Lake Taupo

Introduction In this report, I will be explaining two surface features which are visually interesting to geologists and tourists in the Taupo Volcanic Zone (TVZ), Lake Taupo, and Mt Ruapehu. Lake Taupo is a main tourist attraction as it is the largest lake in New Zealand with a beautiful scenery perfect for activities like recreational fishing and sky diving. Furthermore, it generates electrical energy via the Waikato river that is used by people all around waikato. Mt Ruapehu is also a tourist

Undulating volcanic plateau. Parent material- Rhyolitic rock Question 2 – Soil types Describe the main soil characteristics for the region including their soil texture, depth, plant available water and drainage. Soil texture- The soil around the Taupo area is a sandy loam which is normally made up of sand along with varying amounts of silt and clay. Soil depth- greater than one meter. Plant available water- the profile of available water for soil depth of 0-100cm or to the root barrier is very high

Task: 1 Locational Context Tongariro National Park is located in the North Island of New Zealand, south of Lake Taupo. The reference points are: • Between 39 degrees and 39.5 degrees South of the equators • Between 50 – 100km from the sea • Between 500 and 2700m above sea level • In the centre of the North Island of New Zealand (page 5, Natural Landscapes, Year 12 notes) 1. Map of New Zealand, North Island The Park is home to two large volcanoes and one parasitic volcano, Mt Ruapehu

Lake Bridgeport was built in 1930 for flood control, water storage and recreation. Tarrant County owns the land and water that makes the lake. There is a spillway that takes water through the Trinity River to Eagle Mountain Lake and Lake Worth. This year has been a rough year for Lake Bridgeport with three digit temperatures and draining water to the other lakes. Since one of the purposes to build Lake Bridgeport was for storage, The Tarrant County water district approved to let out 20,000 acre feet

to December, 2011) of the biomanipulation work done in the lake Nainital for its ecosystem restoration is presented in this paper. In this approach we attempted to manipulate various levels of the food chain, assuming that the nutrient input is stable and cannot be reduced to limit the primary production. At the start of the work important physico- chemical and biological parameters were measured to know the present scenario of the lake. Among physico- chemical parameters the water temperature,

Introduction: Water is not only a necessity to our everyday lives, but it also serves as an important component when it comes to recreation. Knowing how to manage a lake or reservoir for these different aspects is a key ingredient to satisfying our human needs; for survival as well as leisure. Because less than 1% of all water on Earth is safe for humans to drink, it is crucial that these waters be carefully managed to sustain current and future generations. Water-based recreation, such as fishing

concern on the subject today is water contamination. Individuals grew worried that the chemicals used to gather these natural resources will seep into the water and contaminate the United States. The water necessary to frack is gathered from rivers, lakes, ponds, and even aquifers. This is then combined with chemicals and pumped into the ground. Fracking was exempted from the Federal Safe Drinking Water Act and the chemicals used to frack are not tested frequently in our water (Lampe 34). Bordering

which is produced by blue-green algae. When fertilizers and human sewage run into rivers and lakes, these toxins start to appear because nutrients are added that cause the growth of algae known as “super blooms”. However, sea otters don’t go to the areas these blooms occur in like polluted rivers and lakes. Miller then did some research and found that super blooms occurred frequently in a lake, Pinto Lake, that eventually drains into the area of the Pacific Ocean where the dead otters were found

Figure 1. The zones of a freshwater lake (Smith and Smith 2001). Within the lentic ecosystems, temperature plays a crucial role. Lake temperatures does not variate drastically, but does change gradually with every season of the year. Summer, the thermic stratification of lakes, can be studied in different layers (Figure 2). The superior level of a lake that is terminally stratified, is known to be epilimnion, which is the warmer part of the fresh water body. This water remains in the superior part

down, scorching my pale flesh, but I don’t feel it. Fear augments inside me; unsure my limits, I persist. The lake gleamed in the bright mountain sunshine, which would have been warm if not for the breeze, yet all the campers are still full of joy. All except me. I stripp off my towel, revealing my pale, goose-bump ridden skin and a thin black bathing suit. My mom is staring out at the lake, the shining sun hitting her sunscreen smudged face, looking chipper, she reaches down, to pet the dorkus, fuzzy