| | Entrance to the National Park | |
| | | The Natural Entrance to the Caverns. There is also an elevator to the bottom. | |
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| | Looking back up to the entrance from inside the caverns | |
| | | Speleothem. A fancy word for cave decorations. | |
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| | Drapery speleothem. Draperies are formed when a line of running moisture builds up big sheets of rock. | |
| | | Cavern view. It is hard to convey in photos just how huge this place is, Tiny-E. | |
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| | Looking down at tourists on the path. They are blurry because I needed to use time exposure for these photos and I was not always able to keep the camera steady. | |
| | | This rock used to be on the ceiling but then fell. You can tell because the dripping rock down its side is tilted. | |
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| | And looking closer at the speleothems on top of the big rock, it fell a long time ago for this much growth to occur. | |
| | | A close-up view of dripping rock. | |
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| | View in the King's Palace. A large room with lots of speleothems. | |
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| | | Another drapery speleothem, backlit with an electric light. Yes, it really is translucent rock. And you can see a cave cricket at the top of the photo. | |
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| | | When a speoleothem connects ceiling to floor, it is called a column | |
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| | When speleothems grow down from the ceiling, they are called stalactites. This means the water seeping through the rock above has a very low flow rate, allowing the rock to accumulate above. | |
| | | Round, noduley speleothems | |
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| | This flow speleothem looks like a real liquid flow | |
| | | Cavern pool. Since all the water in here seeps through the rock above, there are no fish in any of these pools | |
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| | The Green Pool. Turns out this color is due only to refraction. | |
| | | Stalagmites growing up to stalactites. Stalagmites are speleothems formed by a high flow rate of seeping water, which drops to the ground before the dissolve rock can precipitate. | |
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| | An unusually well-rounded stalagmite. | |
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| | The Lion's Tail. A very fore-shortened view. This stalactite is about 6 feet long, and has popcorn speleothem at the end. Popcorn speleothem is caused by evaporating water. | |
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| | These guys are 30-50 feet tall. These photos don't quite convey that, do they? | |
| | | Another view of the big guys | |
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| | Fairyland. James White, the first explorer of the caverns, came up with many names for things in here. | |
| | | The pair on the left had just the right flow to grow the speleothems the same amount. The one on the right had a much higher rate of flow of water. | |
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| | The Chandelier, in the Big Room of the Caverns. | |
| | | These stalactites are like 40' long! | |
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| | In front of this squat stalagmite, note the ring of rock growing at the level that the water pool used to be at | |
| | | I don't know how this formed. It looks like a big shell of rock. | |
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| | More Chandlier. The stalagmite on the right is maybe 40 feet tall. | |
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| | Big stalagmite. This one is actively growing, meaning water is dropping on it from above | |
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| | Those are not sticks at the bottom of this pit. They're stalactites that fell off a long time ago and then got covered over. | |
| | | A view inside the Big Room | |
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| | A view through a window to the Chandelier | |
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| | Speleothems. They come in all sizes. This alcove was only about 3 feet tall. | |
| | | The path through an area called the Zoo | |
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| | | In the evening in the bat-viewing amphitheatre | |
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| | That's where I entered in the morning | |
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| | Those blurry things are the bats | |
| | | These bats are stragglers. Most have already migrated to places in Mexico. | |
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| | There they go for a nightime feeding | |
| | | A drive back to my hotel in White's City. White's City is basically "Carlsbad Caverns Hotel and Restaurant City". | |
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| | This was weird weather. Here I am in the middile of the desert, and it's 40 degrees out in heavy fog! | |
| | | Driving back to the hotel | |
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| | Sunset over the Gualalupe Mountains | |
| | | Sunset over El Capitain mountain at the southernmost end of the Guadalupe Mountains | |
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