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.

this protocol provides a detailed procedure for co-immunoprecipitation (co-ip) to identify protein–protein interactions.