More Kilauea

Episode 19 of the ongoing Kilauea event began last night in Hawai'i. The image is from this morning (note the time stamp in the upper left (local HST). This is the same time as 7:20 AZ time. You can always view the Kilauea live web cam at this link. Bookmark it!

Kilauea Eruptions in Halema'uma'u Crater

Screen capture from about 1:30 PM Hawaiian local time on April 1, 2025

 If you have not been watching the live WebCam from the Kilauea volcano, check it out here. Spectacular fountaining going on.

HAWAIIAN VOLCANO OBSERVATORY STATUS REPORT
U.S. Geological Survey
Tuesday, April 1, 2025, 11:22 AM HST (Tuesday, April 1, 2025, 21:22 UTC)

KILAUEA (VNUM #332010)
19°25'16" N 155°17'13" W, Summit Elevation 4091 ft (1247 m)
Current Volcano Alert Level: WATCH
Current Aviation Color Code: ORANGE

Activity Summary: 

The high fountain phase of episode 16 of the ongoing Halemaʻumaʻu eruption began at 10:24 a.m. HST on April 1, 2025, about 12 hours after the start of the episode. Fountaining from the south vent rapidly increased to over 200 feet (70 meters) in height by 10:40 a.m. HST and exceeded 700 feet (215 m) by 10:50 a.m. HST. Low dome fountaining and overflows continue from the north vent. 

Episode 16 was preceded by weak spattering in the north vent that began at approximately 5:20 p.m. HST on March 31, 2025. Since 6:00 p.m. HST, spattering became continuous and increased to low fountaining (15-30 feet or 5-10 meters high). Lava level gradually rose in the vent and began overflowing out of the north vent cone onto the floor of Halemaʻumaʻu at 10:57 p.m. HST on March 31. 

At south vent, small spatter fountains were first observed by field crews at 8:30 a.m. HST on April 1, but they probably were active deeper in the vent prior to that time. The south vent became more active at 10:12 a.m. HST on April 1 and began producing significant lava flows. Fountains in this episode are likely to exceed 1000 feet (300 meters) similar to episode 15.  More details about the start of episode 16 can be found in the Kīlauea Daily Update.

Inflationary tilt on the UWD tiltmeter reached around 8 microradians since the end of the last episode, recovering about 90% of the tilt lost from episode 15. UWD tilt began to deflate and seismic tremor greatly increase at same time high fountaining began. Seismic tremor initially began increasing around noon HST on March 31, 2025, followed by a sharper increase around 4:30 p.m. HST the same afternoon. Tremor and infrasound signals continued to steadily increase until rapidly increasing with the onset of high fountains. 

Emissions of SO2 gas are elevated, and during recent episodes have reached 50,000 tonnes per day or more, and similar amounts of gas are expected to accompany any high fountaining activity that may occur during episode 16. Currently, winds at the summit are forecast to be weak, which may allow the plume of gas to spread around the summit region of Kīlauea. In addition, visitors to Hawaiʻi Volcanoes National Park and residents of adjacent areas may be exposed to Peleʻs hair and other small fragments of volcanic glass and tephra being carried in the plume, as they were during episode 15.

Each episode of Halemaʻumaʻu lava fountaining since December 23, 2024, has continued for 13 hours to 8 days, and episodes have been separated by pauses in eruptive activity lasting less than 24 hours to 12 days. 

• Timeline of eruption episodes since December 23, 2024: https://www.usgs.gov/volcanoes/kilauea/science/eruption-information 
• Two Kīlauea summit livestream videos are available here: Kīlauea Volcano, Hawaii (West Halemaʻumaʻu crater) v1cam and Kīlauea Volcano, Hawaii (East Halemaʻumaʻu crater)v2cam

No changes have been detected in the East Rift Zone or Southwest Rift Zone. HVO continues to closely monitor Kīlauea and will issue an eruption update tomorrow morning unless there are significant changes before then. 

Kīlauea Volcano Alert Level/Aviation Color Code remain at WATCH/ORANGE. All current and recent activity is within Hawaiʻi Volcanoes National Park.

