What Is The Geological Origins Of The Region

The oldest rocks found in the Death Valley region were formed in the Precambrian time period no more than 1.8 billion years ago during the latter half of the Proterozoic Eon. The rocks are seen on the steep face of the Black Mountains above the current area of Badwater and were formed via deposits of mud and sand from an ancient volcanic mountain belt. Sometime between 1.8 and 1.7 billion years ago, the volcanic and sedimentary rocks were severely altered when chemical or structural changes occurred because of intense heat or pressure from the Earth's core. Because of this process, any fossilized information about the region was lost making it impossible to truly understand the origin of the region. There is some debate on whether basalt or schist was the original and dominate rock in the region before it was transformed into contorted gneiss, but again, there is no way to prove either theory.

The soil and biotic/abiotic features of the park vary greatly depending on the area of park being studied. The volcanic rock that underlies the

The west coast of North America has been tectonically and volcanically active for billions of years. The Sierra Nevada Mountains in eastern California were born of volcanoes, and magma has been erupting in the Long Valley to the east of the mountains for over three million years (Bailey, et. al., 1989). However, the climactic eruption of the region occurred relatively recently in the region's geologic history. About 760,000 years ago, a huge explosion of magma warped the Eastern Sierra into the landscape that exists today. The eruption depleted a massive magma chamber below the earth's surface so that the ceiling of the chamber imploded, forming what is now known as

headlands and various other wonderful features, being well over 15000 years old this region showcases some magnificent attractions. These regions however are now faced with

Chickasaw National Recreation Area in Sulphur Oklahoma is a place where many families go to escape the hustle and bustle of everyday life. What many may not know is that the waters in this area were a treasured resource even before statehood. Native Americans were the first to speak of the wonderous health benefits of the water and after the arrival of the white man the preservation of this area would become an issue not only for the Native Americans who discovered it but also for the settlers who viewed it as an opportunity to become rich. Acquisition of this land would lead to the founding of Oklahoma’s first and last National Park. Originally named Platt National Park, the birth of this area has given way to years of enjoyment for its patrons, and it has carried in its waters a rich history of Native Americans, the federal government, and a rowdy group of enterprising settlers.

North America is known for having some of the most beautiful national parks. An example of this is Yosemite in California. Though no one can deny the absolute amazing site of Yosemite, it is not the only national park on the west coast that draws in people’s attention. This other national park is called Crater Lake, which is located in Oregon. Crater Lake is one of the most popular places in Oregon. It has as many visitors, up to about 500,000 per year, coming to take a look at the large landscape. This is mostly due to humans turning the large area into a national park in May 22nd, 1902. Crater Lake has evolved from the collapse of a volcano to become a mavourlus national park that has sparked the interest in many visitors.

Lava flows of rhyolite and basalt have flowed through parts of Yellowstone as recently as 70,000 years ago. These lava flows destroyed everything in their paths while moving slowly at a rate of a few hundred feet per day, flowing months, or sometimes even several years. They are thick and cover as much as 130 square miles. They have nearly filled the Yellowstone Caldera, and spilled beyond the caldera’s border. These lava flows are responsible for forming four of the nine named plateaus in

The Lava Beds National Monument is in the border of California and Oregon, which is that too far from here. One of the attractions we will see is a two-mile loop that provides about 20 caves to explore, according to their article. Based on the article is states, “Tourists can explore underground lava tubes that look almost like rocky waterslides. They can also take guided tours of the park, hike along scenic trails, climb cinder cones, and learn about the natural volcanoes and high desert in northern California.” This would be a great experience for many

There are a lot of animal species at the Lava Beds National Monument. At Lava Beds there are 14 species of bats. Mule Deer, Coyote Gopher Snake, Prairie Falcon, Western Meadow Lark, Yellow Bellied Marmot, and Kangaroo Rat are in the grass lands of the Lava Beds National Monument. In the bushlands of the monument, there are Pronghorn, Bobcats, Scrub Jays, Jackrabbits, and Mountain Blue Birds. Mountain Lions, Bald Eagles, and Golden-mantled Groundhogs live in the forest at the Lava Beds. In the rocky lava flows, there are Western Fence Lizards and Western Rattle Snakes. There are Violet-green Swallows, Brazilian Free-tailed Bats, Townsend’s Big-eared Bats, Pacific Tree Frogs, and Pika, in the cave mouths and interior passages. In the lake shore areas of the Lava Beds, there are Skunks, Raccoons, Great Horned Owls, and Short-eared

"Lava Tube, Mojave National Preserve." The Last Adventurer. N.p., 29 May 2014. Web. 04 May 2017. .

Mount St. Helens is an active stratovolcano which is in the Pacific Northwest region of the United States and is located in Washington, Skamania County to be exact. It is a volcano which is very near some major cities including Portland, Oregon and Seattle, Washington. It is in the North American segment of the Pacific called the “Ring of Fire” and this is where the tectonic plates from the “oceanic plate” of the Pacific are forced underneath the “continental plate” of North America.

Students will be in awe of the beauty at Lava Beds National Monument. There are scenic trails that students can explore. Lava Beds National Monument is full of astounding underground caves. Then, one of the most notable features, there are underground lava tubes. According to the article,"Lava Beds National Monument", it states that these lava tubes look like rocky waterslides. This would be the perfect field trip for teaching science. Students who want to be geologists when they grow up would surely love this field trip.

We need to go to the Lava Beds National park because of its volcanic rock and underground caves that have history and geological wonders.It is a secret place and it say that it attracts only about 130,000 people each year.When you enter it has 47,000 -acre park,it also say the visitors can see why president Calvin Coolidge declared Lava Beds a national monument.back in 1925.

If we were to go on this scholastic trip to Lava Bed National Monument, imagine the benefits of it! Students would get to experience a three-dimensional model and outlook on the place. Only benevolent actions could possibly come out of this situation, and to stop the action before it even begins would be dire and unnecessary.

The people in the Medieval times shaped a territory, out of the necessity of solving the problems their ancestors created. The land that became useless and harmful after the turf exploitation, was made suitable for agriculture and living. Throughout time it also was a strategic asset because of the possibility to flood the polder again. Its history is still visible in the territory