A rootless cone , also formerly called a pseudocrater , [1] is a volcanic landform which resembles a true volcanic crater , but differs in that it is not an actual vent from which lava has erupted. They are characterised by the absence of any magma conduit which connects below the surface of a planet.
Year | Metadata | Sections | Top Words | First Paragraph |
2018 |
52230 characters 4 sections 12 paragraphs 16 images 227 internal links 7 external links |
cones 0.503 rootless 0.488 lava 0.273 cone 0.219 steam 0.175 hiwish 0.130 kink 0.125 173 0.125 197 0.124 blows 0.122 807 0.118 ice 0.117 rings 0.112 965 0.108 760 0.096 |
A rootless cone , also formerly called a pseudocrater , [1] is a volcanic landform which resembles a true volcanic crater , but differs in that it is not an actual vent from which lava has erupted. They are characterised by the absence of any magma conduit which connects below the surface of a planet. |
|
2017 |
52047 characters 4 sections 12 paragraphs 16 images 227 internal links 7 external links |
cones 0.506 rootless 0.492 lava 0.274 cone 0.221 steam 0.176 hiwish 0.131 kink 0.126 173 0.126 197 0.124 blows 0.123 807 0.118 ice 0.118 rings 0.112 965 0.108 760 0.097 |
A rootless cone , also formerly called a pseudocrater , [1] is a volcanic landform which resembles a true volcanic crater , but differs in that it is not an actual vent from which lava has erupted. They are characterised by the absence of any magma conduit which connects below the surface of a planet. |
|
2016 |
43208 characters 4 sections 12 paragraphs 14 images 173 internal links 7 external links |
cones 0.506 rootless 0.492 lava 0.274 cone 0.221 steam 0.176 hiwish 0.131 kink 0.126 173 0.126 197 0.124 blows 0.123 807 0.118 ice 0.118 rings 0.112 965 0.108 760 0.097 |
A rootless cone , also formerly called a pseudocrater , [1] is a volcanic landform which resembles a true volcanic crater , but differs in that it is not an actual vent from which lava has erupted. They are characterised by the absence of any magma conduit which connects below the surface of a planet. |
|
2015 |
40569 characters 4 sections 9 paragraphs 11 images 171 internal links 7 external links |
rootless 0.458 cones 0.453 lava 0.286 cone 0.251 steam 0.201 kink 0.144 173 0.144 197 0.142 blows 0.140 807 0.135 rings 0.128 965 0.123 ice 0.121 760 0.110 910 0.106 |
A rootless cone , also formerly called a pseudocrater , [1] is a volcanic landform which resembles a true volcanic crater , but differs in that it is not an actual vent from which lava has erupted. They are characterised by the absence of any magma conduit which connects below the surface of a planet. |
|
2014 |
37472 characters 4 sections 6 paragraphs 8 images 171 internal links 7 external links |
rootless 0.472 cones 0.254 173 0.222 197 0.219 807 0.208 lava 0.201 965 0.191 760 0.170 910 0.163 iceland 0.141 eruption 0.131 cone 0.130 steam 0.124 landbrotshólar 0.123 rauðhólar 0.123 |
A rootless cone , former also called pseudocrater , [1] is a volcanic landform which resembles a true volcanic crater , but differs in that it is not an actual vent from which lava has erupted. They are characterised by the absence of any magma conduit which connects below the surface of a planet. |
|
2013 |
33970 characters 4 sections 6 paragraphs 8 images 169 internal links 5 external links |
pseudocraters 0.377 rootless 0.241 pseudocrater 0.227 173 0.227 197 0.224 807 0.212 lava 0.205 cones 0.195 965 0.194 760 0.174 910 0.166 iceland 0.144 eruption 0.133 steam 0.126 landbrotshólar 0.126 |
A pseudocrater is a volcanic landform which resembles a true volcanic crater , but differs in that it is not an actual vent from which lava has erupted. Pseudocraters are also known as rootless cones , since they are characterised by the absence of any magma conduit which connects below the surface of the earth. |
|
2011 |
8049 characters 3 sections 5 paragraphs 3 images 23 internal links 2 external links |
pseudocraters 0.492 pseudocrater 0.296 lava 0.214 iceland 0.187 eruption 0.174 steam 0.165 landbrotshólar 0.164 rauðhólar 0.164 skútustaðagígar 0.164 eyjafjallajökull 0.148 reykjavík 0.148 mývatn 0.138 superheated 0.138 volcanologists 0.138 phreatic 0.132 |