Hazards: 

This episodic eruption is occurring within a closed area of Hawai'i Volcanoes National Park. High levels of volcanic gas—primarily water vapor (H₂O), carbon dioxide (CO₂), and sulfur dioxide (SO₂)—are the primary hazard of concern, as this hazard can have far-reaching effects downwind. As SO₂ is continuously released from the summit during an eruption, it will react in the atmosphere to create the visible haze known as vog (volcanic smog) downwind of Kīlauea. SO₂ and vog may cause respiratory and other problems at high concentrations. Further information on vog can be found at https://vog.ivhhn.org/

Additional hazards include Pele's hair and other volcanic fragments from lava fountains. Pele's hair is strands of volcanic glass often produced by lava fountaining activity. Volcanic fragments can fall on the ground within a few hundred yards (meters) of the eruptive vent(s), or downwind of the vent(s). Strong winds may waft light particles, including Pele's hair, to greater distances downwind. Once they are on the ground, Pele's hair can sometimes cluster and tangle together, giving it the appearance of a tumbleweed. The extent of Pele's hair deposition is dependent on lava fountaining activity and current wind conditions. Residents and visitors should minimize exposure to Pele's hair and other volcanic fragments, which can cause skin and eye irritation. More information about how Pele's hair, its hazards, and what to do is available here: https://www.usgs.gov/observatories/hvo/news/volcano-watch-recent-lava-fountains-highlight-peles-hair-hazards. A Frequently Asked Questions document developed for the 2022 Mauna Loa eruption includes information about potential health effects of Pele's hair and is available here: https://vog.ivhhn.org/sites/default/files/FAQ_on_air_quality_and_health_during_Mauna_Loa_eruption_v1.6.pdf

Hawaiian lava flows generally advance slowly downslope, and during this eruption flows have been confined to Halemaʻumaʻu crater and the southwest side of Kaluapele, Kīlauea's summit caldera. 

Other significant hazards also remain around Kīlauea caldera from Halemaʻumaʻu crater wall instability, ground cracking, and rockfalls that can be enhanced by earthquakes within the area closed to the public. This underscores the extremely hazardous nature of Kīlauea's caldera rim surrounding Halemaʻumaʻu crater, an area that has been closed to the public since late 2007.

For discussion of Kīlauea hazards, please see: https://www.usgs.gov/observatories/hawaiian-volcano-observatory/hazards.

More Information:

• Hawaiʻi Volcanoes National Park visitor information: https://www.nps.gov/havo/index.htm
• Kīlauea daily activity summary also available by phone: (808) 967-8862
• Kīlauea webcam images: https://www.usgs.gov/volcanoes/kilauea/webcams
• Kīlauea photos/video: https://www.usgs.gov/volcanoes/kilauea/photo-and-video-chronology
• Kīlauea lava-flow maps: https://www.usgs.gov/volcanoes/kilauea/maps
• Kīlauea FAQs: https://www.usgs.gov/volcanoes/kilauea/faqs
• Kīlauea hazards discussion: https://www.usgs.gov/observatories/hawaiian-volcano-observatory/hazards
• Meaning of volcano alert levels and aviation color codes: https://www.usgs.gov/programs/VHP/volcanic-alert-levels-characterize-conditions-us-volcanoes.  

Tierra del Fuego - The Land of Fire (and Mountains, Ice and Strike Slip Faults)!

With the Antarctic Peninsula 600 miles to our stern, the Seven Seas Splendor approached and docked in Ushuaia Argentina on February 5, 2025. This former penal colony (which now houses a fantastic museum), is commonly known as our globe's southernmost city. It is located along the shores of the Beagle Channel on the island of Tierra del Fuego. I've walked the streets and hills of Ushuaia many times, so instead of doing that  again I signed up for a trek into the heart of its rugged mountains.

Part 1 - An Inland Trek on Terra del Fuego

The approach to Ushuaia with Tierra del Fuego's mountains as a backdrop.

