Shoofly oolite idaho code#

There is a possibility it was derived from a Native American phrase. There is some ambiguity as to where the name 'Idaho' came from, but it is generally believed to have simply been made up by George M. Idaho also hosts the largest barrel cheese factory in the world, producing 120K metric tons of cheese per year. Idaho is also famous for producing about one third of all potatoes grown in the USA. Idaho is nicknamed 'The Gem State' because nearly every known gemstone is found within the state. Idaho is landlocked, being bordered by Canada on the north and the states of Washington and Oregon on the west, Nevada and Utah on the south and Montana and Wyoming on the east. Idaho was the 43rd state to be admitted into the Union, on July 3, 1890. Idaho is the 14th largest state by area, ranks 39th by population and 53rd by population density of the 50 United States. We from the League wish you all the best.Idaho is a state located in the northwestern region of the United States of America. We won't respond unless you send incorrect answers.

Shoofly oolite idaho code#

Begin your email with the name and geocaching code of this Earthcache, your name(s), and the number of people in your group.Ĥ. Your logging this cache and sending us the email should happen at around the same time.ģ. You must answer all the questions in your email to us.Ģ. It is not required but if you would like to post a picture of the area or yourself at the location feel free.ġ. How thick is the banding and how high do you estimate it to be?ģ. Send us an email with answers to these questions:ġ. If health does not permit you will be able to see many formations and inspect shoofly oolite from the parking area. Visitors may park in the parking area near the coordinates. Hiking is allowed in side the fenced area. The five acre enclosure secures the oolite formations and small hills. In some places, the exposed oolite has been sculpted into hummocks, small arches or other intriguing shapes, forming a natural sculpture garden. Small deposits are exposed here and there across the 40 miles that separate the flats and the town of Murphy. Siltstone forms the stratum immediately above it.Īfter Lake Idaho drained, erosion carried away softer sediments but left the more resistant oolite to weather above the mud flats. Sea water is more likely to have the necessary wave action, and saltier lakes the proper chemistry.īeach sands of varying thickness underlie the oolite.

The Shoofly Oolite is unique because it formed in fresh water. Wave action in Lake Idaho that varied with the seasons, the weather and the type of sediment in the water at the time washed the ooids back and forth in the shallows, depositing them in thicknesses of 2 to 40 feet on the steeper benches near the shores. Ooids form when calcium carbonate precipitates around individual grains of sand. The oolite on the Mud Flat, known as the Shoofly Oolite, is part of the Glenns Ferry Formation and one of the world's largest freshwater oolites. The tiny round pieces of limestone found on the Flat are called ooids, known as oolite ('egg stone') when deposited in larger formations.

They form the deep sandy slopes and ridges that plants like Mulford's milkvetch need to grow and which are found in only in three areas of Idaho: the Owyhee Front, the Boise Foothills and the area around Weiser, ID. Sediments left behind became the Chalk Hills and Glenns Ferry Formations. Geologists think water from melting glaciers caused Lake Idaho to overflow to the west in a massive flood that gouged Hell's Canyon, along the present-day Idaho-Oregon border. The earth's crust began to be pulled apart, northeast to southwest, stretched thin like taffy, and the Owyhee Mountains and the Boise Front rose along faults bordering the rift, reaching their present heights during the Neogene Period. Extending across southwestern Idaho between the Owyhee Mountains and the Boise Front is the broad valley of the western Snake River Plain, which evidence indicates began as a continental rift.