Monterey Bay Aquarium Research Institute

Volcanoes and Seamounts Logbook
Day 2: In hot water
April 22, 2012 • (Leer en Español)

As the remotely operated vehicle (ROV) descended into the blue depths above the Alarcón Rise, the control room was abuzz with anticipation, because today we were planning to dive on one of strangest environments in the deep sea: a hydrothermal vent field. Hydrothermal vents are regions where hot water is being expelled from the seafloor, giving rise to a rich community of organisms, many of which are not found in any other ocean ecosystem.

Along ocean spreading ridges, like the Alarcón Rise, the seafloor is cracked and faulted due to the high levels of tectonic activity in the region. Cool seawater seeps down through these cracks and is heated by the hot magma below the ridge. As the water is heated, it becomes buoyant and begins to rise back to the surface. During its ascent, the hot water leaches minerals from the Earth's crust. When the hot water exits the seafloor and comes in contact with the cold seawater, these minerals precipitate and over time can form tall chimneys and mounds composed of heavy metal sulfides. The sulfur in the vent water also provides the energy source required to support communities of vent life.

hydrothermal vent
Hydrothermal vent along the Alarcón Rise.

Hydrothermal vents have been documented to the south of our location at 21° north and to the north at Guaymas (located at 27° north), however, vents had not yet been discovered along Alarcón Rise. In fact, very few studies have focused on the Alarcón Rise, and our dive was the first to explore this section of the ridge. Now, you may be wondering, if we’ve never explored this area before, how did we know where to dive to find hydrothermal chimneys? Based on the geology of the region, we knew that there was a high probability that Alarcón Rise would have active hydrothermal vents. However, exploring the entire ridge using the ROV to search for vents would be virtually impossible and incredibly time consuming. Instead, we sent our autonomous underwater vehicle (AUV) to map the region before we arrived. AUV surveys collected one-meter-resolution bathymetry data for the entire ridge segment, and based on these high-resolution maps it was possible to identify features that appeared to be chimneys.

Once the ROV reached the seafloor we headed toward one of the chimney sites identified by the AUV map. As we got closer, we knew that we were heading in the right direction; a thriving community of vent animals spread out before us. Some of the most distinctive animals include the large red tube worms, Riftia sp., that live in clumps around hot-water vents.

tube worms
Tube worm, Riftia sp., communities at hot-water vent sites.
An army of squat lobsters advances over the top of a mound of old tube worm casings.

Since vent communities have never before been observed on this section of the ridge, we stopped to take some samples. A genetic analysis of the animals collected here will be conducted and these genetic markers will be compared to those from other vent sites, specifically vents located at 21° north and Guaymas. These genetic analyses will provide a better understanding of the distribution of vent species along the East Pacific ridge system.

ROV collecting clam
The ROV’s manipulator arm collecting a clam from an active vent site.

After sampling, we continued toward the tall chimney structures identified on our map and, just as predicted, we found several tall chimneys, some active and some inactive. We were able to verify that the chimney heights were also accurately mapped with the AUV. Finding the vents was very encouraging, as it suggested that we could successfully identify hydrothermal chimneys from our AUV map data. Now, without diving on every single vent field, we will be able to determine the distribution of vents along the ridge, infer the distribution of vent communities, and estimate the volume of the sulfide deposits using the AUV maps.

This is the top of the largest chimney we found today. It rises more than 20 meters (65 feet) from the seafloor. While the top does not look very active, there is a thriving community of Riftia at the base.

The active chimneys were spewing large quantities of black smoke, and are thus referred to as black smokers. However, the smoke is not really smoke at all, but rather the heavy-metal sulfides precipitating from the hot vent water as it rapidly cools. Black smokers are some of the hottest hydrothermal vents, with water temperatures greater than 300 degrees Celsius (572 degrees Fahrenheit). We recorded temperatures of more than 250 degrees Celsius (480 degrees Fahrenheit), but this should be viewed as a minimum fluid temperature as it is very difficult to get the temperature probe directly into the stream of hot water. Characterizing the temperature at a specific vent field can be very useful; different minerals will precipitate from vent waters of different temperatures. Additionally, the populations of vent species will vary with temperature.

tube worms with fish
A close-up view of the vent tube worms (Riftia). If you look closely you’ll see several fish hiding in among the worms. The little black spots covering the worm casings are limpets.

After we had thoroughly explored the vent field, we traversed over the northern edge of a very large lava sheet flow. We spent the rest of the dive collecting lava samples to characterize the nature of the volcanism in this area. Stay tuned, because tomorrow we will dive on the southern end of this sheet flow, and we will begin to piece together a more comprehensive picture of the volcanism of the region.