Through the years, I have watched this dock become 3 times longer and 100% wider - all to accommodate the ever increasing traffic to Antarctica. All the ships here are part of the Antarctic trade. The hills in the background are part of Argentina's Tierra del Fuego National Park. To see a previous post about the park click here.**And remember, you can search for any location on this blog using the search function in the upper left!

First, some locations. This is a map of Isla Grande de Tierra del Fuego outlined rather simply in yellow. Ushuaia and Punta Arenas shown for reference and the track of the Splendor is also shown. Note the mountainous southern side of the island and the north being a subdued coastal plain. Isostatic loading, glacial erosion and (in some instances) faulting, are responsible for the large eastward-projecting bays into the islands' western (left) side.

Zooming in a little more, the active Magallanes-Fagnano Fault system is shown (yellow line). This is a left-lateral strike slip fault that separates the South American plate (top) from the Scotia plate (below). The highest elevations shown (south of the fault) are part of the Darwin Range (glaciers emanating from this range are shown at the end of this post). The white line fills another linear valley, where our trek took place and is curiously parallel to the major transform valley. For a recent discussion about slip rates on this fault see this paper.

About 20 miles north of Ushuaia on National Route 3 (the Pan American Highway in Argentina), we reached the valley where our trek would begin. This valley runs parallel to and is south of the Fagnano Lake and valley where the Magallanes-Fagnano Fault is located (the fault is behind the saw-tooth peaks appearing on the skyline). Note that there is also a thrust fault just below the saw-tooth peaks, where metamorphosed Upper Jurassic volcanic and sedimentary sequences (dark rocks and called the Tobífera Fm.) are thrust over and on top of Lower Cretaceous marine rocks (lighter colors and also slightly metamorphosed).

A close-up of the Tobífera volcanic sediments (slightly metamorphosed).

A large beaver dam was encountered at the terminus of our hike. Beavers were brought to Tierra del Fuego in the 1940s with the hopes of creating a demand for pelts. This area however is much warmer than northern North America where they are native and the fur was of poor quality. The beavers remain and have wrought ecological disaster to the local ecosystem. Some efforts have been made to eradicate them but so far have only been locally successful.

U-shaped valley formed by Pleistocene glaciations. The entire southern side of Tierra del Fuego was overrun by ice.

Part 2 - An Evening Cruise on the Beagle Channel and the Cordillera Darwin

Splendor set off at 8 PM from Ushuaia. This view to the south is toward Isla Navarino, located in Chile. The Beagle Channel serves as the international boundary here.

This is a view back to the east toward Ushuaia along the trace of the Beagle Channel.

But up ahead, the clouds parted as the higher peaks in the Cordillera Darwin came into view. Glaciers spill from the heights onto the Southern Patagonia batholith. This is a series of granite intrusions that were emplaced in the Late Jurassic, between about 157 to 145 Ma (there are also much younger intrusions). These granite bodies are the likely source of the Tobífera volcanic sediments seen on the trek in the previous Part above.

This photo was taken at 8 PM local time.

It is somewhat uncommon to have no wind or clouds on the peaks in this area but once again we had a great experience.

The mountains here go from sea level to nearly 9,000 feet in elevation.

Ice spills from the mountains well into non-glaciated terrain.

Note the moraine in the center of the photo.

Many of the glacier names in this stretch are after countries - Italy, Romania, Germany, etc. This is the Italian Glacier (Glacier Italia). The names honor countries that participated in surveys taken in the area during a transit of Venus in 1874.

An image of the Italian Glacier taken in 2008 showing some recession. The photo is from a paper dealing with the extent of these glaciers during the Little Ice Age, which can be accessed here.

The Alemania (German) Glaciar.

The Romanche (Romania) Glacier. I love Tierra del Fuego!

Glimpses of the Antarctic Peninsula

From sweltering Rio de Janeiro and its 92°days to a frosty 34° in Antarctic days and "nights", this voyage has had its variety! We have been lucky with the weather and seeing exceptional views. The crossing from the Falklands to the Peninsula was rather smooth and Seven Seas Splendor takes any motion quite well. Suddenly, the frozen landscape began to appear.

