Tuff Cone is a volcanic landform characterized by a broad, low-rising profile constructed predominantly of explosively ejected pyroclastic material, especially ash and lapilli, typically formed by phreatomagmatic eruptions involving interaction between magma and external water.
92
Publications
3.9K
Citations
263
Authors
121
Institutions
Publications per year
2017–2026
17
Variants
Tuff Cone
Parents
Publications
92
1–5 of 92
Authors
263
- YK
7
h-index
- KN
6
h-index
- SJ
4
h-index
- WH
3
h-index
- HB
3
h-index
1–5 of 263
Institutions
121
Universidad Nacional Autónoma de México
Mexico City, Mexico
6 h-index
9 publications
330 citations
Gyeongsang National University
Jinju-si, South Korea
5 h-index
6 publications
509 citations
Istituto Nazionale di Geofisica e Vulcanologia
Rome, Italy
5 h-index
19 publications
390 citations
Massey University
Palmerston North, New Zealand
4 h-index
13 publications
480 citations
University of Auckland
Auckland, New Zealand
4 h-index
5 publications
181 citations
University of Oxford
Oxford, United Kingdom
4 h-index
8 publications
258 citations
Northern Arizona University
Flagstaff, United States
3 h-index
4 publications
148 citations
Roma Tre University
Rome, Italy
3 h-index
5 publications
169 citations
1–8 of 121
Venues
- Journal of Volcanology and Geothermal Research
22 publications · 789 citations
18
h-index
- Bulletin of Volcanology
11 publications · 371 citations
10
h-index
- Contributions to Mineralogy and Petrology
4 publications · 333 citations
4
h-index
- Journal of Geophysical Research Atmospheres
JGR · 4 publications · 330 citations
4
h-index
- Geological Magazine
4 publications · 122 citations
4
h-index
1–5