Armstrong Redwoods State Natural Reserve: A Walk Among California’s Giants

As you pass through California, take a moment to step away from the city’s frenetic pace. North of the Golden Gate across the bay that lends its name to the bridge bridging it, a multitude of natural wonders await. The sunlit vineyards of Sonoma or Napa counties, of course, and the charms of towns such as Petaluma, certainly. But also the austere verticality of the coastal redwoods, an endemic species of the Pacific coastline of North America, which carpets the fog-swept valleys.

Silence falls as soon as you enter Armstrong Redwoods State Natural Reserve in Sonoma County. The city noises fade and vanish among the colossal trunks of the local giants: the coastal redwoods, silent witnesses to the area’s history — from Indigenous customs to the rise of Silicon Valley’s titans, through the Hispanicization and then Americanization of California. Explanatory panels and clearly marked paths guide the walker among the trees: don’t wander off, you would threaten the local species.

A Millennium of History Before Humans

Before becoming a reserve, these woods were first a inhabited territory. Not even two centuries ago, the sequoia clearings welcomed Indigenous populations. Kashaya Pomo, South Pomo, and Coast Miwok would gather there to trade, play, dance, and sing. Under the trees, dwellings were built with the thick bark of the sequoias, sufficiently insulating to keep the heat. The youngest learned the gestures that would allow the group’s know-how to be perpetuated: weaving baskets, shaping flint, working the materials offered by the forest.

Then California’s face changed. At the end of the 19th century, timber operators began to tackle the vast sequoia forests that covered the region. It was in this context that Colonel James B. Armstrong of Ohio settled in California, giving his name to the park’s oldest giant, a 93.9-meter-tall behemoth born 1,400 years ago.

Facing the scale of tree felling, the colonel and his family bought land and positioned themselves as early local guardians of these forests. Armstrong died in 1900, but his battle continued. His family and friends carried on with the efforts to protect the woods. Armstrong Woods eventually became a county park in 1916, before joining the California State Parks system in 1934. The Armstrong State Redwood Reserve today protects about 326 hectares of forest. It constitutes the largest stand of first-generation redwoods accessible to the public in Sonoma County, and offers a unique glimpse into what the great forests that once covered the region looked like.

Parson Jones, the Reverend Friend of Trees

At Armstrong Redwood, history is written in the trees: the tallest of these woods, the Parson Jones Tree (94.5 meters), bears the name of Reverend William Ladd Jones, known as Parson Jones, a missionary pastor of the Congregationalist Church. He served in the gold-bearing Sierra regions, the sequoia forests around Eureka and the San Francisco Bay. For many years he was a neighbor and friend of James Armstrong and his two daughters. The tree that bears his name will outlive him, by far! It is around 1,300 years old.

The tree dedicated to Reverend Parson Jones is the largest of these woods.

In the Fog, Life

Today the coastal redwood, Sequoia sempervirens, is the largest living thing on Earth. Its endemic natural range is reduced to a narrow stretch along the Pacific Coast, from southern Oregon to central California, rarely more than 80 kilometers from the ocean. Here the coast’s characteristic fog becomes vital: it regularly envelopes the trees, limits the forest’s drying, and brings moisture to an ecosystem that many animal and plant species depend on.

The roots of Sequoia sempervirens reach close to the surface underground, but also extend for dozens of meters around the trunk, intertwining with those of neighboring trees. This subterranean architecture gives them stability against winds and helps capture surface water. When fog condenses on the branches, the water drips to the ground and joins the forest litter, that thick layer of organic matter made up of needles, leaves, bark, and plant debris. Moss, lichens, and roots then help hold and redistribute this precious moisture.

Millennia later, the redwood has proven its capacity to adapt. History shows the species has weathered many climate shifts. After a fire, a storm, or the felling of a tree, the immense root system can sprout new shoots around the stump. Look around you: these young trees sometimes form nearly perfect circles, fairy rings. What might appear to be a cluster of distinct trees is in fact the vegetative offspring of a single individual. An entire forest can thus carry the physical memory of a vanished tree.

Just a few meters above the walker, another scene unfolds. A large portion of animal life concentrates in the canopy, sometimes more than 60 meters above the ground. The cry of a raven breaks the stillness, followed by the hammering of a woodpecker or the rustling of a gray squirrel. Red tree voles also move among the heights and feed especially on the needles of Douglas firs. Down below, a black-tailed deer may cross the undergrowth, while a banana slug glides between the damp leaves. Gray foxes, pumas, raccoons, coyotes, acorn woodpeckers, and Steller’s jays also roam the forest, but often far from human eyes.

At Armstrong Redwood, the fog soaks the branches, the roots surge from the soil, lichens retain the moisture, and fallen trees give rise to new life. The visitor, for his part, is only a passing guest. Let it remain so.

Strange Tourist Tradition Threatens the Giant’s Causeway in Northern Ireland

At first glance, they might look like simple lucky charms left behind by passing travelers. Yet the thousands of coins pressed into the rocks of the Giant’s Causeway, in Northern Ireland, forced conservationists to launch a particularly delicate cleaning operation. More than 20 kg of coins have already been removed from this UNESCO World Heritage site. And despite several months of intervention, thousands of coins remain trapped within the rocks.

A meticulous operation at the heart of an exceptional volcanic site

Located in County Antrim, in Northern Ireland, the Giant’s Causeway is one of the United Kingdom’s most famous geological landscapes. The site contains more than 40,000 basalt columns, formed about 60 million years ago during a volcanic activity. Molten rock flowed into the fissures of the Earth’s crust before cooling, contracting and fracturing, giving birth to these columns with their characteristic geometric shapes. The site is registered as a UNESCO World Heritage site.

