The Book of the National ParksYard, Robert Sterling
History
The Book of the National Parks
Yard, Robert Sterling
National parks and reserves -- United States
| | |
Hawaii, 1916 | Hawaiian Islands| 118 | Three separate volcanic
| | | areas--Kilauea and Mauna Loa on
| | | Hawaii; Haleakala on Maui.
| | |
Lassen Volcanic| Northern | 124 | Only active volcano in United
1916 | California | | States proper--Lassen Peak
| | | 10,465 feet--Cinder Cone 6,879
| | | feet--Hot springs--Mud geysers.
| | |
Mount McKinley,| South central | 2,200 | Highest mountain in North
1917 | Alaska | | America--Rises higher above
| | | surrounding country than any
| | | other mountain in world.
| | |
Grand Canyon, | North central | 958 | The greatest example of erosion
1919 | Arizona | | and the most sublime spectacle
| | | in the world--One mile deep and
| | | eight to twelve miles
| | | wide--Brilliantly colored.
| | |
Lafayette, 1919| Maine Coast | 8 | The group of granite mountains
| | | on Mount Desert Island.
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Another distinction which should be made is the difference between a
national park and a national monument. The one is an area of size
created by Congress upon the assumption that it is a supreme example of
its kind and with the purpose of developing it for public occupancy and
enjoyment. The other is made by presidential proclamation to conserve an
area or object which is historically, ethnologically, or scientifically
important. Size is not considered, and development is not contemplated.
The distinction is often lost in practice. Casa Grande is essentially a
national monument, but had the status of a national park until 1918. The
Grand Canyon, from every point of view a national park, was created a
national monument and remained such until 1919.
THE GRANITE NATIONAL PARKS
GRANITE'S PART IN SCENERY
The granite national parks are Yosemite, Sequoia, including the proposed
Roosevelt Park, General Grant, Rocky Mountain, and Mount McKinley.
Granite, as its name denotes, is granular in texture and appearance. It
is crystalline, which means that it is imperfectly crystallized. It is
composed of quartz, feldspar, and mica in varying proportions, and
includes several common varieties which mineralogists distinguish
scientifically by separate names.
Public-domain text, read in full here on John Shaqi.
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