A pseudocrater is a volcanic landform which resembles a true volcanic crater , but differs in that it is not an actual vent from which lava has erupted. Pseudocraters are also known as rootless cones , since they are characterised by the absence of any magma conduit which connects below the surface of the earth. |
|
2010 |
8049 characters 3 sections 5 paragraphs 3 images 23 internal links 2 external links |
pseudocraters 0.492 pseudocrater 0.296 lava 0.214 iceland 0.187 eruption 0.174 steam 0.165 landbrotshólar 0.164 rauðhólar 0.164 skútustaðagígar 0.164 eyjafjallajökull 0.148 reykjavík 0.148 mývatn 0.138 superheated 0.138 volcanologists 0.138 phreatic 0.132 |
A pseudocrater is a volcanic landform which resembles a true volcanic crater , but differs in that it is not an actual vent from which lava has erupted. Pseudocraters are also known as rootless cones , since they are characterised by the absence of any magma conduit which connects below the surface of the earth. |
|
2009 |
5216 characters 2 sections 3 paragraphs 2 images 17 internal links 1 external links |
pseudocraters 0.565 iceland 0.215 landbrotshólar 0.188 rauðhólar 0.188 skútustaðagígar 0.188 lava 0.185 pseudocrater 0.170 reykjavík 0.170 mývatn 0.159 phreatic 0.152 swamp 0.152 conduit 0.146 characterised 0.137 tephra 0.137 pond 0.133 |
A pseudocrater is a volcanic landform which resembles a true volcanic crater , but differs in that it is not an actual vent from which lava has erupted. Pseudocraters are also known as rootless cones , since they are characterised by the absence of any magma conduit which connects below the surface of the earth. |
|
2008 |
5090 characters 2 sections 3 paragraphs 2 images 15 internal links 1 external links |
pseudocraters 0.565 iceland 0.215 landbrotshólar 0.188 rauðhólar 0.188 skútustaðagígar 0.188 lava 0.185 pseudocrater 0.170 reykjavík 0.170 mývatn 0.159 phreatic 0.152 swamp 0.152 conduit 0.146 characterised 0.137 tephra 0.137 pond 0.133 |
A pseudocrater is a volcanic landform which resembles a true volcanic crater , but differs in that it is not an actual vent from which lava has erupted. Pseudocraters are also known as rootless cones , since they are characterised by the absence of any magma conduit which connects below the surface of the earth. |
|
2007 |
4017 characters 2 sections 3 paragraphs 1 images 15 internal links 1 external links |
pseudocraters 0.576 iceland 0.219 landbrotshólar 0.192 rauðhólar 0.192 lava 0.188 pseudocrater 0.173 reykjavík 0.173 mývatn 0.162 phreatic 0.154 swamp 0.154 conduit 0.148 characterised 0.139 tephra 0.139 pond 0.136 volcanic 0.134 |
A pseudocrater is a volcanic landform which resembles a true volcanic crater , but differs in that it is not an actual vent from which lava has erupted. Pseudocraters are also known as rootless cones , since they are characterised by the absence of any magma conduit which connects below the surface of the earth. |
|
2006 |
3725 characters 2 sections 4 paragraphs 1 images 12 internal links 1 external links |
iceland 0.286 landbrotshólar 0.250 rauðhólar 0.250 pseudocraters 0.250 pseudocrater 0.226 reykjavík 0.226 mývatn 0.212 phreatic 0.201 swamp 0.201 characterised 0.182 tephra 0.182 pond 0.177 lava 0.164 builds 0.163 rootless 0.160 |
When hot lava is running over a wet surface, whether a swamp , a lake, or a pond, the event produces explosive gases. These break through the lava surface in an explosion (a phreatic eruption ), and the tephra builds up crater-like forms which can be very similar to real volcanic craters . These forms are also called rootless cones . They are characterised by not having a root, a magma channel which would connect them to the inner core of the earth. |
|
2005 |
1910 characters 0 sections 2 paragraphs 1 images 4 internal links 0 external links |
pseudocrater 0.519 template 0.486 phreatic 0.463 eruption 0.305 wet 0.252 lava 0.188 flows 0.167 volcanic 0.133 created 0.129 formation 0.118 ground 0.109 |
A pseudocrater is a volcanic formation created by a phreatic eruption , when lava flows over wet ground. |