Skip to main content
Fig. 11 | Journal of Applied Volcanology

Fig. 11

From: The influence of vesicularity on grain morphology in basaltic pyroclasts from Mauna Loa and Kīlauea volcanoes

Fig. 11

The influence of grain size on the correlation between vesicularity and grain shape. Vesicularity values here represent vesicularities per pyroclast measured by pycnometry as in Fig. 4A-D. The color scale shows the general degree of shape regularity, calculated by adding up normalized values of elongation, sphericity, Krumbein roundness and compactness and normalizing the results between 0 and 1. A Vesicularity plotted against most dominant modal grain size of individually crushed pyroclasts. Each data point represents one crushed pyroclast sample, as in Fig. 4A-D. The most dominant modal grain size in each of these pyroclasts is calculated from dynamic image analysis data using Blott and Pye (2001). B Vesicularity plotted against grain size bin. Each data point (stripe) represents a subset of grains of one crushed pyroclast sample that fall in a certain grain size bin. Hence, every data point in (A) corresponds to multiple data in (B), representing one specific pyroclast

Back to article page