Difficulty: Easy
Correct Answer: 3 km above sea level
Explanation:
Introduction / Context:
The term snow line refers to the altitude above mean sea level where snow persists year-round, balancing accumulation and melt. Its height varies with latitude, continentality, and local climate. In mid-latitude continental ranges like the Rocky Mountains (USA), the snow line is substantially higher than in maritime ranges at the same latitude.
Given Data / Assumptions:
Concept / Approach:
Snow line elevation increases with decreasing latitude and with increasing continentality. Dry, sunny summers promote ablation, raising the equilibrium line altitude. In the mid-latitudes of the western USA, many glaciers and perennial snowfields cluster near or above about 3,000–3,500 m. Values around 6,000 m are unrealistic for the contiguous USA, and sea level snow lines occur only in polar regions.
Step-by-Step Solution:
Identify the target mountain system and its latitude: mid-latitudes with inland continental influences.Recall typical equilibrium line altitudes in the Rockies: near 3,000–3,500 m depending on aspect and region.Compare choices: 3 km is plausible; 6 km exceeds North America’s highest peaks; sea level applies only to polar coasts.Select the closest appropriate figure: 3 km above sea level.
Verification / Alternative check:
Topographic maps and glacier inventories show persistent summer snow and small glaciers primarily above ~3,000 m in Colorado’s Front Range and other Rocky subranges, confirming the order of magnitude.
Why Other Options Are Wrong:
Common Pitfalls:
Confusing the winter snowline (seasonal) with the perennial snow line. Do not generalize maritime values (lower) to continental interiors (higher).
Final Answer:
3 km above sea level
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