<?xml version='1.0' encoding='UTF-8'?><metadata xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dcterms="http://purl.org/dc/terms/" xmlns="http://dublincore.org/documents/dcmi-terms/"><dcterms:title>DEMs for Experiment 2</dcterms:title><dcterms:identifier>https://doi.org/10.21979/N9/DCEIWZ</dcterms:identifier><dcterms:creator>Harisma Andikagumi</dcterms:creator><dcterms:publisher>DR-NTU (Data)</dcterms:publisher><dcterms:issued>2023-01-17</dcterms:issued><dcterms:modified>2023-01-19T03:51:40Z</dcterms:modified><dcterms:description>Digital elevation models (DEMs) for Experiment 2 (linearly decreasing ejection volume, constant viscosity)</dcterms:description><dcterms:subject>Earth and Environmental Sciences</dcterms:subject><dcterms:subject>volcanology</dcterms:subject><dcterms:subject>analogue modelling</dcterms:subject><dcterms:isReferencedBy>Andikagumi, H., de Maisonneuve, C. B., &amp; Taisne, B. (2023). The growth of polygenetic volcanoes in the laboratory: Control of eruptive volume and magma viscosity on edifice development and morphology. Geomorphology, 108588., doi, 10.1016/j.geomorph.2023.108588, https://www.sciencedirect.com/science/article/abs/pii/S0169555X23000089</dcterms:isReferencedBy><dcterms:contributor>Harisma Andikagumi</dcterms:contributor><dcterms:dateSubmitted>2022-11-22</dcterms:dateSubmitted><dcterms:type>Digital Elevation Model</dcterms:type><dcterms:license>CC BY-NC 4.0</dcterms:license></metadata>