The Rocks On The Ocean Floor Are Magnetic

Magnetic direction of rock changes as earth s magnetic poles drift.

The rocks on the ocean floor are magnetic.

This is how scientists get the age of the seafloor. Magma acquires the magnetic direction present on earth when it hardens into rock 3. As rocks crystallize from lava at the ridges they literally record the magnetic field of the earth at the time of their creation. Several types of evidence supported hess s theory of sea floor spreading.

This evidence led scientists to look again at wegener s hypothesis of continental drift. Basalts contain magnetic minerals which get aligned in the direction of the magnetic field when the rock solidifies. Eruptions of molten material magnetic stripes in the rock of the ocean floor and the ages of the rocks themselves. The ocean floor is mainly made up of basalt which is formed as a result of underwater volcanic activity.

The volcanic and sedimentary rocks record the paleomagnetism at the time when that part of the ocean floor was created. Among the new findings was the discovery of zebra stripe like magnetic patterns for the rocks of the ocean floor. Select the two correct answers. New rock is formed by magma at the mid ocean ridges and the ocean floor spreads out from this point.

Identify the factors that cause magnetic stripes to form along the ocean floor. Plates move as new rock forms which causes magnetic direction to skew away. These two things were the magnetic striping on the ocean floor and the age of seafloor rocks. Magnetic striping magnetic minerals are found in rocks.

Basalt the once molten rock that makes up most new oceanic crust is a fairly magnetic substance and scientists began using magnetometers to measure the magnetism of the ocean floor in the 1950s what they discovered was that the magnetism of the ocean floor around. The oceanic crust displays a pattern of magnetic lines parallel to the ocean ridges frozen in the basalt. The magnetism of mid ocean ridges helped scientists first identify the process of seafloor spreading in the early 20th century. These stripes of normal and reverse magnetic fields with different sizes can be matched with the geomagnetic reversals records obtained from continental rocks already dated.

Magnetic stripes and isotopic clocks oceanographic exploration in the 1950s led to a much better understanding of the ocean floor. Magnetic striping of the sea floor after mid ocean ridges and trenches were discovered more evidence was discovered that helped to support the theory that the continents had moved around. When magma flows out of a mid ocean ridge small magnetic minerals in the magma align themselves to point in the direction of the earth s current magnetic north. These patterns were unlike any seen for continental rocks.

Plate tectonics and reversals of the earth s magnetic field are responsible for the magnetic stripes found on the ocean floor. The fraction of a rocks overall magnetization that is a viscous remanent magnetization is dependent on the magnetic mineralogy. Evidence from molten material. Paleomagnetic procedure collecting samples on land.