雅思阅读

📖 Reading Passage

The concept of 'deep time' in geology challenges the human tendency to perceive time on a human scale. Unlike the cyclical rhythms of seasons or the linear progression of a lifetime, deep time encompasses billions of years, during which continents drift, climates shift, and species evolve and vanish. This vast temporal framework was first systematically articulated in the 18th century by James Hutton, who argued that the Earth's history could not be explained by catastrophic events alone but required slow, uniform processes operating over immense durations. Modern geology reinforces this view through radiometric dating, which reveals that some rocks are over four billion years old. However, the human mind struggles to grasp such magnitudes, often leading to a 'temporal provincialism' that underestimates the pace of environmental change. Recognizing deep time is not merely an academic exercise; it is crucial for understanding current climate dynamics, as natural variability operates on timescales far exceeding recorded history.