Construct · 1 fields · 1 citations
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Pahoehoe is a basaltic lava flow with a smooth, billowy, or ropy skin, formed when fluid, low-viscosity, relatively gas-poor lava advances under a flexible chilled crust, often spreading as toes and lobes. Macdonald's 1953 comparison of pahoehoe, aa, and block lava fixed the distinction: pahoehoe's unbroken ropy surface contrasts with the rubbly, clinkery top of aa, into which pahoehoe can transform as it cools and is stirred. The referent is a lava-surface morphology tied to flow rheology and strain rate, a different surface type from aa and block lava.[1]
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