The Continental Divide of the Americas does not enter Mexico. Its southern terminus lies at the U.S.–Mexico border in New Mexico—specifically near the Playas Valley / Animas Mountains region (approx. 31.8°N, 108.5°W).
The Divide separates Pacific-bound (Colorado River) from Atlantic/Gulf-bound (Rio Grande, Pecos) drainage. South of the border, the Mexican Plateau lacks a continuous crest—drainage becomes complex, endorheic (internal), or Pacific-bound without a clear dividing line. The hydrologic "divide" concept breaks down in the basin-and-range topography.
People conflate the Continental Divide with the U.S.–Mexico border or the Sierra Madre Occidental (Mexico's western spine). The Sierra Madre is a mountain range, not the continental drainage divide.
Key takeaway: The Continental Divide is a hydrologic concept—it ends where drainage separation ceases to be continentally meaningful, at the U.S.–Mexico border in southwestern New Mexico.