Expedition goal: During this 10-day expedition, MBARI researchers will join geologists from the National and Kapodistrian University of Athens (NKUA) to study underwater hydrothermal seeps around Milos, Greece. The team will deploy a distributed acoustic sensing (DAS) system to detect and characterize hydrothermal activity and use the MOLA AUV—a portable underwater robot developed by MBARI’s CoMPAS Lab—to map seafloor features in high resolution. Together, these platforms will help the team better understand how hydrothermal activity at a dormant underwater volcano shapes seafloor geology and ecology.

Expedition dates: October 15–25, 2026

Location: Paleochori Bay, Milos, Greece

Research technology: Bubble Cam stereo-imaging system, distributed acoustic sensing (DAS), hydrophone, MOLA AUV

The Greek island of Milos is located in the South Aegean Volcanic Arc, a tectonically and volcanically active region shaped by the subduction of the African Plate beneath the Eurasian Plate. Created by volcanic activity more than 2 million years ago, Milos hosts one of the largest known shallow-water underwater geothermal systems in the world. Vast fields of gas and fluid vents are easily accessible in shallow waters around the island. Extensive venting has been documented across the Paleochori shelf and slope—from the shoreline to depths beyond 500 meters (1,640 feet)—often associated with bacterial mats and mineral deposits. These vents release carbon dioxide gas, hydrothermal fluids, and trace elements that play a significant role in shaping seafloor geology and ecology.

MBARI’s CoMPAS Lab develops scalable marine technology that can be easily modified for use across a wide variety of vehicles and platforms. Led by Principal Engineer Giancarlo Troni, this team works to make MBARI’s innovations more broadly accessible to our peers, helping advance ocean exploration.

MBARI’s Seafloor Processes Team is filling critical gaps in our understanding of the processes that sculpt the seafloor. Led by Senior Scientist Aaron Micallef, this team uses advanced technology at sites around the globe to study seafloor geology and answer fundamental questions about how the seafloor evolves and functions.

Together with marine geologist Paraskevi (Evi) Nomikou from the National and Kapodistrian University of Athens (NKUA), these teams will use innovative technologies developed by MBARI engineers to study hydrothermal activity around Milos.

An engineer wearing a hard hat and life vest stands on a yellow fiberglass walkway above a large tank of water, inspecting a portable underwater robot suspended from a crane out of frame.
Led by Principal Engineer Giancarlo Troni (pictured), MBARI’s CoMPAS Lab develops scalable robotic technologies, like the portable MOLA AUV. Image: Lori Eanes © Monterey Bay Aquarium

The MOLA AUV—multimodality, observing, low-cost, agile autonomous underwater vehicle—is a portable, but powerful, autonomous robot for ocean exploration. Equipped with sensors and algorithms for high-resolution navigation, imaging, and mapping, the MOLA AUV is ideal for operating in shallow coastal waters around Paleochori Bay and Spathi Bay, where access is limited to small boats or shore deployment. The vehicle’s compact size and vectorized thrusters configuration enable precise control over all six degrees of freedom—forward, lateral, heave, roll, pitch, and yaw—allowing it to navigate rugged underwater terrain with ease.

Using data collected from the vehicle’s forward-looking sonar, stereo cameras, and laser scanner, the CoMPAS Lab will generate detailed maps and 3D photogrammetry reconstructions that geologists can use to characterize vent features, especially bacterial mats and mineral precipitates that are key indicators of hydrothermal outflows. 

The team will first create accurate maps of areas of interest based on NKUA collaborator Paraskevi Nomikou’s earlier work on the shallow-marine hydrothermal fields of Paleochori Bay. Then, conditions permitting, they plan to extend mapping efforts to deeper hydrothermal vents in Spathi Bay, which have not previously been surveyed or studied in detail due to their depth.

The fieldwork in Milos is an important opportunity to validate recent advances in autonomous navigation, control, perception, and mapping in real-world environments, while collecting new field data for continued algorithm and system development. Together, these deployments underscore the CoMPAS Lab’s strategy of rapidly moving technologies from development to field validation and applying scalable marine robotics to challenging scientific problems.

Two scientists inspect a roll of thin yellow fiber-optic cable on a large black plastic spool on the counter inside a brightly lit scientific lab.
Led by Senior Scientist Aaron Micallef (left), MBARI’s Seafloor Processes Team uses innovative technologies, like distributed acoustic sensing, to study underwater geological processes. Image: Rose Dalrymple © 2026 MBARI

Distributed acoustic sensing (DAS) uses fiber-optic cables as dense sensor arrays. By measuring the phase changes in laser light along the cable, scientists can detect disturbances on the seafloor, including earthquakes, underwater landslides, and fluid seepage. These processes can be relatively small-scale, yet they play a major role in shaping the seafloor.

MBARI’s Seafloor Processes Team has developed Geo-Sense, a portable DAS system that can be deployed wherever there is a seafloor process of interest. The team has adapted Geo-Sense components into a portable travel case to test the effectiveness of DAS technology for detecting and quantifying hydrothermal venting.

The DAS system will be installed onshore in Paleochori Bay, monitoring backscatter along a cable running 700 meters (approximately 2,300 feet) offshore to a depth of 15 meters (49 feet). The team will work with local divers to strategically place the cable near active vents to detect acoustic signals associated with bubble emissions from hydrothermal vents and estimate their seepage rates. These signals are expected to vary across different areas of the bay, potentially reflecting differences in bubble size and nucleation processes. The temporal distribution of these acoustic events will offer insight into evolving gas seepage patterns and may reveal correlations with environmental or volcanic activity. 

The team will deploy hydrophones and cameras near the cable to collect complementary data about the release of gases from the seafloor. The hydrophones are underwater microphones that record the high-frequency sound of gas bubbles percolating from the seafloor, while the Bubble Cam is a new stereo-imaging system developed by MBARI engineers to quantify gas seepage. Data from both instruments will provide context for reviewing acoustic signals recorded by the DAS system.