These were such an interesting geologic curiosity, I just had to do a little research to learn more about them. It turns out that Moqui Marbles (according to the Science Daily website) are hematite concretions formed underground when minerals precipitated from flowing groundwater. The marbles are very similar to rocks known as "blueberries" that have been found on Mars. In Utah the rocks had iron in them originally. Water travels through these rocks and leeches out the iron. The water moves through cracks, holes, layers or pores until it reaches some place where the chemistry is different and causes the iron to precipitate out of the water as hematite. After the concretions formed in groundwater, the surrounding Navajo sandstone slowly eroded away over millions of years, so the hard, erosion-resistant concretions accumulated on the ground.
Seeing the marbles was certainly one of the highlights of our trip and the strangeness of seeing them would linger in our thoughts throughout the rest of the trip. After getting our fill of seeing the marbles, we continued on our hike across the plateau towards Tunnel canyon.
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