
Tunnel View
There's a moment driving into Yosemite Valley where the road curves, the trees break, and the whole thing just unfolds in front of you.
You've seen the photos.
Everyone has. You think you know what to expect.
You don't.
Nothing prepares you for the depth of it — the way El Capitan anchors the left wall while Bridalveil Fall drops on the right, and Half Dome sits in the distance framing the far end of the valley like someone placed it there deliberately. The colors. The light. The sheer vertical scale of granite walls rising thousands of feet straight up from a valley floor that somehow stays wide and open and readable all the way to the horizon.
I was with my family the first time I saw it. We rounded that corner together and the car went quiet. The kids went quiet. My wife went quiet. I went quiet.
I had trouble parking the car. I couldn't stop looking long enough to find a space.
That doesn't happen often on a family road trip.
What you're looking at is surprisingly contained for something that feels this vast. The valley is about seven miles long and less than a mile wide. The granite walls on either side rise somewhere between 3,000 and 4,000 feet straight up from the floor.
Those numbers don't prepare you either. You have to see it.

I've been to a lot of remarkable places. I photograph them specifically because I believe places have stories worth telling. But standing at Tunnel View, camera in hand, I ran into a problem I don't usually have: I wasn't sure a photograph could do this justice either.
The word people reach for is magical. It's overused. It's also, in this case, completely accurate.
They say a magician never reveals his tricks. But this is The Story Behind The Place — and here's the thing about Yosemite: understanding exactly how this valley was made, why it looks the way it does, and how close it came to never being protected at all doesn't demystify it. It makes it more magical.
So let's pull back the curtain. Because what's behind it is astonishing.
The Ice Did This
Most valleys are V-shaped.
Rivers cut downward over time, carving a narrow channel that widens gradually as you rise. That's the default. That's what erosion does when water is doing the work.
Yosemite Valley is not V-shaped.
It's broad and flat at the bottom, with walls that rise nearly straight up on both sides — some of them close to vertical for thousands of feet. The first time you really look at it, something registers as unusual even if you can't immediately name why.
That shape comes from ice.
Over multiple ice ages, glaciers moved through this valley — slowly, relentlessly, over thousands of years. Where a river cuts down, a glacier pushes outward. It grinds against the walls, scrapes away the rock, and leaves behind something wider and more open than water alone could ever produce.
A U-shape instead of a V.

And once you know that, everything else in the valley starts to make sense in a way it didn't before.
Those waterfalls — some of them dropping more than 2,000 feet — didn’t exist before the glacier. Before the ice, smaller side streams flowed gently down into the main valley at roughly the same level. Then the glacier came and carved the main valley floor thousands of feet deeper.
The side streams stayed where they were.
When the ice finally retreated, those streams were left stranded at the top of walls that hadn’t existed before — with nothing between them and the valley floor but air. They’re called hanging valleys. The water has no gradual path down. It just… falls.
Yosemite Falls. Bridalveil. Nevada Fall. All of them created by the same glacier that made the valley itself.

The flat meadows on the valley floor — quiet, almost out of place against the cliffs — mark where the glacier finally retreated and left a lake behind. Over time, sediment filled it in. The water slowed. The lake became a meadow. What looks like peaceful open grassland was underwater not that long ago — geologically speaking.
I can't fathom the amount of ice — or the sheer power of it — that it would take to carve this entire valley. Or for a lake this size to just disappear "overnight."

The river threading through those meadows didn't shape this valley. It arrived after the shaping was already done, following a path that was carved long before it got there.
Even the trails follow the same logic — rising where the terrain allows, turning where it doesn't.

Seeing It — And Fighting For It
John Muir first came to this valley in 1868 and never quite got over it. He spent years here — studying it, writing about it, arguing for it — at a time when the prevailing instinct was to look at land like this and ask what it could be used for. Muir kept asking a different question: what if the point was to leave it alone?
He became the most influential voice for preserving wild places in American history. He helped establish Yosemite as a national park. He co-founded the Sierra Club. He took President Theodore Roosevelt camping here in 1903 and convinced him, over three nights under the stars, that places like this deserved federal protection.

But he didn't win every fight.
The Hetch Hetchy Valley — a glacier-carved valley just north of here, so similar to Yosemite in scale and beauty that Muir considered it an equal — was dammed in 1913 to supply water to San Francisco despite everything he did to stop it.
Some believe he never recovered from it. He died the following year.
I'm not sure the decision was wrong given what San Francisco needed. But some things on this planet can't be undone. Hetch Hetchy is one of them.
Hetch Hetchy still sits underwater today.
It's worth knowing that when you're standing at Tunnel View feeling like this valley was inevitable. It wasn't.
It was argued for, fought over, and in one case, lost.
What Adams Knew
Ansel Adams came to Yosemite for the first time in 1916 as a fourteen year old boy, with a Kodak Brownie camera his parents gave him for the trip. He spent the rest of his life coming back.
Adams didn't just photograph Yosemite — he developed his entire technical system here. The Zone System — a method for precisely controlling exposure and contrast that transformed the way photographers think about light — grew directly out of his decades of work in this valley.
He shot in black and white by choice. Not limitation. Color film existed. But Adams believed that stripping away color forced both the photographer and the viewer to engage with what was actually there — the form of the rock, the weight of the sky, the relationship between light and shadow. Color, he felt, was a distraction from structure.

I thought about that standing in the meadow, camera in my hands, looking at a shot that felt busy and cluttered in color. Something wasn't working. I converted it to black and white.
The cliff face came forward. The river settled into its path. The trees found their edges. And the light — the bright California light hitting the granite — looked almost like snow against the dark of the forest.
I understood immediately why he kept coming back.

What color had been hiding, black and white revealed.
It took Adams a lifetime of work to articulate that instinct into a system that changed photography.
It took me about thirty seconds to rediscover why he was right.
What Almost Happened Instead
It's worth knowing that when you're standing at Tunnel View watching your family go quiet.
What feels permanent was fought for.
What feels inevitable wasn't.
And that is the story behind the place.
