Auckland is built across 53 volcanic centers, and the youngest one formed only about 600 years ago. You wouldn’t necessarily know that walking around the city. There’s no huge volcano looming over downtown. Instead, you notice grassy hills, old craters and islands sitting out in the harbor. A lot of what looks like ordinary Auckland is actually volcanic terrain. Maungawhau, better known as Mount Eden, is one of the easiest places to see it. Walk to the top and you can look straight into the crater with the skyline behind you. These hills were important long before modern Auckland existed. For Māori, the volcanic cones are maunga, ancestral mountains with cultural and spiritual importance. Many were also used for pā, or fortified settlements. People cut terraces into the slopes for homes, dug pits for food storage and built defensive earthworks. Some of those features are still visible. The traditional Māori name Tāmaki Makaurau is often translated as “Tāmaki desired by many.” It makes sense when you look at the geography. There was fertile land, good fishing, two large harbors and short overland routes where waka could be carried between waterways. Maungakiekie, or One Tree Hill, was once one of the largest pā in the region and supported thousands of people. Today, it’s easy to see it as just another great Auckland viewpoint. Look a little closer and you can still see how people shaped the land centuries ago. Rangitoto is even harder to miss. The island sits out in the Hauraki Gulf and can be seen from much of the city, but it’s surprisingly young. It formed during eruptions around 600 years ago and is the youngest volcano in the Auckland Volcanic Field. Those eruptions were witnessed by people living in the area at the time. You can take a ferry out and walk across old lava fields to the summit. Along the way are lava caves, pōhutukawa forest and old holiday baches near the shoreline. The volcanic field works a little differently than most people expect. The old cones probably won’t erupt again. If Auckland has another eruption, scientists expect it to open a new vent somewhere else in the field. So that grassy hill beside a neighborhood may be an extinct volcano. The dip in a park might be part of an old crater. Those lines cut into a slope may be the remains of a Māori settlement. Auckland gets treated as a jumping-off point for the rest of New Zealand, but I’d give it more time. Walk Maungawhau. Spend some time on Maungakiekie. Take the ferry to Rangitoto. You start seeing the city differently once you know what shaped it. This is the kind of thing I write about in my newsletter. Places you may already know, with stories that give you more to notice when you get there. If that sounds like your kind of travel, subscribe to the Timeless Traveler.