Waimangu Volcanic Valley is one of the newest attractions in the area of Rotura, a city near the center of the North Island of New Zealand. It’s discovery.

Slides:



Advertisements
Similar presentations
Archipelago: A large group of islands
Advertisements

What? Where? Why? How? Who?. What are we learning today? Waterfalls: How do differences in rock hardness affect them? What are the main features / parts.
The drive from Christchurch, on the eastern edge of the South Island of New Zealand, to Lake Wanaka, where we stayed, was a pleasant one. Heres a shot.
Milford Sound was everything we had heard: massive, impressive, gorgeous. Formed thousands of years ago, the sound is really a fjord (which means its massive.
Tundra a biome where the tree growth is hindered by low temperatures and short growing seasons. 
Unit C Chapter 6 Lesson 1 C6 – C11
Geography of Ancient Egypt
As we approached Lake Wanaka, we crossed this nice bridge over a fast moving river.
Water Underground S6E3 Students will recognize the significant role of water in Earth processes. S6E3.a Explain that a large portion of the Earth’s.
The first sight that Judy and I took in when we drove down from Auckland, the capital of New Zealand, to the Lake Taupo area, was “Huka Falls.” Just north.
Bob and Judy Russell conquer “Preikestolen” in Norway (May 2004) Bob and Judy Russell conquer “Preikestolen” in Norway (May 2004)
Learning About Landforms
Geography Picture Dictionary One
In the small town of Waitamo, where the tour bus to the Glow Worm Caves gathered us up, there were nice Agapanthus growing everywhere.
GEO-BOWL All Grades “We play mind games.” This part of a map tells what the map is about. Title.
Section 7.2 Erosion and Deposition Objectives
Mr. Ramsey 6th grade Social Studies Licking Heights Central
AFRICA ANTARCTICA ASIA OCEANIA EUROPE N AMERICA S AMERICA ARCTIC ATLANTIC INDIAN PACIFIC SOUTHERN.
They Could Still Be Mountains. You can see why these mountains are called the Rocky Mountains. They have steep sides of bare, jagged rock, rising to sharp.
Yellowstone Supervolcano By: Jackson Smith
The Caribbean: Physical Environment. Climate in nice most of the year, although rainy from May to November Trade winds – blow from east across the Atlantic.
Investigation: Plants Station 2: Food Bulbs 1)What is the function of a food bulb?_____________________________________________________ 2) How are plants.
Earth’s Layers 6.E.2 Notes. Anatomy of Earth Crust Mantle Outer Core Inner Core.
Do you know what’s going on in Timpanogos Caves? By: Diantha Smith, 2009 Cave Basics.
Earth’s Features.
Chapter 5 Lessons 1 – 3 Chapter 6 Lesson 1, 2
Bellringer Describe the relationship between the silica content of magma and the resulting eruption of the volcano.
Our Changing Earth The Earth is made up of different kinds of materials, including rocks. Soil, water, and the gases of the atmosphere. Soils have different.
Rocks. Three Types of rock Igneous Metamorphic Sedimentary Three totally different types of rock that all basically come from the same materials.
FRESHWATER CHAPTER 10 PG Section 1: Water on Earth Pg. 314.
Physical Geography of Sub-Saharan Africa
Work and Energy  Energy is the ability to do work or cause change.  Two Types of Energy: Potential Energy = energy that is stored in an object due to.
Mount St. Helens April 10, On March 20, 1980, after a quiet period of 123 years, earthquake activity once again began under Mt. St. Helens. March.
Changes Within the Earth 1-2. I. Physical Characteristics  A. The Earth’s Layers  1. Core – center of the earth consisting of very hot metal (mainly.
First Grade Science and Social Studies
Volcanoes C Volcano A mountain formed when red-hot melted rock flows through a crack onto the earth’s surface A mountain formed when red-hot melted.
Sub-Sahara Africa Geography Landscapes © 2010 TESCCC 6 th Grade Social Studies, Unit 5, Lesson 1 Africa.
Physical Geography of the United States and Canada.
Lake Wanaka is a cold, clear lake in a valley surrounded by some nice mountains. The city by the same name is one of the main tourist areas on the South.
Photo Project Created By: Drew Deerman. Tranquil Thoughts.
Bodies of Water and Landforms. Oceans Large bodies of SALT water the surround a continent. Large bodies of SALT water the surround a continent.
Glossary. climate the weather conditions of a particular place or region over the four seasons of the year.
Landforms Any natural feature of the earth's surface.
A wall built across a river creating a lake that stores water.
Dam -A wall built across a river, creating a lake that stores water. Page 2.
Plateau A high, flat area that rises steeply above the surrounding land. 1.
How Volcanic Activity Shapes Earth
Glaciers. Geologists define a glacier as any large mass of ice that moves slowly over land. There are two types of glaciers: Continental glaciers Valley.
Hi, my name is Charlotte Shale. I am a Sedimentary rock called Shale, as you can see by my name. I live in Yellowstone. It is a great place to live as.
One day, while Judy rested, Bob checked out the “Craters of the Moon” just outside Lake Taupo. This was another geothermal area to explore.
Plate Tectonics 8th Science.
Atmosphere 0.002% Ocean 97.2% Ice caps & glaciers 2% biosphere Rivers, lakes 0.6% Underground- lithosphere I P Et S E+C.
Land and Water By Cathy Wharmby Fall Landforms What are landforms? A kind of land with a special shape.
Changes to the Earth’s Surface: Erosion
To get out of the city for a day, we drove our little Honda over what is called the “Great Ocean Road.” We explored the area west of Melbourne for about.
Christchurch (far right) is located in the southern part of New Zealand’s South Island. A major city, it is nestled among mountains and on the edge of.
New York State Landforms. New York is about 300 miles wide and 300 miles tall. New York is full of LANDFORMS! Landforms are the natural shapes we see.
Deserts. Dazzling Desert An area of land that receives less than ten inches of rainfall a year. Take a look outside. What is it like where you live? You.
Land. Here are some pretty hills. It takes a long time to hike (or walk) up a hill.
Geographic Regions of the US. Coastal Plain The first region is the Coastal Plains region. This region is along the Atlantic Ocean and Gulf of Mexico.
Yellowstone National Park Xavier Brodie, Valorie Henderson, Rixi Sandoval, Corey Williams tional-parks/yellowstone-national-park/
Peggy Young 2 nd Grade sofland/typesofland.html.
Why Did the Sheep Cross the Road?. High, in the Rocky Mountains of Colorado, live beautiful sheep called bighorn sheep. 1.
Unit 1 Lesson 2 New Jersey’s Natural Regions pgs
My Geography Book By.
- define ecosystems and biomes
Fresh Water.
beach cliff coast mountain forest ocean river sea valley vegetation
Heat.
Lively urban city just to the distance vast towers so full of busy people and just a step away is the great nature along with a scenery of the wondrous.
Presentation transcript:

