Hot Springs - Cook/Lowery15

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HOT SPRINGS
By Hanna D.
MAPS AND LOCATION
Question 1
This is My
park which
is located
in
Arkansas
Maps and Location
Arkansas Hot springs
national park
Hot
Springs
is near
little
rock
Relief map of Acadia national park
Maps and Location Hot springs united states
WHAT YEAR HOT
SPRINGS BECAME A
OFFICIAL NATIONAL
PARK AND WHY
Question 2
Question 2
Hot springs is a United States National park located in
central Garland county Arkansas. Hot springs was originally
established before the concept of a national park even existed. It at
the time was considered a area of recreation. It was established by
the US congress on April 20,1832. Hot springs is the first and oldest
park created by 40 years! The hot spring water has been popularly
believed for centuries to possess medicinal properties, and was a
subject of legend among several Native American tribes. Since Hot
Springs National Park is the oldest park maintained by the National
Park Service, it was rightfully the first to receive its own US quarters
in April 2010 as part of Americas the beautiful coin series.
Bibliography
• N.p., n.d. Web. 6 Dec. 2015.
https://www.lib.utexas.edu/maps/national_parks/hot_springs_map.
jpg
• N.p., n.d. Web. 6 Dec. 2015. https://computerbasicsnationalparksproject.wikispaces.com/file/view/LocMap_Hot_Spring
s_National_Park.png/334988426/385x253/LocMap_Hot_Springs_Na
tional_Park.png
ROCK TYPES
Question 3
Types of Rocks
• Mostly sedimentary but some igneous
• Chert
• Novaculite
• Sandstone
• Shale
Types of Rocks Explained
Shale: Shale is a Sedimentary rock it forms from compaction of clay
and silt and is a mud stone that stands out more because it is
considered “laminated” which means it has thin layers. It looks like
this:
Chert: Chert is also sedimentary and is a form of quartz Chert often
breaks with sharp edges it looks like this:
Types of Rocks Explained 2
Sandstone: Sandstone is one of the most common sedimentary
rocks. It is a mineral made of sand grains that may contain clay or silt
to fill in gaps between sand particles. It looks like this:
Novaculite: Novaculite is a form of chert found in the mountains of
Arkansas and Oklahoma it looks like this:
LANDFORMS
Question 4
Landforms and facts
Facts
• Hot Springs is 5,550 acres
Landforms
• Hot water
• Mountains
• Cascades
• Lakes
Landforms Explains
• Mountains: When 2 plates collide or crash and form what we call
mountains or even sometimes volcano's
• Cascades: A small waterfall
• Hot springs: Small body of water in a stream or current
• Lake: Body of water smaller than a sea or ocean
Bibliography Questions 3&4
• "Hot Springs." NPS: Nature & Science» Geology Resources Division. N.p., n.d. Web. 06
Dec. 2015. http://www.nature.nps.gov/geology/parks/hosp/
• N.d. Shale. Web. 6 Dec. 2015. . Web. 6 Dec. 2015.
http://geology.com/rocks/pictures/shale-colors-380.jpg .
• "Shale." : Sedimentary Rock. N.p., n.d. Web. 06 Dec. 2015.
http://geology.com/rocks/shale.shtml .
• "Chert." : Sedimentary Rock. N.p., n.d. Web. 06 Dec. 2015.
http://geology.com/rocks/chert.shtml
• N.d. Web. 6 Dec. 2015. http://f.tqn.com/y/geology/1/S/r/y/flintnodin.jpg .
Bibliography continued
• N.d. Web. 6 Dec. 2015.
http://www.storeforknowledge.com/Assets/ProductImages/standard/geo-NSALarge.jpg
• Sandstone." : Sedimentary Rock. N.p., n.d. Web. 06 Dec. 2015.
http://geology.com/rocks/sandstone.shtml
• "Novaculite." Wikipedia. Wikimedia Foundation, n.d. Web. 06 Dec. 2015.
https://en.wikipedia.org/wiki/Novaculite
• N.d. Web. 6 Dec. 2015. https://c1.staticflickr.com/9/8746/16734688037_6b52d78fc1_b.jpg
• "Hot Springs National Park - National Geographic." National Geographic. N.p., n.d. Web. 06
Dec. 2015. http://travel.nationalgeographic.com/travel/national-parks/hot-springs-nationalpark/
TECHNOLOGY
Question 5
Technology
• Water
• Baths
• This helps my park because it attracts people and the baths help
water to get filtered
Biblogaphy
• United States. National Park Service. "Hot Springs National Park
(U.S. National Park Service)." National Parks Service. U.S.
Department of the Interior, 22 Dec. 2015. Web. 04 Jan. 2016.
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