We approached Antarctica by way of the South Shetland Islands, transiting the Nelson Strait and motoring southward toward Greenwich and Livingston islands. These "outer bands" of rocky islands are composed of volcaniclastic material (sediments derived from volcanic terrain). The cause is subduction of the Phoenix plate beneath the Antarctic plate, beginning in the Middle Jurassic (∼160 Ma) and continuing through to the Neogene (23 Ma).

A Google Earth image our route upon entering the Peninsula area. The Captain brought us into Half Moon Bay on Livingston Island and then further south to Deception Island.

The clouds parted to reveal Livingston Island, second largest in the South Shelands after King George Island. In view are the Tangra Mountains with Helmet Peak visible. The peak is 1254 m (4114 ft.) in elevation. Many fossil plants and trees come from the sedimentary rocks on Livingston Island. A paper about the paleobotany of Livingston Island can be accessed here.

This is Baily Head on the southeast corner of Deception Island. It is a tuff cone (also called scoria or cinder cones) that was emplaced in a sub-glacial setting. During the Pleistocene Epoch (2.58 Ma to about 10,000 years) ice covered the entire edifice of Deception Island. However, ice cover cannot stop volcanic eruptions and as they say, "The show must go on!" Note the yellowish-colored tuff beds on the top right of the cone, eruptive material called palagonite, that is quenched in the presence of melted glacial ice.

Deception Island was first sighted by sealers in January 1820 and visited later that year by famed American sealer Nathaniel Palmer, who named the island for its narrow and thus, deceptive entrance, now called Neptunes Bellows. The British built a station inside the bay in the 1940s but it was destroyed by the volcanic eruptions that rocked the island between December 1967 and February 1970. I have highlighted the location of Baily Head with a green circle, the feature shown in the previous photo.

Many details about the geologic history of Deception Island are still forthcoming but not for a lack of study. Classified as a large shield volcano, its diameter on the seafloor is 30 kilometers (or about 20 miles)! The island gradually grew from a water depth of more than 4000 ft. (1300 m) before it broke to the surface as either a subaerial or sub-glacial edifice. Its original elevation is unknown, as sometime between 10,000 and 6,000 BP (years Before Present) much of the volcano was catastrophically destroyed in a massive phreatic steam blast, much like the eruption of Krakatoa in 1883 or the Thera volcano that created Santorini Island in Greece about 3,600 years ago. At Deception Island, hot magma likely encountered seawater or melted glacial ice to create the steam explosion that created this large caldera. Soon after, water from the Bransfield Strait entered the depression to form Port Foster, 6 miles (or 10 kilometers) in diameter. Most of the exposed rocks today are post-caldera rocks. Historical documentation of eruptions are from 1839 to 1842 and those of the 1960s.

See previous posts from me here and here with views of the interior of the caldera and Port Foster.  

A lone iceberg at sunset (9:20 PM local time) on February 1, 2025 - sailing south from Deception Island.

December 2, 7:40 AM. Shrouded in fog is not an unusual occurrence in the Antarctic Peninsula but no one signed up to see this. Our goal was Wilhelmina Bay and we tried two different entrances on each side of Nansen Island. Still thick fog. So, quick thinking had us retrace our wake, back out into the Gerlache Strait, where clearer skies were hoped for.

And it worked! This is a view to the south from outside Wilhelmina Bay. We spent our 2nd day here cruising toward Niemeyer Channel and Fournier Bay. However, on Day 3...

We found ourselves at the north entrance of the Errera Channel (background). The channel was full of ice but we eventually pulled up adjacent to Cueverville Island (right).

It may be difficult to see but note the pinkish areas on Cueverville Island where gentoo penguins are nesting.

The Peace Boat moves toward the Ererra Channel under increasingly ideal conditions.

Passengers on Deck 12 of Splendor enjoying a glorious sunny day!

Over on the Arctowski Peninsula the clouds were dancing around the peaks.