Waimangu Volcanic Valley is one of the newest attractions in the area of Rotura, a city near the center of the North Island of New Zealand. It’s discovery revealed even more volcanic activity in the midst of a lush valley full of vegetation. The wooden carving stems from the Maori culture.

Just as we drove up to the valley, this pretty (unidentified) bird flew near us and began to look for seeds from a pretty (but unidentified) plant.

The Valley is full of very dense plant growth—mostly palms, but other bushes and trees. Hidden in this growth, about a half mile away, is the volcanic activity. Note the lush pine trees on the far horizon, outside the thermal area.

Along our walk, we glimpsed a flowing river and areas of steaming, rocky “slag” created by the hot steam coming up from underground.

As we crested a hill, we saw “Frying Pan” Lake at the bottom of the valley. The lake sits on top of cracks in the earth—and steams continuously with hot water.

Frying Pan Lake is somewhere between 140 degrees (near the surface) to even hotter water (near the bottom). Around the edges of the lake, sulfur residue floats on top.

At the edge of Frying Pan Lake (upper left, out of view), there is a huge cliff of steaming rock. The lake then flows out into a stinky, hot yellow- green mixture.

Every so often, we would see boiling cauldrons, with crusty sulfur crystals forming as the water runs down the higher rock mound.

The area around the bubbling holes in the ground was solid, but neither of us wanted to test the strength by walking across the crystallized area.

Once in awhile, the water would come out of the ground “clear.” Made us want to make soup. Well, perhaps not.

While Judy rested, Bob climbed about 100 stairs, up over a crest— and discovered this gorgeous, aquamarine-colored lake. The lake rises and falls as the seasons change and, yes, it was hot—but not nearly as hot as Frying Pan Lake.

Perched on one of the hills in the valley, not far from Frying Pan Lake, was a cross. It was placed there to commemorate where some hapless tourists strayed a little far from the path and were scalded to death. We stayed on all paths!

Bob and Judy stand by Frying Pan Lake—it was a gorgeous (albeit HOT) day for a nice walk in the interesting Waimangu Volcanic Valley.