Lava Beds National Monument Analysis

One summer my parents informed my brother Ben and I we were going on a trip to Yellowstone National Park. I had never been so excited for anything in my life. I had a passion and love for nature, and being that Yellowstone had some of the most beautiful and interesting geological features on Earth, I knew I would have a blast. They said we would be going in a few weeks, and I literally couldn’t wait. I kept asking questions upon questions, and finally, my dad just got annoyed. “Go research it, Juliette.” He said. “The internet will know more than I do.” I took his advice and went to research Yellowstone.

Powerful forces of the earth cause a landmass to slide under the water. The hot water from the floor of the ocean then melted the rock from the land, forming granite rocks (U.S. Department of the Interior). Mesozoic volcanic and sedimentary rock are scattered through Sierra Nevada Batholith, which covered most of the park during the Jurassic and Cretaceous times (Harris). Weathering and the batholithic makeup impact the exterior of the landforms within these national parks. Yosemite National Park has a very similar geological history compared to the Sequoia and King Canyon National parks, due to the fact that they all lie in the Sierra Nevada’s peak and western slopes (Harris). When it comes to lithospheric extension in the Death Valley Region, during the time of rapid growth, the plates in this region rapidly expanded. In the region of the Sequoia and King Canyon national park the plates did not expand rapidly, thus indicating that more extension occurred in the Sequoia and Kings Canyon region (Jones). Under the surface, there are many marble caves that are endemic to the area (U.S. Department of the Interior). It is clear that natural forces like these have the ability to create beautiful and interesting geology. The description of the tectonic plates would be an ocean continent subduction zone (U.S. Department of the Interior | U.S. Geological Survey). This occurs because of the above process. A specific rock located in the national park is the Moro Rock. Moro rock is a large granite rock that is shaped like a dome. It was made by the process of exfoliation that has to do with the layers of granite expanding over time (U.S. Department of the Interior | U.S. Geological Survey). The exfoliation process creates many of the rock features located in the park. This exfoliation process is the same one that creates many of

the volcano and the areas ecology - learning about things science has not had the chance to

According to chapter 49 in Geology of National Parks, rocks in these parks mainly consists of some metavolcanic rocks, early Mesozoic metasedimentary along with batholiths made of granite from the Cretaceous period. Also, glacial sediments cover the bedrock in deep valleys and at high elevations. There are also avalanche cutes on the west side of Mount Whitney in the Sequoia National Park which occurs after an avalanche carrying trees, ice, even trees moves down a steep slope leaving behind a smooth path(pg.742). Most of the preexisting rocks in the Sierra Nevada area were destroyed the batholith intrusions, but separate granite intrusion separate curtains or sheets of metamorphic rock called roof pendants which can be found in both the Sequoia and Kings Canyon National Parks. According to the article, “Geology of the Sierra Nevada,” these batholiths are what remains from ancient volcanoes, and the intrusive igneous rocks form underground as the minerals in the molten rock cools down slowly.

There was once a President that was named Calvin Coolidge that declared the lava beds a national monument in 1925 the landscape in the park was covered in lava. All of the underground caves and lava tubes were formed by the lava eruption that cause it to stay like that.

How can you get Fort McHenry, Sutter's Mill, Minute Man National Park, Independence National Historical Park, Ellis Island National Monument, Manzanar National Historic Site, Fort Sumter National Monument, Edison National Historical Park, Death Valley National Park, Yorktown National Historical Park, Valley Forge National Historical Park, Appomattox Courthouse National Historical Park, Golden Spike National Historic Site, The Alamo Brown v. Board of Education National Historic Site, and Fort Clatsop National Historical Park all into one classroom in Oregon? Even more challenging, the classroom is located in a juvenile detention facility so the students will not be making any site visits. . There are photos and websites, traveling trunks and lesson

The Raton-Clayton volcanic field is about 20 000 km2 in size, and has been active periodically for the past 9 million years. The area is filled with peaks, cones, and lava-capped mesas. The mesas developed as lava flowed into valleys and depressions, cooled off and formed a resistant top layer over sedimentary rocks. As the surrounding rock eroded, the lava protected the underlying stratigraphy from erosion. This caused todays topography, where that which was once the lowest point, is now the highest. There is some disagreement over why the volcanic field is here, one possible cause is that it is near the end of the Jemez Lineament, which has numerous volcanic centers along its reach, possibly

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 canyon is free to visit with plenty of parking and public facilities. There is an accessible path that leads to the scenic lookout. Camping, off-roading, and rock climbing are currently forbidden.

A loud morning for some residents in small Mexican as villages, as clouds of ash and smoke shield the sun, and mandatory evacuations are in full effect. Hundreds have been moved from their homes for fear that the small eruption from an active Mexican could escalate into a much larger event, which could endanger lives on a much larger scale.

Would you ever like to go to a special, amazing, extraordinary field trip? If so then what was it. Have you ever heard of six flags, it is a water park that has all type of slides, roller coasters and more? Well six flags are one of the field trips that I would want to go to. Many teachers argue that the field trips are not educational, but I argue that six flags has many educational things.

For my UTEP event I went to the fossil and rock exhibit. Although I was limited to only a few exhibits, those exhibits were very interesting. Some of the exhibits that I saw were the rock, fossil and history exhibits. The one I found most interesting was the rock exhibit. This exhibit was made up of rocks found in this general area (El Paso New Mexico and Mexico). It had a wide range of rocks from crystals to quarts to obsidian rocks. The one I found most beautiful was the Calcite crystal. This crystal was from Durango Mexico and it almost looks like a white rose. This experience for me was very educational. I learned many things like, how the pressure on a rock can affect the way it looks and feels. I also learned that at one point El Paso

The active volcano that I chose to research is Popocatepetl volcano. Popocatepetl volcano is an active volcano located in Mexico. The volcano is oftentimes referred to as “El Popo” by many Mexicans. El Popo is a composite cone volcano. Being a composite cone volcano, El Popo is characterized by a steep cone shape, which was created by many composite layers of material pouring out over numerous eruptions. The lava that comes out of El Popo is extremely viscous. The highly viscous lava does not travel very far, and typically cools down rapidly. Scientists believe that El Popo is about 730,000 years old. It has erupted more than 15 times since 1519. In 1994 El Popo produced gas and ash, which caused nearby towns to evacuate. The toxic

It is called Yosemite National Park. Yosemite National Park attracts 4 million people annually, which is another reason why Lava Bed National Monument does not attract as many tourists. The national monument is a great place to take us on a field trip, because it has a profusion of things to wander at. I am sure that all the eighth grade students would love to go to Lava Bed National Monument. It would also be like a science field trip too, because our science teacher could teach us about the natural volcanoes at the huge national monument. I think many students would be excited to wander in the dark caves, because they might find a huge variety of things they never seen before. I bet that many of the students would have an astonishing look on their faces. The Lava Bed National Monument would be a substantial experience for

To this end we organize a range of field trips that include visits to museums, zoos, botanical gardens, and historic buildings. While each of these trips includes a curriculum that we follow to ensure that each child is learning important information, each fieldtrip is also planned with the idea of encouraging creative endeavors, so a trip to an historical cemetery might be followed by our participants putting on a play in which they dress up as important figures from local history. Such projects help children learn, make new