### Venusian Resurfacing
The surface of Venus has remarkably few impact craters, suggesting a relatively young surface age of 300 to 600 million years. Scientists agree that volcanism is responsible for erasing older craters, but they debate the timeline and nature of this resurfacing.
*Hypothesis 1*
Venus experiences episodic, global volcanic events. Because Venus lacks Earth-like plate tectonics, internal heat cannot escape steadily. Instead, heat builds up in the mantle over hundreds of millions of years, eventually causing the lithosphere to weaken and overturn. This leads to rapid, planet-wide volcanic resurfacing within a span of less than 100 million years, followed by a long period of geological inactivity during which heat accumulates again.
*Hypothesis 2*
Venus undergoes gradual, localized resurfacing. The planet is geologically active, with continuous but small-scale volcanic eruptions and tectonic deformation occurring in various regions at different times. Over hundreds of millions of years, these scattered, ongoing events gradually bury and erase older craters, maintaining a young average surface age without requiring a single, catastrophic global event.
Which of the following statements best summarizes the core claim of Hypothesis 2 regarding the resurfacing of Venus?
- The surface is renewed through steady, ongoing volcanic and tectonic processes occurring in localized areas.Answer
- BThe surface is renewed through sudden, global volcanic events triggered by mantle heat buildup.
- CThe surface is renewed through the continuous subduction and movement of global tectonic plates.
- DThe surface is renewed by intense solar radiation melting the crust in a uniform, planet-wide pattern.