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It depends on the meaning of "tend to." They tend to not be as common, but yes they do occur for a variety of reasons, including glacial rebound ... the great ice sheets that covered continents, such as North America, were so massive that they actually pressed the North American continent down, like loading a massive block of ice onto a relatively small ship, it caused the ship -- North America -- to sink down into the mantle a bit. When the great ice sheets that caused the continent to be pressed downward melted and the water from it drained away, the continental interior was no longer in equilibrium -- in the previous hypothetical analogy, after the massive block of ice melts off the ship, its mass no longer presses the ship downward and the ship bobs upward. The continent rebounds upward from its massive ice-depressed lower level, but the upward motion is not smooth and causes strain within the continental bedrock, leading to earthquakes deep within the continent instead of the more common earthquakes occurring at the continent's edges.

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