School History of North Carolina : from 1584 to the present timeMoore, John W. (John Wheeler)
History
School History of North Carolina : from 1584 to the present time
Moore, John W. (John Wheeler)
North Carolina -- History
The Appendix contains the present "Constitution of North Carolina."
Then follows a series of "Questions on the Constitution," prepared
expressly for this work by Hon. Kemp P. Battle, LL. D., President
of the University of North Carolina. This is an entirely new and
valuable feature in a school book, and contains an analysis of our
State government. This is just the information that every citizen of
North Carolina ought to possess, and teachers should require all
their students of this history to read and study the Constitution
and endeavor to answer the questions thereon.
No State in the Union possesses a record of nobler achievements
than North Carolina. Her people have always loved liberty for
themselves, and they offered the same priceless boon to all who
came within her borders; and it was a full knowledge of this
trait of our people which made Bancroft say "North Carolina was
settled by the freest of the free."
CHAPTER I.
PHYSICAL DESCRIPTION OF NORTH CAROLINA.
The State of North Carolina is included between the parallels
34° and 362° north latitude, and between the meridians 752° and
842° west longitude. Its western boundary is the crest of the
Smoky Mountains, which, with the Blue Ridge, forms a part of the
great Appalachian system, extending almost from the mouth of the
St. Lawrence to the Gulf of Mexico; its eastern is the Atlantic
Ocean. Its mean breadth from north to south is about one hundred
miles; its extreme breadth is one hundred and eighty-eight miles.
The extreme length of the State from east to west is five hundred
miles. The area embraced within its boundaries is fifty-two
thousand two hundred and eighty-six square miles.
2. The climate of North Carolina is mild and equable. This is
due in part to its geographical position; midway, as it were,
between the northern and southern limits of the Union. Two other
causes concur to modify it; the one, the lofty Appalachian chain,
which forms, to some extent, a shield from the bleak winds of the
northwest; the other, the softening influence of the Gulf Stream,
the current of which sweeps along near its shores.
3. The result of these combined causes is shown in the character
of the seasons. Fogs are almost unknown; frosts occur not until
the middle of October; ice rarely forms of a sufficient thickness
to be gathered; snows are light, seldom remaining on the ground
more than two or three days. The average rainfall is about fifty-
three inches, which is pretty uniformly distributed throughout
the year. The climate is eminently favorable to health and
longevity.
Public-domain text, read in full here on John Shaqi.
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