The three phases of the Moon's later history included the formation of the original crust, followed by the creation of the maria basins, and then the development of the highland regions. After the crust solidified, volcanic activity led to the filling of large basins with basaltic lava, forming the smooth, dark maria. Subsequently, the highlands emerged as the Moon's surface continued to evolve and experience impacts, resulting in the rugged terrain we see today. Each phase reflects significant geological processes and impacts in the Moon's history.
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