There are three laws of science that scientists use to date the crust by studying the layers of rocks. These laws are called the Law of Original Horizontality, the Law of Superposition, and the Law of Faunal Succession.
The main type of rock in oceanic crust is basalt. Basalt is a fine-grained igneous rock formed from the rapid cooling of lava at or near the Earth's surface. It is dark in color and rich in minerals like pyroxene and plagioclase feldspar.
relative dating is when you give an estimate date.
White rocks can come from a variety of sources, such as quartz, marble, or limestone. These rocks can form naturally through the deposition of minerals or chemical reactions in the Earth's crust. They can also be artificially produced through processes like grinding or crushing.
Absolute geologic time refers to the chronological age of a rock or event, typically measured in years. It is determined using radiometric dating techniques, which allow for precise dating of rocks and fossils based on the decay of radioactive isotopes. This provides a more accurate and quantitative way to establish the timing of geologic events in Earth's history.
The Earth consists of four main layers: the inner core, outer core, mantle, and crust. The inner core is solid and composed mainly of iron and nickel. The outer core is also composed of iron and nickel, but it is in a liquid state. The mantle is a semi-solid layer made up of silicate rocks, and the crust is the Earth's thin, solid outermost layer.
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it is determined by studying the relative and absolute ages of rocks and fossils
Earths under crust surrounded by Upper Mantle (35-60 km) .The mantle is composed of sillicate rocks that are rich in iron and magnesium relative to the overlying crust.
the crust and the core
iron and magnesium
it is made of rocks
Age is how old the rock is relative to other rocks, position is where the rock is in relation to other rocks. Tectonic motion and other forces can easily turn a portion of the Earths crust upside down resulting in older rock lying above younger layers.
Basalt and limestone.
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Silicates make up close to 95 percent of the rocks in the Earth's crust
The basic materials of the earths crust are; silicate rocks, primary granite, igneous, metamorphic, and sedimentary rocks.
The rule is that lower levels were laid down before upper levels. One has to be a little cautious where rocks are very distorted as the layers can become inverted.