Despite the difference in size Martian and Hawaiian volcanoes have numerous characteristics in common. Specific features such as lava channels, collapsed lava tubes, levees and flow fronts, all very common in Hawaii, are also abundant on the flanks of some of the Martian volcanoes. Striking differences also exist, such as the apparent lack of radial rift zones on some Martian volcanoes and the paucity of cinder and spatter cones. Some of the best photographs of Martian and Hawaiian volcanic features are presented. Descriptive legends are provided for each picture. An overview of the geological processes and structures depicted is included
Extensive changes occurred after the initial observations (Greeley, 1971) of lava tube and channel f...
A ground examination is made of lave tubes and channels. The surface morphology and the changes note...
Puu Mahana has previously been interpreted to be a littoral cone, formed at a secondary rootless ve...
Surface features on the flanks of Martian shield volcanoes photographed by Mariner 9 are identified ...
This resource is part of a collection that compares the geology and weather of Earth and Mars. This ...
The long lava flows of Mauna Loa, Hawaii have been cited as Earth's closed analogs to the large Mart...
Martian volcanism is reviewed. It is emphasized that lava plains constitute the major type of effusi...
The territory of Hawaii consists of eight principal islands of a total area of about 6460 square mil...
Work in progress on Hawaiian drainage evolution indicates an important potential for understanding d...
Channels and valleys were known on the Martian volcanoes since their discovery by the Mariner 9 miss...
View of southeastern wall of Haleakala crater, East Maui, and one of the colourful cinder cones. Hal...
Kilauea volcano, 1250m (4090ft) is the youngest and most active of Hawaii's volcanoes. It can be stu...
Destructive, deadly, and able to uproot and ruin lives, yet awe inspiring and a supportive platform ...
We present a theoretical treatment of the ascent, emplacement, and eruption of magma on Mars. Becaus...
Lava tube and channel development in basalt flow in upper east rift zone of Kilauea volcano, Hawai
Extensive changes occurred after the initial observations (Greeley, 1971) of lava tube and channel f...
A ground examination is made of lave tubes and channels. The surface morphology and the changes note...
Puu Mahana has previously been interpreted to be a littoral cone, formed at a secondary rootless ve...
Surface features on the flanks of Martian shield volcanoes photographed by Mariner 9 are identified ...
This resource is part of a collection that compares the geology and weather of Earth and Mars. This ...
The long lava flows of Mauna Loa, Hawaii have been cited as Earth's closed analogs to the large Mart...
Martian volcanism is reviewed. It is emphasized that lava plains constitute the major type of effusi...
The territory of Hawaii consists of eight principal islands of a total area of about 6460 square mil...
Work in progress on Hawaiian drainage evolution indicates an important potential for understanding d...
Channels and valleys were known on the Martian volcanoes since their discovery by the Mariner 9 miss...
View of southeastern wall of Haleakala crater, East Maui, and one of the colourful cinder cones. Hal...
Kilauea volcano, 1250m (4090ft) is the youngest and most active of Hawaii's volcanoes. It can be stu...
Destructive, deadly, and able to uproot and ruin lives, yet awe inspiring and a supportive platform ...
We present a theoretical treatment of the ascent, emplacement, and eruption of magma on Mars. Becaus...
Lava tube and channel development in basalt flow in upper east rift zone of Kilauea volcano, Hawai
Extensive changes occurred after the initial observations (Greeley, 1971) of lava tube and channel f...
A ground examination is made of lave tubes and channels. The surface morphology and the changes note...
Puu Mahana has previously been interpreted to be a littoral cone, formed at a secondary rootless ve...