It is in the interstices of these formations that visitors gradually began to wedge coins. The gesture seems to carry symbolic significance, with some tourists considering the money as a good luck charm or a sign of love. But the coins remain exposed to sea spray and humidity, and their prolonged presence in the fissures can become problematic for the rocks…

The National Trust therefore undertook their removal in May 2025, after an alert from the Geological Survey of Northern Ireland. Early observations had highlighted effects that were both physical and chemical on the basalt. The intervention required the expertise of a stone mason, Nathan Morrow. The teams could not simply pull the coins out for fear of damaging the columns. Pliers were used for those near the surface, while a jointing tool allowed access to coins wedged deeper in the cracks.

The difficulty varied greatly from one place to another. Some coins came out quickly, while the most deeply lodged ones could require more than 20 minutes of work each. In total, the operation involved around 200 hours of work. “Approximately 200 hours of work were devoted to the project”, said Cliff Henry, the National Trust’s nature engagement lead, to Need To Know.

Salt accelerates corrosion of coins stuck in cracks

But the problem is not limited to the number of coins scattered on the site. Their composition and the conditions to which they are exposed can also worsen their impact on the rock. British copper coins minted since 1992 notably have a steel core coated with copper. The 5, 10, and 20 pence coins are, meanwhile, made of steel coated with nickel. Yet these metals do not react to the environment in the same way. With humidity and especially the salt brought by sea spray, corrosion accelerates. The different metal layers can separate and expand inside the cracks, exerting pressure on the basalt.

This degradation also makes the coins difficult to identify after a few years. “The coins corrode so quickly in the salty and humid conditions of the Causeway that it becomes impossible to determine what currency they were, not to mention their date, after only a few years”, explained Cliff Henry.

The majority of recovered coins unsurprisingly came from the United Kingdom and the euro area, visitors tending to use the currency they have in their pockets. Only a portion could still serve as money, the others being too deformed or corroded.

Despite these hours of effort, the cleaning did not manage to remove everything. Several thousand coins would thus remain wedged in the cracks. Some are now too deeply buried to reach. Others are so rusted that moving them could further damage the rocks.

Cliff Henry, for his part, compares their accumulation to a carnival ride in which new coins gradually push the older ones inward. “As in a Penny Falls game in an arcade, the coins have been pushed further into the joints by the new coins hammered in at the front”, he explained.

The phenomenon could therefore continue to pose problems even after the end of the main operation, completed in June 2026. New coins have already been found after the cleaning, including 42 removed by Cliff Henry last month. The National Trust now plans to monitor the formations regularly and remove new deposits.

Informational panels have also been installed to ask visitors not to push coins into the rocks. The National Trust also plans to turn a portion of the recovered coins into objects for display to concretely demonstrate the consequences of this practice.

Rock Climbing: Scaling Mauritania’s Granite Giants

Mounina Bero, 17 years old, eyes the void beneath her feet, then remains motionless on a rocky ledge of Ben Amira, twenty meters above the ground, stubbornly refusing for long minutes to abseil down. Her elder sister, Kallat, encourages her from below, having taken up climbing two years ago, not without first overcoming the reluctance of the people in her village – after all, no one here had ever seen a woman do such a thing! Since then, the young girl dreams of becoming a tour guide specializing in rock climbing.

Grand Traverse of the Volcanoes: In the Heart of Auvergne’s Giants

On the roads of Cantal, everyone knows that slender figure with a determined stride, a walking stick in hand, a black beret crowned with a small cow on the head. Each day, Brother François, with a youthful look beneath his white hair, goes from farm to farm to help milk the cows, cut the hay, or repair the fences. François Cassingena-Trévedy, by his civil name, is a regional figure, known far beyond his village of Sainte-Anastasie, reaching Murat and even Aurillac. This affable 66-year-old man defines himself as a peasant monk. An Alsatian, a Normalien, a theology professor, a translator of Virgil, he is also a poet and writer, author of 25 books. One of them (Cantique de l’infinistère, ed. Desclée de Brouwer, 2016) speaks of his love for Auvergne by recounting a walk through the volcanoes that changed his life.

“C’est un pays rude, austère, raboteux, mais aussi sensuel, dit-il depuis les plateaux herbeux qui dominent son village. Un bout du monde infini, où les montagnes sont comme de grandes houles de lave solidifiée. C’est en marchant que j’ai décidé de quitter mon monastère pour me dédier à cette terre et à ses habitants.”

To feel, like him, this telluric summons, nothing beats setting one foot in front of the other on the volcanic bedrock of Auvergne — basalt, phonolite, Volvic stone, pozzolana… — while contemplating the conical mountains and the valleys that lie ahead on the horizon. And why not undertake the Grande Traversée des Volcans d’Auvergne (GTVA)?

The Great Volcanic Crossing

This new itinerary, created in 2024 and spanning the départements of Puy-de-Dôme and Cantal, invites you to discover the natural heritage of the region, from the iconic Puy de Dôme (1,465 m) to the Plomb du Cantal (1,855 m), passing through the Sancy massif, the Cézallier plateau and the valleys of Puy Mary. Open to all, it stretches 210 kilometers and can be completed in one go in eleven days for the bravest, but one can of course choose only a portion. Arriving in Cantal, some travelers may cross Brother François along the last third of the route. “We imagined this itinerary as a condensate of the region’s beauties – peaks, plateaus, rivers, lakes, villages – using the already existing GR [long-distance hiking trails], explains Michel Faure, local head of the French Hiking Federation, who designed the 98 kilometers of the route in the Puy-de-Dôme.