Continental shields, or cratons, are generally of low elevation and old in age.

Question

Quizplus · Accepted Answer

Continental shields, or cratons, are indeed generally of low elevation and old in age. They are the ancient, stable cores of continents and are composed mostly of Precambrian rocks that have been deformed and eroded over time. These shields have not experienced tectonic activity in millions of years, making them relatively flat and low-lying compared to younger, more mountainous regions.

Continental Shields, or Cratons, Are Generally of Low Elevation and Old