‘雪丘’ (xuě qiū) literally combines ‘雪’ (xuě), meaning ‘snow’, and ‘丘’ (qiū), meaning ‘hill’ or ‘mound’. Together, they describe a natural accumulation of snow shaped into a rounded, hill-like pile—what English calls a ‘snowdrift’. Unlike the more general term ‘雪堆’ (xuě duī, ‘snow pile’), ‘雪丘’ emphasizes a distinct, often wind-sculpted, elevated form with gentle slopes, commonly seen in open fields, mountain passes, or along roads after heavy snowfall.

This word is used primarily in descriptive or literary contexts—especially in weather reports, nature writing, or travel narratives—to evoke imagery of winter landscapes. It’s not typically used for small or irregular piles of snow (e.g., those shoveled by hand), nor for icy or compacted snow formations like ‘冰丘’ (bīng qiū, ‘ice mound’). Native speakers tend to use it when highlighting shape, scale, and natural origin rather than just quantity.