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Re: Eclipse Chairs on 2009-11-18
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TTavalea
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Weblogg-ed on 2009-11-13
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Now I’ll be the first to admit that it’s not a perfect question in terms of
trying to get some sense of the personal learning lives from the teachers who
were participating. But in the context of a discussion we’d been having about
the passion-based learning opportunities that the Web now affords, I was hoping
to learn what they wanted to think more deeply about when it came to their own
interests and their own learning. Unfortunately, most of what I got back (on the
first go round at least; I asked them to do it again) was about how to use the
tools in the classroom, and very little about what they wanted to learn about
learining around their own passions with others who share them. -
Now I’ll be the first to admit that
it’s not a perfect question in terms of
trying to get some sense of the
personal learning lives from the teachers who
were participating. But in the
context of a discussion we’d been having about
the passion-based learning
opportunities that the Web now affords, I was hoping
to learn what they wanted to think
more deeply about when it came to their own
interests and their own learning.
Unfortunately, most of what I got back (on the
first go round at least; I asked
them to do it again) was about how to use the
tools in the classroom, and very
little about what they wanted to learn about
learining around their own passions
with others who share them. - 1 more annotations...
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- UWA Library | Scanning the Environment for the Library Strategic Plan 2008 -2010 on 2009-06-01
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MTU Volcanoes Page on 2009-06-01
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Volcano - Wikipedia, the free encyclopedia on 2009-06-01
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A volcano is an opening, or rupture, in a planet's surface or crust, which allows
hot, molten rock, ash, and gases to escape from below the surface. Volcanic
activity involving the extrusion of rock tends to form mountains
or features like mountains over a period of time. The Ancient Romans called
volcanoes Vulcano, after Vulcan,
their fire god.[1]Volcanoes are generally found where tectonic plates are diverging or converging. A
mid-oceanic ridge, for example the Mid-Atlantic
Ridge, has examples of volcanoes caused by divergent tectonic plates pulling apart; the
Pacific Ring
of Fire has examples of volcanoes caused by convergent tectonic plates coming together.
By contrast, volcanoes are usually not created where two tectonic plates slide
past one another. Volcanoes can also form where there is stretching and thinning
of the Earth's crust
(called "non-hotspot intraplate volcanism"), such as in the African Rift
Valley, the Wells Gray-Clearwater volcanic
field and the Rio Grande Rift in North America and the
European Rhine Graben with its
Eifel volcanoes.
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- How Volcanoes Work on 2009-06-01
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How Volcanoes Work on 2009-06-01
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This website is an educational resource that describes
the science behind volcanoes and volcanic processes. The site is sponsored by
NASA under the auspices of Project ALERT (Augmented Learning Environment and Renewable
Teaching). It is intended for the education of university students of
geology and volcanology and teachers of earth science. Each section in the menu
builds upon previous sections. For users who lack fundamental knowledge of
volcanological principles and terms, it is best to proceed through the website
in a progressive manner. More advanced users will find each section
self-contained and can navigate through the website as their interest
dictates.
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- Volcanoes Online on 2009-06-01
- Global warming - Wikipedia, the free encyclopedia on 2009-06-01
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Online curriculum centre on 2009-06-01
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The Diploma Programme
The International Baccalaureate (IB) Diploma Programme is a
challenging two-year curriculum, primarily aimed at students aged 16 to 19. It
leads to a qualification that is widely recognized by the world’s leading
universities. More information about the Diploma Programme can be found on the IB public
website.
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