it will have cracks and it will start to sink and rise
Three types of evidence supporting the idea of seafloor spreading include magnetic striping of the ocean floor (paleomagnetism), the presence of young volcanic activity near mid-ocean ridges, and the discovery of deep-sea hydrothermal vents that release hot mineral-rich water. These pieces of evidence suggest that new oceanic crust is continuously forming at mid-ocean ridges and spreading outward.
Magnetic striping: Patterns of alternating magnetic polarity in the rock of the ocean floor provide evidence of the seafloor moving away from mid-ocean ridges. Age of the oceanic crust: Younger rocks are found nearer to mid-ocean ridges, supporting the idea of continuous seafloor creation. Ocean drilling samples: Rock samples from the ocean floor show consistent patterns of increasing age with distance from mid-ocean ridges, supporting the theory of seafloor spreading.
The discovery of mid-ocean ridges, where new oceanic crust is formed, supported the theory of sea-floor spreading. The mapping of magnetic stripes on the ocean floor, showing alternating patterns of magnetic polarity, provided further evidence for sea-floor spreading. The age of the oceanic crust getting progressively younger away from the mid-ocean ridges supported the concept of sea-floor spreading.
The three types of imprint evidence are footwear impressions, tire impressions, and tool marks. Footwear impressions are left behind by shoes, tire impressions by vehicle tires, and tool marks by tools or objects in contact with a surface. They are useful in forensic investigations to identify the source of the imprint.
The three types of plate boundaries are divergent boundaries, where plates move away from each other; convergent boundaries, where plates move towards each other; and transform boundaries, where plates slide past each other horizontally.
Mid-ocean ridge spreading: Tectonic plates move apart at mid-ocean ridges, causing magma to rise from beneath the Earth's crust and solidify, creating new oceanic crust. Back-arc basin spreading: Tectonic plates separate at back-arc basins behind subduction zones, leading to the formation of new oceanic crust. Rift spreading: Continental rift zones experience seafloor spreading when a continent begins to split apart, forming a new ocean basin.
Earthquakes along the seafloor, tsunamis, and changed water movements.
Three types of evidence supporting the idea of seafloor spreading include magnetic striping of the ocean floor (paleomagnetism), the presence of young volcanic activity near mid-ocean ridges, and the discovery of deep-sea hydrothermal vents that release hot mineral-rich water. These pieces of evidence suggest that new oceanic crust is continuously forming at mid-ocean ridges and spreading outward.
Earthquakes along the seafloor, tsunamis, and changed water movements.
Seismic Waves, Rock formations, and the shapes of the continents over time
Seismic Waves, Rock formations, and the shapes of the continents over time
three are : eruptions of molten material magnetic stripes in the rock of the ocean floor and the ages of the rocks themselves :)
three are : eruptions of molten material magnetic stripes in the rock of the ocean floor and the ages of the rocks themselves :)
Magnetic striping: Patterns of alternating magnetic polarity in the rock of the ocean floor provide evidence of the seafloor moving away from mid-ocean ridges. Age of the oceanic crust: Younger rocks are found nearer to mid-ocean ridges, supporting the idea of continuous seafloor creation. Ocean drilling samples: Rock samples from the ocean floor show consistent patterns of increasing age with distance from mid-ocean ridges, supporting the theory of seafloor spreading.
Morphological evidence.Genetic and genomic evidence.Geographical evidence.
Three types of plate boundaries are spreading boundaries, colliding boundaries, and sliding boundaries. um actually they are divergent, convergent, and transform
Well all I have to say is y'all are real stuffy and messy on here and if u all don't have anything good to say dnt even get on my website