While on Anvers Islands, rocks of the Trinity Peninsula Group were visible from beneath huge thicknesses of ice. For a more in-depth description of these rocks, see today's Facebook post from the Arizona Geological Survey. I am a contributor to posts on that site, accessed here on Facebook. To access the post moving forward, scroll to a date of February 7, 2025 on their FB site.

Humpback whales also made an appearance for us. There were at least five pairs as we headed toward Dallmann Bay.

And then, the sky opened! Streaming cirrus clouds above an icy world.

This completed our three day stay in the Antarctic Peninsula. I will be posting about Terra del Fuego and the Chilean fjords in future posts. As Captain Marco likes to say on Splendor, "Ciao for now!"

The Southern Coast of Brazil

Rio de Janeiro 

RDJ - it seems to me now -  is a place that I used to know. Back in the 1990s, I came here a lot and stayed a month or two at a time. That seems like a different life and I am a certainly a different person now. But the memories of this unique combination of a giant megapolis situated within and upon a stunning landscape still holds enchantment for me. That is, if you can ignore the sweetish-smell of rotting fruit permeating the air or the polluted water in the very restricted and closed basin that is Guanabara Bay (one of the original Seven Natural Wonders). Rio is essentially a mix between a city on a bay - like San Francisco - and a world-class landscape - like Yosemite Valley. What a place!

The magnificent landscape surrounding Guanabara Bay is perhaps most easily recognized near its entrance (upper left), where the Paõ de Açucar (Sugarloaf) monolith seems to rise up from beneath the sea. The rocks are between about 714 and 644  million years old (Ma), being emplaced during the Panafrican-Brasiliano orogeny (younger ages have been reported across the bay in Niteroi of 564 and 533 Ma, meaning that a precise age is elusive so far). This mountain building event is related to the amalgamation of the Gondwana supercontinent, that formed after the breakup of its predecessor, Rodinia. Crustal collisions caused metamorphism within the crust as well as the production of liquid magma. This occurred as various South American cratons came together - see the diagram below for a visual. (Cratons are the ancient cores of the continents and today's South America is made up of four, formerly disparate cratons). 

Another view to the south and east reveals more of this stunning landscape! The peak in the distance is Pedra da Gávea, rising some 2,769 feet (842 m) above the sea. Some say it is the highest coastal monolith in the world. Note it's relatively flat top that is a different and younger granite in contact with the metamorphic rocks below. While these monoliths appear to be original shapes of plutons, they are not. The shapes are the result of tropical weathering.

This is a close-up of the most widely used building stone in Rio de Janeiro. It is technically an augen-gneiss. Its abundance, durability, and textural beauty enhances its use throughout many of Rio's buildings and rock-lined walls. When it is polished, it is one of the most beautiful rocks I've ever seen and I fell in love with it while walking the promenades of a quiet neighborhood called Urca, located at the base of the Sugarloaf in photo 1.

The majority of the rocks in Rio's landscape formed as a result of continental convergence. Cratons shown in purple and light blue were microcontinents that collided to form larger land masses. Rio de Janeiro is located where the numeral 4 is depicted, in a collisional terrain called the Ribeira Belt, shown in light brown. Other mobile belts of a similar age are darker brown with the numbers representing different mobile belts; yellow stars are locations of ophiolite, slivers of ocean crust that was caught and crushed between two cratons. 

Note how some cratons overlap both Africa and South America (Amazonian with West Africa and Congo with Saõ Francisco (SFC). The two modern-day continents would not attain their present outlines until the opening of the Atlantic much further into the future in the Cretaceous (120 Ma). 

The diagram is from Figure 5 in: S. Oriolo, P. Oyhantçabal, K. Wemmer, S. Siegesmund; 2017, Contemporaneous assembly of Western Gondwana and final Rodinia break-up: Implications for the supercontinent cycle; in Geoscience Frontiers, Vol. 8, # 6, pp. 1431-1445, ISSN 1674-9871. https://doi.org/10.1016/j.gsf.2017.01.009.

(https://www.sciencedirect.com/science/article/pii/S1674987117300294).  

