What evidence exists for sea floor spreading? explain.

ocean bottom spreading is a procedure that happens at mid-sea edges, where new maritime outside is shaped through volcanic action and after that continuously moves from the edge.  

explanation:

there are three distinct kinds of proof that exist for ocean bottom spreading, these are:  

1. rocks situated close to the mid-sea edge are more youthful than rocks situated close trenches.  

2. comparable groups of attractive rocks are found on the two side of the mid-sea edge.  

3. data acquired from seismic tremor occasions demonstrate that maritime outside layer is sinking into the mantle at the trenches.  

ocean bottom spreading is a geographical procedure in which structural plates move separated from one another. the point recorded above are the proof that ocean bottom spreading happens.

one is through turgidity. this occurs before ground tissue ( collenchyma

and sclerenchyma cells) become well

developed to give structural support to the plant as it grows bigger. the xylem

tissue (composed of rigid tissue) of the young

plant render this support and also maintaining osmotic turgidity of the surrounding

plant cells.