Article posted April 19, 2012 at 04:27 PM GMT0 •
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I have two bottles that I have sent a picture of. One of the bottles I have is the clear one. It is from 1934. Its selling time was from 1929-1943 this was a pure cider vinegar bottle. The brown one I would like to know more about and about the National Disstillers on the top. That’s what I want to know more about. My dad found these up at an old logging site in northern Minnesota.
Article posted April 19, 2012 at 04:27 PM GMT0 •
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Article posted February 6, 2012 at 06:26 PM GMT0 •
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We got to have fun. I found out how to be a good friend. People were nice to me. we thought of problems in our school and how to fix it. And it was a full day of kindness.
Article posted February 6, 2012 at 06:26 PM GMT0 •
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Article posted January 24, 2012 at 06:35 PM GMT0 •
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It must have been hard to be ruled by britan especially because its a different country and have wars and then get taxed by them but it was brave to fight for somthing you belive in
Article posted January 24, 2012 at 06:35 PM GMT0 •
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Article posted December 15, 2011 at 05:24 PM GMT0 •
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There are three main types of fault that may cause an earthquake: normal, reverse (thrust) and strike-slip. Normal and reverse faulting are examples of dip-slip, where the displacement along the fault is in the direction of dip and movement on them involves a vertical component. Normal faults occur mainly in areas where the crust is being extended such as a divergent boundary. Reverse faults occur in areas where the crust is being shortened such as at a convergent boundary. Strike-slip faults are steep structures where the two sides of the fault slip horizontally past each other; transform boundaries are a particular type of strike-slip fault. Many earthquakes are caused by movement on faults that have components of both dip-slip and strike-slip; this is known as oblique slip.
Reverse faults, particularly those along convergent plate boundaries are associated with the most powerful earthquakes, including almost all of those of magnitude 8 or more. Strike-slip faults, particularly continental transforms can produce major earthquakes up to about magnitude 8. Earthquakes associated with normal faults are generally less than magnitude 7.
This is so because the energy released in an earthquake, and thus its magnitude, is proportional to the area of the fault that ruptures[3] and the stress drop. Therefore, the longer the length and the wider the width of the faulted area, the larger the resulting magnitude. The topmost, brittle part of the Earth’s crust, and the cool slabs of the tectonic plates that are descending down into the hot mantle, are the only parts of our planet which can store elastic energy and release it in fault ruptures. Rocks hotter than about 300 degrees Celsius flow in response to stress, they do not rupture in earthquakes.[4][5] The maximum observed lengths of ruptures and mapped faults, which may break in one go are approximately 1000 km. Examples are the earthquakes in Chile, 1960; Alaska, 1957; Sumatra, 2004, all in subduction zones. The longest earthquake ruptures on strike-slip faults, like the San Andreas Fault (1857, 1906), the North Anatolian Fault in Turkey (1939) and the Denali Fault in Alaska (2002), are about half to one third as long as the lengths along subducting plate margins, and those along normal faults are even shorter.
Article posted December 15, 2011 at 05:24 PM GMT0 •
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Article posted September 30, 2011 at 03:07 AM GMT0 •
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the british came to America . they grew crops such as fruits and vegtables . the indians taught them how to grow corn . they had to trust them that he taught them well.the could not quit otherwise they would die.one day the cheif went to scout or explore .In the front of the colony they had a defense system .their were no phone back then but you did not need it because you were able to walk to who you to talk to house.they were were brave to come here and start new civilization
Article posted September 30, 2011 at 03:07 AM GMT0 •
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Article posted September 28, 2011 at 08:14 PM GMT0 •
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My weathering park shows the three forces of weathering they are wind water and temperature see if you can find the examples of weathering.
In the park there was a tall statue with really seeable hieroglyphics.
It starts to rain water can ware away rock.
Now the statue is still as tall as before but the hieroglyphics are hard to see .
My weathering park window shows how different forces broke down the statue . it did this with rain weathering is a powerful agent that changes the earths surface
Article posted September 28, 2011 at 08:14 PM GMT0 •
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