ZJ Speaks

7-24-11

IT IS HOTTTTT!!

Ugh the heat wave is hottt.

This isn’t fun any more but the trip is. We stopped early to find a hotel and there was a baseball tornament going on so there was only 1 room in the hotel out of 5 hotels and we got it.

The next day we went to the goose county park and that night people where shooting off fire works and I couldn’t sleep.

Today we are in a park and we just got out of the pool it was nice and refreshing.          ZJ

 Badlands (WIKI)

A badlands (also badland) is a type of dry terrain where softer sedimentary rocks and clay-rich soils have been extensively eroded by wind and water. It can resemble malpaís, a terrain of volcanic rock. Canyons, ravines, gullies, hoodoos and other such geological forms are common in badlands. They are often difficult to navigate by foot. Badlands often have a spectacular color display that alternates from dark black/blue coal stria to bright clays to red scoria.

The term badlands represents a consensus in North America. The Lakota called the topography "Makhóšiča", literally bad land, while French trappers called it "les mauvaises terres à traverser" – "the bad lands to cross". The Spanish called it tierra baldía ("waste land") and cárcava. The term badlands is also apt: badlands contain steep slopes, loose dry soil, slick clay, and deep sand, all of which impede travel and other uses. Badlands form in semi-arid or arid regions with infrequent but intense rain-showers, sparse vegetation, and soft sediments: a recipe for massive erosion.

Some of the most famous fossil beds are found in badlands, where erosion rapidly exposes the sedimentary layers and the scant cover of vegetation makes surveying and fossil hunting relatively easy.

Some of the best-known badland formations can be found in the United States and Canada. In the U.S., Makoshika State Park in Montana, Theodore Roosevelt National Park in North Dakota and Badlands National Park in South Dakota together form a series of extensive badland formations. Another popular area of badland formations is Toadstool Geologic Park in the Oglala National Grassland of northwestern Nebraska. Dinosaur National Monument in Colorado and Utah are also badlands settings. A small badland called Hell's Half-Acre is present in Natrona County, Wyoming. Additional badlands also exist in various places throughout southwest Wyoming, such as near Pinedale and in the Bridger Valley near the towns of Lyman and Mountain View, near the high Uintah Mountains.