The Seafloor Magnetic Pattern Is Best Described as

By combining magnetic polarity data from rocks on land and on the seafloor with radiometric age dating and fossil ages scientists came up with a time scale for the magnetic reversals. The seafloor magnetic pattern is best described as.


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C parallel to but not symmetric about mid-ocean ridges.

. Parallel to and symmetric about mid-ocean ridges O c. B not related to the location of mid-ocean ridges. The first four magnetic periods are.

Asked By Wiki User. 3 The seafloor magnetic pattern is best described as _____. This is because the oldest sea floor is subducted under other plates and replaces by new surfaces.

Parallel to and symmetric about mid-ocean ridges c. Matuyama reverse - 730000 years ago to 248 million years ago. In most elements electrons are paired and each electron of the pair spins in an opposite direction.

Parallel to and symmetric about ocean ridges. The seafloor magnetic pattern is best described as _____ asked Sep 22 2016 in Environmental Atmospheric Sciences by Unique. Perpendicular to and symmetric about mid-ocean ridges e.

B the magnetic pattern of rocks on the seafloor. Not related to the location of mid-ocean ridges b. The seafloor magnetic pattern is best described as.

Asked Aug 31 2020 in. Arguments are presented suggesting that important characteristics of the anomaly patterns could be due to the measurement process itself rather than being a direct reflection of geomagnetic reversals and plate movement. But movement of molten rock creates the magnetic field in the outer core.

The center of Earth is too hot to support an electric field. Perpendicular to and symmetric about mid-ocean ridges. Very little of the sea floor is older than 150 million years.

36 The seafloor magnetic pattern is best described as. The seafloor magnetic pattern is best described as a not related to the location The seafloor magnetic pattern is best described as a School California Polytechnic State University San. A not related to the location of mid-ocean ridges.

Confirmation of seafloor spreading was supported by the. This is their best hypothesis. E fossils in marine sediments.

B perpendicular to but not symmetric about mid-ocean ridges. D perpendicular to and symmetric about mid-ocean ridges. Parallel to but not symmetric about mid-ocean ridges d.

The seafloor magnetic pattern is best described as 9 A parallel to and symmetric. The seafloor magnetic pattern is best described as Select one. Magnetic anomalies are best described as-Parallel to but not symmetric about ocean ridges-Perpendicular to and symmetric about ocean ridges-perpendicular to but not symmetric about ocean ridges-Parallel to and symmetric about ocean ridges.

What is the summary for the poem A Song in. The Seafloor Magnetic Pattern Is Best Described As Parallel to and symmetric about ocean ridges. Confirmation of seafloor spreading was supported by the.

The seafloor magnetic pattern is. The tectonic plates are constantly in motion and new surfaces are always being created. The oceanic patterns of magnetic anomalies are thought to be one significant evidence supporting the general notions of plate tectonics.

Brunhes normal - present to 730000 years ago. Parallel to but not symmetric about mid-ocean ridges. Not related to the location of mid-ocean ridges.

C parallel to but not symmetric about mid-ocean ridges. B parallel to and symmetric about mid-ocean ridges. Scientists use the magnetic polarity of the sea floor to determine the age.

A not related to the location of mid-ocean ridges. Vine and Matthews determined that new ocean floor was being produced at ocean ridges by examining. Parallel to and symmetric about mid-ocean ridges.

The seafloor magnetic pattern is best described as 9 A parallel to and symmetric from GEOL 1003 at Acadia University. The seafloor magnetic pattern is be best described as. A not related to the location of mid-ocean ridges B parallel to and symmetric about mid-ocean ridges C parallel to but not symmetric about mid-ocean ridges D perpendicular to and symmetric about mid-ocean ridges E perpendicular to but not symmetric about mid-ocean ridges.

Heavy elements like iron make the journey from the mantle to the crust via volcanic activity. The seafloor magnetic pattern is best described as. Perpendicular to but not symmetric about mid-ocean ridges.

Magnetic stripes in oceanic basalts are _____ and _____ around ocean ridges. Thermal contraction of hot lithosphere. A parallel to and symmetric about mid-ocean ridges.

E parallel to and symmetric about mid-ocean ridges. The seafloor magnetic pattern is best described as Select one. Perpendicular to but not symmetric about mid-ocean ridges.

The Seafloor Magnetic Pattern Is Best Described a April 13 2022 The oceanic patterns of magnetic anomalies are thought to be one significant evidence supporting the general notions of plate tectonics. 9 The seafloor magnetic pattern is best described as ________.


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