I could on and on about Rio. But I have to catch a ship - we're sailing south to other locations in Brazil! As we left the dock in Rio, the futuristic Museu do Amanhã (Museum of Tomorrow) was visible. This was constructed in advance of the 2016 Summer Olympics in Rio. 

Ilha Grande

Ilha Gande (Big Island in Portuguese) was a green surprise! With the summertime temperature already in the high 80s at 10AM, the proximity to the water in the village of Abraão was welcoming.

Map of Ilha Grande. The island is a little less than 8 miles long and 4 miles wide. The location relative to the mainland can be seen in the upper left. Ferries to the mainland take only 1.5 hours. Brazil is slightly smaller than the continental USA. Image from Wikipedia by Rosso Robot. 

Approaching Abraão by the ship's tender, it did not look like much. About 4,000 people live in the village however.

This is not the main beach-fronting street but more of a look inland into the non-tourist area. The commercial center has palapa-like restaurants and curio shops. I was surprised that a medium-sized cruise ship like Splendor came to a place like this but it was well worth it.

A street mural.

A very calm day in the harbor. The temperature was hot and it was steamy.

Splendor at repose at Ilha Grande.

We walked a half a mile toward the ruins of the penitentiary...

...and there were some beautiful glimpses along the way of the tide zone, that included smooth, rounded boulders of the same granite and gneiss seen further north in Rio de Janeiro. The rounded shapes form by spheroidal weathering. See a description of this process in the next photo.

A small rockfall in 2023 had exposed a relatively fresh look into how the rounded granite boulders are formed. Note that the entire body of rock is massive to begin with. But as fractures and cracks develop within the granitic mass, water seeps into the cracks and begins to chemically weather the granite. The feldspars in the rock do not like humid conditions and turn to "mush" through time. Eventually a hard, unweathered core of rock remains surrounded by the crumbly weathered fracture zone. Voilà! Spheroidal weathering and the rounded boulders fall out and are washed to the shoreline..

On one of the rounded boulders, metate marks were seen. Human habitation has been here at least for 7,000 years.

There are many fresh-water springs that emanate from the landscape, providing domestic water and a cool swim.

We hiked up the hill to see an aqueduct that fed water to the penitentiary. Impressive!

Beach scene from the heart of Abraão. One of our local guides told me that he came here from Rio to surf when he was 16 years old. He fell in love with the island and its laid back way of life. He vowed to return. It took him a few more years but he has now lived on the island for 25 years. When he moved here, his mother was aghast - as a former penitentiary island, she was worried for his safety.

Santos and Brazilian (and Italian) Coffee Culture

São Paulo is the fourth largest city in the world with nearly 22 million people. About 50 miles from the coast its port is a city called Santos. This has been a major port in Brazil for centuries and when the coffee crop was introduced in the 1600s, this was a major export location.

The main street in Santos is being refurbished on the "Brazilian schedule". It's been underway for years.

The morning stop was Museu do Café - the Coffee Museum. This used to be where the buying and selling of the crop crop took place so it is an ideal location to learn about the long history of Brazilian coffee.

This is a view of the balsa or trading floor. It operated just like the New York Stock Exchange with buyers and sellers screaming prices from the chairs beneath the ornate stand glass above. A detail is below.

Detail of the stained glass on the ceiling of Bolsa do Café. To learn more about the buildings history, see this.

A special exhibit was in place concerning the making of espresso, something Brazilians learned to love beginning at the start of the 20th century. It arrived to these shores from Italy. See a description of this exhibit here.

Santos is also the home of the Pele Museum, since he began his career playing for Santos!

Everything Pele can be found here, from his humble rural upbringing, to the lessons in life and futebol from his father, to his signing a contract at the age of 15 with Santos and his illustrious career. I really enjoyed this museum. 

A Day at Sea Towards Uruguay 

As we left Brazilian waters we had a gloriously calm day at sea sailing toward Montevideo Uruguay. The weather was superb and seas calm as glass. Streaming to the south out of the north were the wispy tendrils of beautiful cirrus clouds. They were present in the sky for most of the afternoon. I love cirrus clouds! Awesome!