Water H2O Is An Example Of . Electronegativity is defined as the ability of an atom to attract electrons in a chemical bond. View chem cpt 2.docx from med 101 at lincoln technical institute, new britain. Water Buoyancy, Cohesion & Adhesion Kids Discover from www.kidsdiscover.com Electrons are shared between the hydrogen and. An ionic bond is a type of chemical bond in which the atoms have different electronegativity values from each other. H2o is a molecular formula, since it shows the actual number of each atom in the molecule, and it is also an empirical formula since it shows the atoms in their simplest ratio (2.
Convergent Oceanic Oceanic Example. After that new crust is made, while magma rises up to form volcanoes, it can also make under water volcanoes. When a supercontinent such as pangaea breaks up, a diverging boundary can be found in the middle of a continent.
Convergent Boundaries EXPLORE LEARN from khsappliedgeography.weebly.com
It is viscous, trapping gases as it. Earthquakes occur in the benioff zones that dip underneath the continental edge. Andesitic magma is less dense than the surrounding material, and can have a temperature of 1000 o c.
The Marianas Trench, For Example, Is A Deep Trench Created As A Result Of The Philippine Plate Subducting Under The Pacific Plate.
This is the point where the north and south american plates are subducting underneath the caribbean plate. When two oceanic plates meet, one plate sinks below the other. Challenger deep, the deepest part of the oceans is part of the marina trench in the subduction zone between the pacific and philippine plates.
Andesitic Magma Is Less Dense Than The Surrounding Material, And Can Have A Temperature Of 1000 O C.
See answer (1) best answer. When an oceanic plate meets up with another oceanic plate, the colder, the older, and denser oceanic plate starts to bend and sink into the mantle part. This produces magma, which rises and may be erupted explosively as andesite at the surface.
Colder, Denser And Older Oceanic Lithosphere Subducts Back Into The Asthenosphere (Slab Drag) J.
Above is a cross section of the oceanic trench found at this convergent boundary. When two plates converge one is usually subducted under the other and in the process a deep oceanic trench is formed. As with the convergence of oceanic and continental plates, trenches are formed at the subduction zone.
The Aleutian Islands Of Alaska Are An Example Of An Island Arc.
As the plate heats up the water is liberated, lowering the melting point of the mantle and causing partial melting. Any convergent boundaries containing an oceanic crust will result in the most dense oceanic lithosphere subducting and an oceanic trench at. Earthquakes occur in the benioff zones that dip underneath the continental edge.
• There Are Three Types Of Convergent Plate Boundaries:
An example would be the convergence of the oceanic nazca plate colliding with the continental south american plate producing the andes mountain chain. The andes mountain range of western south america is another example of a convergent boundary between an oceanic and continental plate. When a supercontinent such as pangaea breaks up, a diverging boundary can be found in the middle of a continent.
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