The title says “Red Cliffs,” but you might be thinking, “They don’t look very red to me!” In more neutral light the formations in the upper part of the photograph, and even more so the formations above the margins of the photograph, do have the familiar red rock quality — though it would be fair to say that they are as much brown as red. But in this stark early morning light, just after sunrise, the colors are warmed so much that they are more yellow or orange.
In many ways the geology of Death Valley produces a blank canvas for photographers who want to work with varied light. For the most part, Death Valley’s colors are subtle. The lighter portions of the formations in this photograph are a sort of muted tan in midday light. But as with so many other subjects here, this muted, neutral quality allows them to pick up the colors of sunrise/sunset, twilight, colorful clouds, and reflections from nearby formations.
G Dan Mitchell is a California photographer and visual opportunist. His book, “California’s Fall Color: A Photographer’s Guide to Autumn in the Sierra” (Heyday Books) is available directly from him. Blog | Bluesky | Mastodon | Substack Notes | Flickr | Email
2 responses to “Base of the Red Cliffs”
-
Hi Dan,
Here I am, wasting some time on a Sunday afternoon and I came back to this photo of yours. It has not lost any of the intrigue that originally caught my eye and led me to post a comment. Forgive me for diving deeper still into the details of the lighting, that for me, is the strength of this photo. Again, forgive me, but I have to take some issue with a comment of your’s re: the light falling on the foreground.You say…”The foreground light is coming from behind and above my camera position — a combination of more reflected light and light from the open sky.”
I’ll accept that open sky is supplying some over all fill light, but it is much weaker than the main, semi-hard light coming from the left. The evidence of this can be seen in the delineation of the vertical striations on the rock face at the left side of the frame. Each individual striation has a highlight at its peak then a shadow in the depression to the right, in a repeating pattern. Whatever the source of illumination, the bulk of its directional quality can’t be coming from above and behind the camera position. That would produce a much flatter light than what is seen here. The result then would be the foreground rock’s striations being less textural, less visible, more boring without the contrast of the highlight/shadow repeating pattern.On that same foreground rock, the upper left and the lower right (the ankle and the toes of the “giant’s foot”) are both darker and flatter, the result of being lit only by the open sky, providing an omnidirectional, flatter and lower level of illumination.
The overall, bottom line still exists…I love this shot! The above details are just an explanation of why it works so well for me. Thank you, Dan!
-
Charlie,
Thanks for taking the time to write a long post on this photograph. But I must admit that I’m a bit confused by your comment.
You wrote:
”You say…”The foreground light is coming from behind and above my camera position — a combination of more reflected light and light from the open sky.”
But when I look at the text I wrote to accompany this photograph, in the post you replied to, I do not see that I wrote anything like that there. I wonder if you were looking at a different photograph than the one you commented on?
In the photograph on this page — “Base of the Red Cliffs” — the sun is definitively behind and above my camera position. It is not straight behind me, but is coming from a slight angle over my right shoulder, which is why the shadows stretch towards the left.
Let me know if you can figure out why your comment doesn’t seem align with this photograph or its descriptive text.
Dan
-
This site uses Akismet to reduce spam. Learn how your comment data is processed.
(All media © Copyright G Dan Mitchell and others.)
Join the discussion — you are welcome to leave a comment or question. (Comments are moderated and may not appear immediately.)