<?xml version="1.0" encoding="UTF-8"?><rss version="2.0"><channel><title>Landform Atlas</title><description>Plain-English explainers on landforms — rivers, coasts, volcanoes, karst, deserts and glaciers — each told through a real place, with the best videos on the topic.</description><link>https://landformatlas.com/</link><item><title>The Taklamakan Desert in 10 Questions — How a Sea of Sand Formed in Inner Asia</title><link>https://landformatlas.com/why-is-there-a-desert-in-the-middle-of-asia-taklamakan/</link><guid isPermaLink="true">https://landformatlas.com/why-is-there-a-desert-in-the-middle-of-asia-taklamakan/</guid><description>Where is the Taklamakan, why is it so dry, where does its sand come from and why did Silk Road traders avoid it? Ten short answers with diagrams.</description><pubDate>Sat, 03 Oct 2026 00:00:00 GMT</pubDate></item><item><title>How Fairy Chimneys Form — and Why People Lived Underground in Cappadocia</title><link>https://landformatlas.com/how-fairy-chimneys-form-cappadocia/</link><guid isPermaLink="true">https://landformatlas.com/how-fairy-chimneys-form-cappadocia/</guid><description>Volcanic ash, a hard cap of rock and millions of years of rain built Cappadocia&apos;s fairy chimneys. The same soft stone let people carve whole cities underground.</description><pubDate>Fri, 02 Oct 2026 00:00:00 GMT</pubDate></item><item><title>How Ha Long Bay Was Formed — a Drowned Limestone Landscape</title><link>https://landformatlas.com/how-ha-long-bay-was-formed/</link><guid isPermaLink="true">https://landformatlas.com/how-ha-long-bay-was-formed/</guid><description>Ha Long Bay&apos;s nearly 2,000 islands began as seabed limestone, were carved by rain into towers, then drowned when the sea rose after the last Ice Age.</description><pubDate>Fri, 02 Oct 2026 00:00:00 GMT</pubDate></item><item><title>Why Rivers Meander — and How Oxbow Lakes Are Born</title><link>https://landformatlas.com/why-rivers-meander-oxbow-lakes/</link><guid isPermaLink="true">https://landformatlas.com/why-rivers-meander-oxbow-lakes/</guid><description>Fast water on the outside of a bend, slow water on the inside. Here is how rivers like the Mississippi curve, wander and leave oxbow lakes behind.</description><pubDate>Fri, 02 Oct 2026 00:00:00 GMT</pubDate></item></channel></rss>