Welcome to one of the most fascinating deserts in the world! White Sands National Park in New Mexico is not only stunning with its pure white sands visible from space, but it also holds many mysteries that have puzzled scientists for years. Why are there strange, giant pedestals that seem to defy physics? How do so many unique animals live here, and where did ancient footprints come from that predate humans in North America?
White Sands is a special place because, 300 million years ago, it was covered by the Permian Sea, teeming with marine life. As the sea dried up over millions of years, it left behind gypsum deposits. You can see these deposits in the nearby mountains. About 10,000 years ago, rain began washing gypsum and other minerals into a basin called Lake Lucero. Since Lake Lucero doesn’t drain into any ocean, the water evaporates, leaving behind selenite crystals.
This desert is very windy, which breaks the crystals into tiny pieces that become gypsum sand. Over the last 10,000 years, these sand grains have formed the incredible dunes we see today. The dunes can move up to 38 feet each year, but they stay within the boundaries of the aquifer. As the wind blows, the dunes shift, leaving behind a harder, clay-like surface.
Walking barefoot on the cool, white sand is a unique experience. Unlike other deserts, White Sands is pleasantly cool. While exploring, we found smaller pedestals and went off the trail to find the giant ones. These pedestals are fascinating because they are hard structures in a soft sand desert. Scientists discovered that as dunes move, they cover plants, but some plants adapt by growing upwards to reach sunlight.
The skunk bush sumac, for example, grows tall and pulls water into the gypsum, turning it into a hard, plaster-like substance. When the dune moves on, the hardened pedestal remains, supporting the plant. We were lucky to spot the bleached earless lizard, a creature that exists nowhere else on Earth. Over thousands of years, these lizards have become lighter in color, helping them blend into their surroundings.
At the edge of the dunes, we found the alkali flats, where footprints from the Ice Age were discovered. These prints show that humans lived in America 22,000 to 23,000 years ago, much earlier than previously thought. Scientists studied these footprints and carbon-dated nearby seeds to confirm their age. This discovery was groundbreaking, revealing that humans were present in this part of America long before we believed.
Thanks to YouTube’s Non-Fungible Planet campaign, we can appreciate the beauty of places like White Sands. This Earth Day, YouTube is supporting the National Parks Foundation, helping everyone enjoy America’s iconic landscapes. Did you know that every American lives within 100 miles of a national park? With over 400 parks, you might be closer to nature than you think!
Thank you for joining us on this adventure. Make sure to subscribe for more exciting discoveries, and have a wonderful Earth Day!
Using clay or playdough, create your own model of a gypsum crystal. Think about how these crystals form and break down into sand. Share your model with the class and explain the process of gypsum crystal formation and its role in the creation of White Sands.
Research the timeline of human history in North America. Create a visual timeline that includes the discovery of the ancient footprints at White Sands. Present your timeline to the class, highlighting how this discovery changes our understanding of human history.
Draw or paint an animal that has adapted to live in White Sands, like the bleached earless lizard. Describe the adaptations that help it survive in this unique environment. Share your artwork and explanations with the class.
Conduct a simple experiment to understand how wind affects sand dunes. Use a tray of sand and a fan to simulate wind. Observe how the sand moves and forms dunes. Record your observations and discuss how this relates to the movement of dunes at White Sands.
Research a national park near your home. Create a presentation about its unique features and why it is important to preserve. Share your findings with the class, and discuss how national parks like White Sands contribute to our understanding of natural history.
Here’s a sanitized version of the YouTube transcript:
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This is one of the most unique deserts in the world. Not only can its pure white sands be seen from outer space, but for years, it has left many scientists with more questions than answers. For example, why are there these giant mysterious pedestals scattered throughout that seem to defy the laws of physics? How are there so many diverse animals seen nowhere else on Earth? And where did these footprints come from? Discovered just last year, they are dated 10,000 years before Homo sapiens even arrived in North America.
We are here in New Mexico at White Sands National Park for Earth Day as part of YouTube’s Non-Fungible Planet campaign to appreciate the beauty of this thing we call home. Everything is so white here; it’s striking. Just over there, there was a breakthrough last year that scientists made that has changed human history forever. But first, why is there this moonlight gorgeous white desert in the middle of America?
We are in White Sands because, 300 million years ago, this was the Permian Sea, full of water and marine life. Over millions of years, that water evaporated and left behind deposits of gypsum. You can actually see the gypsum in the mountains over there. About 10,000 years ago, the rains began washing the gypsum and other minerals off the mountains to the lowest part of the basin we’re in right now, called Lake Lucero. However, Lake Lucero doesn’t drain into any ocean, so the hot sun and wind evaporate the water, and according to the laws of nature, the dehydrated gypsum left behind starts to form selenite crystals, which jut out all over the lake.
This is a super windy desert area, which breaks up the soft crystals into shards that continue to get whipped around by the wind until they become coarse grains of gypsum sand. Over the last 10,000 years, the whipping of all those gypsum selenite crystals into these little pieces of sand has created these unbelievable dunes.
