Rock A has a superior hardness to rock B
A dike is formed when lava cuts across rock layers and hardens. This igneous intrusion results in a narrow, tabular rock formation that can be exposed on the Earth's surface due to erosion or uplift.
When magma cuts across another rock and hardens, the resulting formation is called an "intrusion" or "igneous intrusion." This occurs when molten rock, or magma, forces its way into pre-existing rock layers and solidifies, typically forming structures such as dikes or sills. Intrusions are important in understanding geological processes and the history of the Earth’s crust.
Rubbing a rock against porcelain can test the hardness of the rock. If the rock leaves a scratch on the porcelain, it indicates that the rock has a higher hardness level than the porcelain. This can help in identifying the relative hardness of the rock based on the Mohs scale.
Diamond is the hardest natural material and can cut through other rocks. Its exceptional hardness is due to its unique crystal structure.
A pluton that cuts across existing rock layers is known as a cross-cutting pluton. This occurs when magma intrudes into pre-existing rock formations and solidifies, creating an igneous body that disrupts the original stratigraphy. The principle of cross-cutting relationships in geology states that the features that cut across others are younger than the rocks they intersect. Examples of such plutons include dikes and stocks.
Lava that cuts across rock layers hardens to form a feature called a Dike.
A crosscutting feature occurs when a rock or body of sediment cuts across, through fractures, faults, or magma. Any feature that cuts across must be younger than the rock or sediment that it cuts across.
What is the narrow tube-like body of intrusive igneous rock that cuts across existing rock calle
an intrusive body of magma that cuts across layers of rock
A dike is formed when lava cuts across rock layers and hardens. This igneous intrusion results in a narrow, tabular rock formation that can be exposed on the Earth's surface due to erosion or uplift.
The principle you are referring to is the principle of cross-cutting relationships. It states that any feature that cuts across a rock must be younger than the rock it cuts across. This applies to intrusive rock bodies, which are younger than the rocks they intrude into.
Dikes are always younger than the surrounding rock layers. The same holds true for any kind of intrusion. It will always be younger than anything that it is intruding into. To put it simply, you can't force an object into a bed of rock unless the bed of rock is already there.
The relative age of the fault is younger than the sedimentary rock layers it cuts across. The fault must have formed after the deposition of the sedimentary rock layers, as it disrupts them.
The rock would likely be classified as having a hardness of around 3.5 on the Mohs scale of mineral hardness. This would indicate that the rock is softer than minerals like quartz but harder than minerals like calcite. Examples of rocks with this hardness include gypsum and calcite.
A crosscutting feature is always younger than the rock layers it cuts through because the feature always forms after the rock layers have been formed, making the rock layers older.
A crosscutting feature is always younger than the rock layers it cuts through because the feature always forms after the rock layers have been formed, making the rock layers older.
dike.