caa a22 4500 606149805 CHVBK 20210128100536.0 cr unu---uuuuu 210128e20151101xx s 000 0 eng 10.1007/s00531-015-1243-6 doi (NATIONALLICENCE)springer-10.1007/s00531-015-1243-6 Monogenetic volcanism: personal views and discussion [Elektronische Daten] [K. Németh, G. Kereszturi] Monogenetic volcanism produces small-volume volcanoes with a wide range of eruptive styles, lithological features and geomorphic architectures. They are classified as spatter cones, scoria (or cinder) cones, tuff rings, maars (maar-diatremes) and tuff cones based on the magma/water ratio, dominant eruption styles and their typical surface morphotypes. The common interplay between internal, such as the physical-chemical characteristics of magma, and external parameters, such as groundwater flow, substrate characteristics or topography, plays an important role in creating small-volume volcanoes with diverse architectures, which can give the impression of complexity and of similarities to large-volume polygenetic volcanoes. In spite of this volcanic facies complexity, we defend the term "monogenetic volcano” and highlight the term's value, especially to express volcano morphotypes. This study defines a monogenetic volcano, a volcanic edifice with a small cumulative volume (typically≤1km3) that has been built up by one continuous, or many discontinuous, small eruptions fed from one or multiple magma batches. This definition provides a reasonable explanation of the recently recognized chemical diversities of this type of volcanism. Springer-Verlag Berlin Heidelberg, 2015 Monogenetic volcanism nationallicence Scoria cone nationallicence Maar nationallicence Tuff ring nationallicence Tuff cone nationallicence Cinder cone nationallicence Phreatomagmatic nationallicence Volume nationallicence Explosive nationallicence Conduit nationallicence Eruption nationallicence Németh K. Volcanic Risk Solutions, Institute of Agriculture and Environment, Massey University, Private Bag 11 222, Palmerston North, New Zealand aut Kereszturi G. Volcanic Risk Solutions, Institute of Agriculture and Environment, Massey University, Private Bag 11 222, Palmerston North, New Zealand aut International Journal of Earth Sciences Springer Berlin Heidelberg 104/8(2015-11-01), 2131-2146 1437-3254 104:8<2131 2015 104 531 https://doi.org/10.1007/s00531-015-1243-6 text/html Onlinezugriff via DOI BK010053 XK010053 XK010000 Metadata rights reserved Springer special CC-BY-NC licence nationallicence 1 research-article jats NATIONALLICENCE NATIONALLICENCE NL-springer NATIONALLICENCE 856 40 https://doi.org/10.1007/s00531-015-1243-6 text/html Onlinezugriff via DOI NATIONALLICENCE 700 1- Németh K. Volcanic Risk Solutions, Institute of Agriculture and Environment, Massey University, Private Bag 11 222, Palmerston North, New Zealand aut NATIONALLICENCE 700 1- Kereszturi G. Volcanic Risk Solutions, Institute of Agriculture and Environment, Massey University, Private Bag 11 222, Palmerston North, New Zealand aut NATIONALLICENCE 773 0- International Journal of Earth Sciences Springer Berlin Heidelberg 104/8(2015-11-01), 2131-2146 1437-3254 104:8<2131 2015 104 531