Recent HiRISE images from Mars have shown 10-25m coils in channelized lava flows at Athabasca Valles. The definitive reason for their formation is not fully understood, but it is thought to be a result of primary volcanic processes. While Craters of the Moon National Monument and Preserve has long been considered an excellent analog for Martian volcanism, there is no record in the literature of similar lava coils having been observed there. Based on contextual morphology, we identified and searched potential lava coil zones using imagery in Google Earth and Google Maps. Of the twenty-five lava channels searched, twelve showed possible lava coils. The coils ranged from 1 to 7 meters in diameter and tended to be located in the center portions...
The lava flows of Craters of the Moon National Park have received a great deal of scrutiny because o...
Surface features on the flanks of Martian shield volcanoes photographed by Mariner 9 are identified ...
In order to investigate sources of lava and water to the Cerberus plains of Mars, geomorphological m...
Sinuous collapse chains and skylights in lunar and Martian volcanic regions have often been interpre...
Abstract: Lava tubes form when narrow lava channels crust over, build levees which arch over the cha...
The Late Amazonian volcanic plains east of Olympus Mons contain numerous channels and fossae. Channe...
Kilometre-sized flows (KSFs) have been observed in many regions on Mars and have been typically inte...
The surface morphology of a lava flow results from processes that take place during the emplacement ...
Kilometre-sized flows (KSFs) have been observed in many regions on Mars and have been typically inte...
Investigating recent eruptions on Earth is crucial to improving understanding of relationships betwe...
Lava tubes have the potential to serve as a sustainable solution to long-term lunar habitation by pr...
Lava tubes have the potential to serve as a sustainable solution to long-term lunar habitation by pr...
We have used new compositional information on Martian basaltic rocks from the Mars Exploration Rover...
Lava caves could be useful as outposts for the human exploration of the Moon. Lava caves or lava tub...
The Tharsis Montes rift aprons are composed of outpourings of lava from chaotic terrains to the nort...
The lava flows of Craters of the Moon National Park have received a great deal of scrutiny because o...
Surface features on the flanks of Martian shield volcanoes photographed by Mariner 9 are identified ...
In order to investigate sources of lava and water to the Cerberus plains of Mars, geomorphological m...
Sinuous collapse chains and skylights in lunar and Martian volcanic regions have often been interpre...
Abstract: Lava tubes form when narrow lava channels crust over, build levees which arch over the cha...
The Late Amazonian volcanic plains east of Olympus Mons contain numerous channels and fossae. Channe...
Kilometre-sized flows (KSFs) have been observed in many regions on Mars and have been typically inte...
The surface morphology of a lava flow results from processes that take place during the emplacement ...
Kilometre-sized flows (KSFs) have been observed in many regions on Mars and have been typically inte...
Investigating recent eruptions on Earth is crucial to improving understanding of relationships betwe...
Lava tubes have the potential to serve as a sustainable solution to long-term lunar habitation by pr...
Lava tubes have the potential to serve as a sustainable solution to long-term lunar habitation by pr...
We have used new compositional information on Martian basaltic rocks from the Mars Exploration Rover...
Lava caves could be useful as outposts for the human exploration of the Moon. Lava caves or lava tub...
The Tharsis Montes rift aprons are composed of outpourings of lava from chaotic terrains to the nort...
The lava flows of Craters of the Moon National Park have received a great deal of scrutiny because o...
Surface features on the flanks of Martian shield volcanoes photographed by Mariner 9 are identified ...
In order to investigate sources of lava and water to the Cerberus plains of Mars, geomorphological m...