See more ideas about seafloor spreading earth science plate tectonics.
Sea floor spreading cartoons.
Small dog being taken for walk undersea using snorkel to breath.
Displaying top 8 worksheets found for sea floor spreading answer key.
The process is continuous because forces cause opposite sides of the midocean ridge to constantly move apart making new room for the process to repeat.
Some of the worksheets for this concept are sea floor spreading work inside earth work name date sea floor spreading l 1 2 3 a model of seafloor spreading sea floor spreading sea floor spreading modeling sea floor spreading chapter 8 plate tectonics.
Spreading rates determine if the ridge is fast intermediate or slow.
Seafloor spreading occurs along mid ocean ridges large mountain ranges rising from the ocean floor.
We are two sisters on a mission to demystify science with humor and relevance by creating videos gifs comics and resources such as our handouts and unlectured series our focus is high school biology as pinky is a former high school biology teacher but we receive feedback that some of our videos are useful for introductory biology at the college level and any other levels that are.
I didn t know it would come to this.
Apr 6 2020 explore marion mcclary s board seafloor spreading on pinterest.
The rate at which new oceanic lithosphere is added to each tectonic plate on either side of a mid ocean ridge is the spreading half rate and is equal to half of the spreading rate.
The mid atlantic ridge for instance separates the north american plate from the eurasian plate and the south american plate from the african plate the east pacific rise is a mid ocean ridge that runs through the eastern pacific ocean and separates the pacific plate from the north american.
I m sorry you somehow found this.
Have you noticed lately that your students just aren t listening when you try to teac.
Seafloor spreading is the continuous process of forming new igneous rock at midocean ridges by injection of magma that forms new seafloor.
Spreading rate is the rate at which an ocean basin widens due to seafloor spreading.