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<rdf:RDF xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#" xmlns:dc="http://purl.org/dc/elements/1.1/"><rdf:Description rdf:about="https://dirros.openscience.si/IzpisGradiva.php?id=29050"><dc:title>Shapes of ideal stalagmites</dc:title><dc:creator>Szymczak,	Piotr	(Avtor)
	</dc:creator><dc:creator>Ladd,	Anthony J. C.	(Avtor)
	</dc:creator><dc:creator>Lipar,	Matej	(Avtor)
	</dc:creator><dc:creator>Pekarovič,	Dean	(Avtor)
	</dc:creator><dc:subject>geomorphology</dc:subject><dc:subject>physics</dc:subject><dc:subject>karst</dc:subject><dc:subject>stalagmites</dc:subject><dc:description>Stalagmites are isolated columns of calcium carbonate growing on a cave ﬂoor; theirgrowth is driven by the constant dripping of supersaturated solutions from the roofof the cave. In this paper, we derive a closed-form expression for the shape of asteadily growing stalagmite. Our analysis gives rise to three distinct shapes, all of themobservable in nature, with the shape characterized by a single dimensionless parameter.Transitions between different shapes occur at a speciﬁc value of this parameter, withadditional selection rules determining the shape and size of stalagmites evolving underspeciﬁc cave conditions. Our theory shows that the stalagmite shape inﬂuences the 13Cisotope shifts, which are an important source of paleoclimatic information.</dc:description><dc:date>2025</dc:date><dc:date>2026-04-20 09:53:29</dc:date><dc:type>Neznano</dc:type><dc:identifier>29050</dc:identifier><dc:language>sl</dc:language></rdf:Description></rdf:RDF>
