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Measuring Deep Time: How Scientists Unraveled Earth's 4.5-Billion-Year History

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Introduction There is a particular difficulty in thinking about geological time. A human life is measured in decades. Written history reaches back only a few thousand years. Even the oldest monuments built by civilizations occupy almost no space at all when placed against the history of the planet. Yet the rocks beneath our feet preserve evidence of events that began hundreds of millions, and in some cases billions, of years ago. Earth is about 4.54 billion years old . Today, that number appears in textbooks, geological maps, scientific papers, and laboratory reports with almost casual familiarity. But the number was not always known, and it was not obtained from a single experiment. Scientists had to discover a way of measuring time on a scale for which human experience offered no useful reference. There was no geological clock large enough to watch for billions of years. There was no written record from Earth's earliest history. Even the oldest rocks preserved at the ...

Weathering: How Earth's Surface Breaks Down and Transforms Rocks

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Introduction A fresh rock surface can give a misleading impression of permanence. Stand beside a newly exposed rock face and it may look almost unchanged from the block of rock that was buried beneath the ground for thousands or millions of years. Its minerals are still recognizable, the joints are visible, and the rock may feel hard beneath a geological hammer. But exposure changes the conditions around it. Water begins to enter fractures. Oxygen reaches minerals that were previously isolated from the atmosphere. Temperature changes act on the exposed surface. Groundwater follows discontinuities that were once closed or only weakly connected. In some environments, roots and microorganisms become part of the process as well. The rock has entered a different stage of its geological life. This is weathering . Weathering is often introduced as the breakdown of rocks at or near Earth's surface. That definition is correct, but it does not fully describe what happens to an en...