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| Himalayan Mountains, Asia |
The Ringing mountains are the largest peaks in the Tablelands and the only ones capped in snow. They are made up of granite, diorite, monazite, shale, and limestone. High quality garnets are mined in the Ringing Mountains. From a distance of a hundred miles, the Ringing Mountains look like a ridge of reddish clouds hugging the horizon. As you move closer, their soft edges gradually grow sharper and more distinct. Within five miles of the mountains, the range takes on the appearance of a great wall.
The Windswept Mountains are made up of sandstone, shale, and limestone. They mark the northwestern base of the Ivory Triangle region. This high mountain range juts abruptly from the sandy wastes at the edge of the Tablelands on its northwestern side. These mountains are called the Windbreak Mountains because they protect the Gulg and Nibenay region from the prevailing west winds blowing off the Tablelands.
The Black Spine and Mekillot Mountains are made up of granite, gneiss, mudstone, and limestone. The Mekillot Mountains are an old, low-lying range in the center of the Great Ivory Plain. They're shaped like the backs of giant mekillots. The Black Spine Mountains are east of the Windbreak Mountains. They look like a huge gith, with a granite spine. Both of these mountain ranges get little rain.
There are other mountain ranges in the Tablelands as well, such as the Smoking Crown Mountains, the Kregill Mountains, and the mountain range near South Ledopolous. These mountain ranges are likely similar to the dry Black Spine and Mekillot Mountain ranges in composition, flora, and fauna.






