Meanders are not characteristic of young rivers. They indicate a mature or old stage of river development.
Meanders develop when a river's energy shifts from vertical erosion (downcutting) to lateral erosion (sidecutting). Helical flow patterns erode outer banks (cut banks) and deposit on inner banks (point bars), amplifying bends over time.
The confusion may arise because meanders are dynamic—actively migrating and changing—which might seem "youthful." But they require the low gradient and floodplain development that only come with maturity.