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GC1E7PB

EarthcacheSudbury Astrobleme!

A cache by The Mighty Canadian Juicepig     Hidden: 7/15/2008

Size: Size: Not chosen (Not chosen)     Difficulty: 2 out of 5     Terrain: 3.5 out of 5 (1 is easiest, 5 is hardest)


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N/S ? ??.??? W/E ??? ??.??? 
In Ontario, Canada

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1.85 billion years ago, this was not a friendly place. Welcome to the crater rim of the second largest confirmed impact crater on earth.
The Sudbury Basin was created 1.85 Billion years ago when a 10km wide spacerock travelling 75 kilometers per second, gently nudged the area, causing this 250km wide crater, that was at one point 15-20km deep. Magma from the earths mantle filled the crater, creating the rich mineral deposits of Nickle, Copper, Platinum, Palladium, Aluminum and gold that Sudbury is best known for.

Astrobleme : "Star Wound", an ancient weathered impact structure

The impact was thought to be equivalent to 10 Billion Hiroshima Bombs, vaporizing the asteriod, and melting a large swath of the Canadian shield. Debris from the impact was spread over an area of 1.6 million square kilometers, and flung over 800 kilometers from the impact. If a similar incident were to happen today, the impact would instantly destroy all people, places and things within 800km of the impact, cause the earths atmosphere to be flooded with several thousand cubic miles of volcanic gas, sulpher, Carbon Dioxide and Monoxide, before igniting and wiping clean the entire continent in a bath of fire.

The impact crater is much smaller today (roughly 60km long, and 30 km wide). After 1.85 billion years of erosion, mountain building, a few hundred ice ages, and other natural events only the north-west rim of the crater remains fully intact. The formation of the Grenville and LaCloche mountains to the south pushed the southern rim of the crater northward, giving the crater and Oval shape. A subsequent meteorite impact 35 million years ago deformed the north-east section of the ridge - creating Lake Wanepeti.



On the eastern side of the Sudbury Astrobleme is the Wanapitei impactor site - Another impact crater left by a much smaller impact only 37 million years ago. Local myths suggest that the lake is actually bottomless, but renowned oceanographer Jacques Cousteau determined that was not the case in various case studies of the odd lake. Contained within the lake is a gravitational anomaly called the Temagami Magnetic Anomaly, that generates a magnitude of over ten thousand nanoteslas - making it the strongest magnetic anomaly in North America. Some geologists believe the anomaly to be the original Wanepeti meteorite, while others believe it to be unrelated. One of many unanswered geology questions about the area.

The Sudbury Astrobleme is the second largest crater verified impact site on earth after the "Vredefort" in South Africa. It is larger then the much younger 3rd place contender "Chicxulub", the Dinosaur Killer in Yucatan Mexico.

Today the remenants of this impact run a 3 billion dollar a year mining industry in the area, producing over 900 million kilograms of Nickel, more then 10% of the world's consumption.

TO LOG THIS CACHE

Go to the Coordinates listed above. You will find a parking lot with many different types of stones, minerals and metal ores, with a description of how they were formed. Use the trail to travel down into the "High falls" area, and locate a "Wild" rock (there are plenty to choose from)

Take a picture of this "wild" rock, then identify it using the plaques and examples in the parking lot.

Your found log will need to contain:
- A picture of the "wild" rock (a rock in the wild) and coordinates
- A picture of the "captive" rock (a rock with a plaque in the parking lot)
- A brief description of what the rock is, use your own words! The plaque will help you with this, just put it into simple terms!

 


1 user(s) watching this cache.

Inventory Inventory

Additional Hints (No hints available.)

(Decrypted Hints)

Find...

Impact!

Onaping High Falls

Plenty of rocks down there!!
Sudbury and Wanepeti

Sudbury and Wanepeti (small)

Logged Visits (16 total. Visit the Gallery (39 images))

Found it15     Publish Listing1     

Warning. Spoilers may be included in the descriptions or links.
Cache find counts are based on the last time the page generated.

 September 5, 2009 by maddy82 (676 found)
My husband and I are visiting from Ottawa and we really enjoyed seeing this area. We found a "wild" quartzite rock. We learned that the silica in the rock is was used in the smelter at Copper Cliff and Coniston instead of sand. This reduced the volume of slag produced and thus lowered the metal lost by the slag.

View This Log
Photo Captive Quartzite
Photo Wild Quartzite

 August 22, 2009 by lynnandpeter (85 found)
I found this cash after a day of cashing. The captive rock reduced the volume of slag produced and lowered the slag metal loss content. My kid had alot fun!!!

View This Log
Photo Captive rock 2
Photo Captive rock
Photo Wild rock

 August 22, 2009 by juliendon (229 found)
found this one after doing my longest bushwack cache . my captive rock was used to help reduce the amount of slag produced and and lowered the slag content

View This Log
Photo wild rock
Photo captive rock

 August 4, 2009 by TeamTrail (135 found)
We found our wild rock located at N46 35.414 W081 22.888 and is "Onaping Formation", fall back breccia from a meteorite impact.

Always great to stop and view the falls.

TFTC

View This Log

Photo Captive Rock Close Up
Photo Wild Rock

 August 4, 2009 by TEAM BULLSGUT (440 found)
My wild rock found at N46 35.378 W081 22.884 I identified as quartzite. This silica rock is said to help reduce the amount of slag produced in the smelting process

View This Log
Photo quartzite captured
Photo quartzite wild

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Current Time: 2/9/2010 10:25:59 PM (GMT-08:00) Pacific Time (US & Canada) (6:25 AM GMT)
Last Updated: 9/5/2009 4:25:56 PM Pacific Daylight Time (11:25 PM GMT)
Rendered: From Database
Coordinates are in the WGS84 datum


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