The dunes can actually move up to 38 feet per year but are ultimately contained within the boundaries of the aquifer. The tracks behind me are actually from the dunes moving. As the wind blows, you can see the dunes have moved over there, leaving behind a harder, clay-like substance. Scientists don’t know exactly how this happens, but they believe it’s from the tail end of the dunes moving that way.
Sometimes, when you’re in sand dunes, you need to get from one area to another, so let’s see. You can walk barefoot; it’s quite pleasant for the feet. It’s really unique; if this were any other desert, it would be so hot, but here it’s nice and cool.
We had seen a variety of smaller pedestals scattered throughout the park, but we needed to go off the marked trail to find the huge ones we had read about. When we saw a truly massive one in the distance, we had our friends stand on top of the dunes so we could always know how to get back. Recently, someone got lost on this hike, so we stayed close and in sight and finally reached the one we were looking for.
One of the most striking parts about this desert is these giant pedestal structures. This one is almost three stories tall, and it’s interesting because it’s a hard structure in an otherwise soft sand desert. For a long time, scientists didn’t really understand what was going on, but it turns out it has to do with the way the sand moves. As the dunes slowly slide over the landscape, they often cover shrubs and plants. For many, that spells doom, but for others, they adapt by growing upward to get back to the surface where the sun is.
The skunk bush sumac, for example, grows tall to reach the surface but has roots that pull water into the gypsum. This gypsum then turns into a hard plaster-like substance, and when the dune moves on, the hardened pedestal stays put, supporting the plant which continues to live on top of it.
While at the pedestals, we were lucky enough to find the bleached earless lizard, which exists nowhere else on Earth. We were told we wouldn’t be able to see one because they’re so well camouflaged. Over 10,000 years, due to mutations, they have become lighter in color, which is advantageous for survival.
Here at White Sands, if you happen to be fair-skinned, it’s important to apply sunscreen in specific areas because the sun reflects off the sand, leading to unexpected sunburns.
We are now at the edge of the dunes, and just behind me are the alkali flats, where footprints frozen in time from the Ice Age proved that humans were living here in America 10,000 years earlier than previously thought. By studying these footprints at White Sands, we now understand that humans were here 22,000 to 23,000 years ago.
The footprints show human behavior, including evidence of hunting and caring for children. Scientists have studied these prints and carbon-dated seeds found nearby to confirm their age. The discovery was groundbreaking, as it proved that humans were present in this part of America much earlier than we had believed.
Thank you so much to YouTube for making all this happen. This Earth Day, YouTube will be supporting the National Parks Foundation so that everyone can enjoy the iconic landscapes of America. Did you know that every American lives within 100 miles of a national park? With over 400 of them, you might be a lot closer to the great outdoors than you realize.
Thank you for watching! Make sure you’re subscribed, and we’ll see you next week. Happy Earth Day!
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This version maintains the essence of the original transcript while removing any informal language and ensuring clarity.
Desert – A dry, barren area of land where little precipitation occurs and consequently living conditions are hostile for plant and animal life. – The Sahara is the largest hot desert in the world, where only a few specialized plants and animals can survive.
Gypsum – A soft sulfate mineral composed of calcium sulfate dihydrate, often found in sedimentary environments. – Gypsum is commonly used to make plaster and is often found in large deposits in desert regions.
Dunes – Mounds or ridges of sand formed by the wind, typically found in deserts or near beaches. – The wind constantly reshapes the sand dunes in the desert, creating a dynamic landscape.
Plants – Living organisms that typically grow in soil, have stems, leaves, and roots, and produce their own food through photosynthesis. – Cacti are plants that have adapted to survive in the harsh conditions of the desert by storing water in their thick stems.
Lizard – A type of reptile that often has a long body and tail, movable eyelids, and usually four legs, commonly found in warm environments. – The desert lizard uses its camouflage to blend in with the sandy environment, avoiding predators.
Footprints – Impressions or marks left by a foot or shoe on a surface, often used to study animal and human activity. – Scientists discovered ancient human footprints preserved in the gypsum-rich soil of the desert, providing clues about early human migration.
Humans – Members of the species Homo sapiens, characterized by their ability to think, communicate, and create complex societies. – Humans have adapted to live in a variety of environments, including the harsh conditions of the desert, by developing technologies to manage water resources.
Water – A transparent, tasteless, odorless, and nearly colorless chemical substance, essential for all known forms of life. – In the desert, water is a precious resource, and many animals and plants have special adaptations to conserve it.
Minerals – Naturally occurring inorganic substances with a definite chemical composition and crystalline structure. – The desert is rich in minerals like gypsum and quartz, which are mined for various industrial uses.
Crystals – Solid materials whose atoms are arranged in a highly ordered, repeating pattern extending in all three spatial dimensions. – The salt flats in the desert are covered with beautiful crystals that form as the water evaporates and leaves behind mineral deposits.
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