Igneous rocks that have recently solidified at the ridge crest would typically exhibit a magnetic anomaly known as normal magnetization. This occurs because the iron-bearing minerals within the magma align with the Earth's magnetic field as the rocks cool and solidify. Since these rocks form at mid-ocean ridges, they will record the current orientation of the Earth's magnetic field at that time, leading to a positive magnetic anomaly. Over time, as the magnetic field reverses, older rocks will show alternating patterns of normal and reversed magnetization, contributing to the seafloor magnetic stripe pattern.
igneous rock
igneous rocks are made of solidified lava.
Igneous rocks are formed from melted rock that has cooled and solidified. Examples include granite, basalt, and obsidian.
Such rock is referred to as plutonic igneous rock if it is part of a large solidified mass of magma at large depths in the crust, or as intrusive igneous rock if simply solidified at some depth within the crust. Plutonic igneous rock is therefore a type of intrusive igneous rock.
Uplift and solidification
Solidified magma or lava is igneous rock.
igneous rock
Igneous rock is formed from solidified and cooled magma or lava.
igneous rocks are made of solidified lava.
Solidified magma or lava.
Igneous rocks are formed from melted rock that has cooled and solidified. Examples include granite, basalt, and obsidian.
It's called extrusive igneous rock--rapidly solidified lava.
Intrusive igneous rock.
The igneous rock is formed when a rock that is solidified from molten or partly molten matierial.
Igneous rocks, which come in many different forms.
Hot lava, when cooled and solidified, forms igneous rocks. Examples include basalt, granite, and obsidian.
Basalt, the extrusive igneous rock that comprises most of the oceanic crust, is the most common type of solidified lava.