocean-floor where new rocks are formed are at the rift in mid-ocean ridge. hope this helps :)
On each side of the mid-ocean ridge is a mirror of the striped pattern on the other side. When drawn, these patterns show alternating bands of normal and reverse polarity that match the geomagnetic reversal time scale, scientists can assign ages to the sea-floor rocks. The youngest rocks were at the center, and the older rocks father away. The ages of the sea floor rocks are symmetrical. The only place on the ocean-floor where new rocks are formed are at the rift in mid-ocean ridge. hope this helps :)
Types of rocks are inside the Earth, so scientists study them.
On each side of the mid-ocean ridge is a mirror of the striped pattern on the other side. When drawn, these patterns show alternating bands of normal and reverse polarity that match the geomagnetic reversal time scale, scientists can assign ages to the sea-floor rocks. The youngest rocks were at the center, and the older rocks father away. The ages of the sea floor rocks are symmetrical. The only place on the ocean-floor where new rocks are formed are at the rift in mid-ocean ridge. hope this helps :)
Scientists date sea-floor rocks by looking at patterns in the rocks, including magnetic patterns, and by looking at the geomagnetic reversal time scale.
Scientists who study rocks are called petrologists.
you can find the youngest rocks on the top of the ocean floor.
Scientists concluded that meteroroids had bombared the moons surface.
they classify the rocks by their texture and compisition
We look at the ocean floor to study the mantle because the ocean floor is made from rocks that were once part of the mantle but have be changed. These changes can be undone to a certain degree, and can allow us to study at the very least the major changes of the shallow mantle.
There are no rocks on the ocean floor because they turn to sand. The moving of the water gradually wears away at the rocks.
Rocks on the sea floor are very young because most have resulted from recent volcanic activity. Volcanic activity is constantly erupting on the ocean's floor and creating new rocks.