The Earth's rotation is slowing but at a much slower rate than 1 leap second every so many years. The length of time it takes the Earth, at the present time, to rotate once is 86,400.002 seconds compared to 86,400 seconds back in 1820. The rotation has slowed roughly only by 2 milliseconds since 1820. That seems like an insignificant amount of time BUT over the course of the planet's entire lifetime, it has had very profound effects on the geophysics of the planet.
It has caused mountains to rise, earthquakes, etc. to occur as we will see. This article is about, factoring in the tremendous geophysical activity that was caused, by the Earth's slowing rotation, in the interior of the planet, its crust, oceans and atmosphere over its entire lifetime.
The Sub-bureau for Rapid Service and Predictions of Earth Orientation Parameters of the International Earth Rotation Service (IERS), located at the US Naval Observatory, monitors the Earth's rotation. Part of its mission involves the determination of a time scale based on the current rate of the rotation of the Earth.
They estimate that the Earth's rotation is slowing at about 1.4 milliseconds per solar day per century which roughly agrees with the rate of rotation of the Earth has actually slowed down since 1820.
Tracing these tiny milliseconds back for 4.5 billion years adds up to a very significant amount of time for a solar day. I have determined that the day/night rotation was 63,000 seconds shorter than the present 86,400 seconds it is today. This would put the Earth's rotation at about 6.5 hours per day/night cycle, when it was created, 4.5 billion years ago. (This is a much faster rate of rotation than the Cassini-Huygens mission (2003 to 2004) determined Saturn's 10.5 hours rotation period to be.)
This rate of rotation would have exerted tremendous stress throughout the newly formed planet. If the rate of rotation has been slowing fairly constantly, over the ages, we can see that the earth was rotating very fast originally, for it to slow down to the present 24 hour rate it is today. What ever it was - its angular momentum was much faster and therefore its "centrifugal force" was tremendously strong when the planet was very young. This caused the young, fast spinning, Earth to have a much more pronounced oblate shape, possibly even having a "Saturn type ring" orbiting around it.
In the past, when the Earth was younger and spinning faster, the stronger angular momentum caused the Earth to assume a more pronounced oblate spheroid shape much greater than the twenty-seven miles it is today. A 15% increase in the equatorial circumference of the faster rotating young planet, relative to its present rotation, could produce approximately 3600 more miles of surface around the young planet's equatorial zone.
This was a lot of surface to crunch into the ever changing shape of the planet as its rotation gradually slowed over the ages. Since the ratio of strength of gravity and angular momentum (centrifugal force)is always changing, the shape of the planet never reaches equalibrium - it is always changing.
(The fast spinning star, Vega, makes a full rotation about its axis once every 12.5 hours, (only about 1/2 the Earth's early rate) which causes it to assume a 23% ellipical bulge at its equator, so a 15% greater bulge for the faster spinning Earth is not out of the question.)
The constant struggle between gravitational force and the weakening angular momentum caused by the slowing of the Earth's rotation, has had a profound effect on the Earth's geophysical activity throughout the ages. This constant struggle between these two gigantic forces has caused a continual adjusting of the Earth's shape as the ratio of the strengths of angular momentum and gravity have changed.