—Julie Martin

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Volcanoes & Seamounts

R/V Western Flyer

The R/V Western Flyer is a small water-plane area twin hull (SWATH) oceanographic research vessel measuring 35.6 meters long and 16.2 meters wide. It was designed and constructed for MBARI to serve as the support vessel for ROV operations. Her missions include the Monterey Bay as well as extended cruises to Hawaii, Gulf of California and the Pacific Northwest.

ROV Doc Ricketts

ROV Doc Ricketts is MBARI's next generation ROV. The system breaks new ground in providing an integrated unmanned submersible research platform, with many powerful features providing efficient, reliable and precise sampling and data collection in a wide range of missions.

Push cores

A push-core looks like a clear plastic tube with a rubber handle on one end. Just as its name implies, the push core is pushed down into loose sediment using the ROV's manipulator arm. As the sediment fills up the core, water exits out the top through one-way valves. When the core is pulled up again, these valves close, which (most of the time) keeps the sediment from sliding out of the core tube. When we bring these cores back to the surface, we typically look for living animals and organic material in the sediments.

Niskin bottles

Niskin bottles are used to collect water samples as well as the tiny bacteria and plankton in that volume. The caps at both ends are open until the bottles are tripped, when the caps snap closed.


The box fits in a partition in the sample drawer. It is shown open, with an animal being placed into it by the ROV's manipulator. When the lid is closed, the box will hold water to protect the animals inside.

Rock crusher

This device is used to collect volcanic glass fragments from the surface of a flow. It is made of about 450kg of lead and steel and is launched over the stern of the ship on a wire. Fragments of rock that break off of the lava flow on impact are trapped in wax-tipped cones mounted around the crusher. The wax is melted in the lab to liberate the rock particles for analysis.

Benthic toolsled

The benthic toolsled is attached to the bottom of the ROV for our geology dives. Its components are the manipulator arm and the sample drawer. The sample drawer is shown open on deck, full of rocks. Normally it is closed when the vehicle is operating and is opened only when a sample needs to be stowed. Partitions in the drawer help us keep the rocks in order. The rocks often look alike, but the conditions and chemistries of the eruptions are different so it is important that we know where each came from.

Glass suction sampler

This equipment is used to vacuum glass particles and larval animals from cracks and crevices. The carousel of small plastic jars fitted with wire mesh will be mounted in the benthic toolsled. The hose will be held by the ROV's manipulator and a suction will be drawn by the pump.

Sediment scoops

Canvas bags on a T-handle for collecting gravel or other materials that fall out of a push-core.

Temperature probe

Held by the ROV's manipulator, the wire on the right is placed into the fluid emitted from a hydrothermal vent to record the temperature.


Vibracoring is a common technique used to obtain samples from water-saturated sediment. These corers work by attaching a motor that induces high frequency vibrations in the core liner that in turn liquefies the sediment directly around the core cutter, enabling it to pass through the sediment with little resistance.


R/V Western Flyer

Ian Young


George Gunther
First Mate


Matt Noyes
Chief Engineer


Andrew McKee
Second Mate


Lance Wardle
First Engineer


Shaun Summer
Relief First Engineer


Olin Jordan


Craig Heihn
Relief Deckhand


Jason Jordan
Relief Deckhand


Dan Chamberlain
Electronics Officer


Patrick Mitts


ROV Doc Ricketts

Knute Brekke
Chief ROV Pilot


Mark Talkovic
Senior ROV Pilot


Randy Prickett
Senior ROV Pilot


Bryan Schaefer
ROV Pilot/Technician


Eric Martin
ROV Pilot/Technician


 Research Team

Dave Clague
Chief Scientist

Dave's research interests are nearly all related to the formation and degradation of oceanic volcanoes, particularly Hawaiian volcanoes, mid-ocean ridges, and isolated seamounts. Topics of interest include: compositions of mantle sources for basaltic magmas and conditions of melting; volatile and rare-gas components in basaltic magmas and their degassing history; chronostratigraphic studies of eruption sequence and evolution of lava chemistry during volcano growth; subsidence of ocean volcanoes and its related crustal flexure, plate deformation, and magmatic activity; geologic setting of hydrothermal activity; origin of isolated seamounts; and monitoring of magmatic, tectonic, and hydrothermal activity at submarine and subaerial volcanoes.

