Image Archive

Most of the Leg 1 science party. (photo by Allison Fundis) 

Chuck McGuire plays a few tunes during Bosun's poetry night. (photo by Allison Fundis) 

John reads Hughes during Bosun's poetry night. (photo by Allison Fundis) 

Thompson crew member, Dana Africa, and Dean Lisa Graumlich knit while they listen during Bosun's poetry night. (photo by Allison Fundis)

Chris Holm plays an Eddie Vedder song during Bosun's poetry night. (photo by Allison Fundis) 

Alden Denny reads a limerick during Bosun's poetry night. Lexi Brewer, Debbie Kelley, and Kendra Daly listen. (photo by Allison Fundis) 

Mike Harrington reads Billy Collins during Bosun's poetry night. (photo by Allison Fundis) 

Sue Banahan reads a Pablo Neruda poem during Bosun's poetry night. 

Captain John Wilson reads a poem at Bosun's poetry night. (Photo by Allison Fundis) 

Jim (the Thompson's lead engineer), Allison Fundis, and Alden Denny enjoy a little down time. (photo by Captain John Wilson) 

A little down time in the sun during a fantail BBQ. (photo by Allison Fundis)

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A collapse pond forms from the draining of pooled molten lava after a solid roof has formed over a lava pond. The weight of the unsupported roof may cause it to collapse. Pillars form where water rises from beneath a flow creating pillars of crystallized magma from within the deepening lava pools.

Skip Denny and Dana Manalang log events during their 4 hour watch in the ROPOS control room. Mitch Elend and Monica Riess (back) work to stich together images into a photomosaic as they come in from the digital still camera mounted on the ROV. (photo by Allison Fundis) 

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Josh Chernoy and Vincent Auger of the ROPOS crew secure the USBL pole that is used to navigate the ROV. (photo by Allison Fundis)

Lineated sheet flows form when molten lava flows out from underneath the edge of a solidified crust. The lineations are a result of the crust scraping against the surface of the moving molten lava.

Jumbled sheet flows form when the solidifying surface of the lava begins to fold under compression from the flow behind it.

Hackly sheet flows form when the solidifying surface of the fast moving lava experiences so much deformation that the solidified surface begins to break apart and piles up on itself. The edges are very rough and sharp.

tubeworms from ENLIGHTEN '10

Lobate flows form from low effusivity flows. (more..)

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Pillow lavas (also called pillow basalts) result from the quenching - or very rapid cooling and crystallization - of the outer portion of a small extrusion of lava. Continued extrusion breaks through one pillow and forms a new adjacent pillow. Striations may occur from the lava being scraped by the rough edges at the point of fracture and extrusion.

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