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The fissures in the valleys of the mid-oceanic ridges are a outlet for lava flows reaching the ocean floor. The lava rolls out of these fissures cooling and hardening into new crust. This new crust however is soon broken open by new fissures which more lava pours out of, this causes the sea floor spreading, which explains the age discrepancy of the sea floor as it ranges away from the ridge...
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The floor nearer to the ridge is distinctly newer than the floor away from the ridge proportionally. As the lave flows away from the ridge, it becomes cooler and harder, growing denser and heavier as it does. This causes the lava to sink into the floor back down to the mantle near the edge of a continent or basin...
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