Geographically, an intermontane plateau is one that is “cradled” between mountain ranges. The Mexican Plateau fits this definition perfectly, as it is bounded by the massive Sierra Madre folds. This positioning creates a unique climate; the mountains block moist air from the Gulf of Mexico and the Pacific, making the plateau interior relatively arid. In contrast, the Patagonian Plateau is a piedmont type (at the foot of mountains) and the Laurentian Plateau is a continental shield. Understanding these distinctions is vital for classifying landforms based on their relationship with surrounding tectonic features.