Seafloor spreading happens in both the Pacific and Atlantic Oceans, where new ocean crust forms at underwater ridges and pushes the older crust away from the ridge. In the Pacific Ocean, when the ocean crust meets land (continental plates), the older crust gets pushed underneath the land (this process is called subduction).
In the Pacific, more crust is being pulled back down into the Earth than is being made at the ridges. This means that the Pacific Ocean is getting smaller over time. In contrast, the Atlantic Ocean is getting bigger because it creates more new crust than it loses.