Jenny Paduan
Research Specialist

Jenny works with Dave Clague in the submarine volcanism project, processing the high-resolution MBARI mapping AUV data and interpreting the maps using ROV observations and samples from our research sites. On this cruise, she will stand watches in the ROV control room, help with rock and sediment sample workup and curation once the vehicle is on deck, and coordinate these cruise logs. She is now quite solidly a marine geologist, but her degrees are in biochemistry (Smith College) and biological oceanography (Oregon State University). She is thankful for the opportunities that have led her to study volcanoes, and loves being involved with the research and going to sea. She looks forward to discovering more about how Earth works.

Lonny Lundsten
Senior Research Technician

On this cruise, Lonny will be in charge of biological sample collection and processing and video data management. This work entails identifying unique biological and geological features that will be seen during the dive, while using MBARI-designed software to log the observations. He is especially excited about this expedition, because no one has surveyed this particular seamount before, and he expects to find many new species on this cruise.

Julie Martin
Senior Research Technician

Julie works with the submarine volcanism group, where she currently produces high resolution maps of the seafloor that are used to identify geologic features along submarine ridges and seamounts. Her research interests also include modeling of volcanic ash from sub-aerial, large-scale explosive eruptions.

Ryan Portner
Postdoctoral Fellow

Ryan's work with the submarine volcanism project primarily focuses on the formation and distribution of volcaniclastic deposits on active and extinct seamounts and mid-ocean ridges. By categorizing the diversity in these deposits with respect to volcanic landforms he hopes to better understand the underlying controls on explosive vs. non-explosive deep marine eruptions. His background research on deep-marine gravity flow deposits preserved in sedimentary-volcanic successions exposed on land lends a comparable platform to study similar deposits of the modern oceans.

Julie Bowles

Julie is a Research Associate and Staff Scientist with the Institute for Rock Magnetism at the University of Minnesota. As a paleomagnetist, Julie studies variations in Earth's magnetic field and how those variations get recorded in rocks and sediments. One of Julie's particular interests involves using paleofield variations recorded in mid-ocean ridge lava flows to place age constraints on the flows. On this expedition, Julie is interested both in using this technique to try to date some of the young lava flows and in gaining a better understanding of how the Earth's field has varied in this particular location.

Paterno Castillo

Pat is a Professor of Geology at the Scripps Institution of Oceanography, University of California, San Diego. His research interests include petrology and geochemistry of magmas produced within and along divergent and convergent boundaries of tectonic plates, magmatic and tectonic evolution of continental margins and mantle geodynamics. On this expedition, Pat is interested in the petrologic and tectonic evolution of the newly formed oceanic basement in the Gulf of California.

Brian Dreyer
Isotope Geologist
UC Santa Cruz
Institute of Marine Sciences

Brian studies the recent magmagenesis and petrology of the Juan de Fuca Ridge. His interest in mid-ocean ridges began during his postdoctoral fellowship with MBARI's submarine volcanism project; there, he utilized uranium-series disequilibria within individual lavas of Axial Seamount to clarify eruption and petrogenetic timescales. At mid-ocean ridge systems globally, Brian is interested in a) how variability in lava morphology, geochemistry, and petrology reflect deeper mantle-melting and magmatic processes and their complex interplay with tectonism and b) improving the chronological framework of the ridge magmatic plumbing systems. Brian received his Ph.D. in Earth and Planetary Science from Washington University in St. Louis in 2007.

Rigoberto Guardado
Universidad Autónoma de Baja California

Rigoberto Guardado is a teacher and research scientist with the Facultad de Ciencias Marinas (Marine Sciences Faculty) at the University of Baja California in Mexico. As a oceanographer, Rigoberto studies sedimentation processes in the ocean. On this expedition, Rigoberto is interested in learning more about the sediments in this area of the Gulf of California.

Ronald Michael Spelz Madero

Ronald Spelz earned his Ph.D. in earth sciences from Centro de Investigación Científica y de Educación Superior de Ensenada (CICESE) in 2008. His research interests are mainly focused in the structural geology and tectonic geomorphology of fault bounded basins and mountain range-fronts in northern Baja California. He is also part of the multidisciplinary research team studying the origin and effects of the El Mayor-Cucapah 7.2 magnitude earthquake which struck northern Baja in April 4, 2010. Ronald presently works in the Marine Sciences Faculty at the Universidad Autónoma de Baja California.

Hiram Rivera
Universidad Autónoma de Baja California

Hiram Rivera is part of the Coastal Management group and teacher in the Faculty of Marine Science at Universidad Autónoma de Baja California. Since 2008 he has worked as a technician with geographic information systems (GIS) applied to fisheries resource management. From 2010 to now he has worked with his students in public participation geographic information systems (PPGIS) 3D models applied to the use of GIS to broaden public involvement in policymaking. His interest for this cruise is to learn about the techniques associated with digital cartography of the Gulf of California.

Last updated: Apr. 26, 2012