Harriot, Thomas, Mss. 6789

List of thumbnails

< >
1001
1001 (502r) 		1002
1002 (502v)
1003
1003 (503r) 		1004
1004 (503v)
1005
1005 (504r) 		1006
1006 (504v)
1007
1007 (505r) 		1008
1008 (505v)
1009
1009 (506r) 		1010
1010 (506v)
< >
page |< < (441r) of 1074 > >|
    <echo version="1.0RC">
      <text xml:lang="eng" type="free">
        <div type="section" level="1" n="1">
          <pb file="0881.jpg" o="441r" n="881"/>
          <p>
            <s xml:space="preserve"> Three reasons to prove that there
              <lb/>
            is a passage from the Northwest
              <lb/>
            into the South </s>
          </p>
          <p>
            <s xml:space="preserve"> 1. The tydes in Port Nelson (where S
              <emph style="super">r</emph>
            Tho: Button did
              <lb/>
            winter) move constantly. 15, or. 18. foote; which is not
              <lb/>
            found in any Bays Throughout the world but
              <lb/>
            in such seas as lie open att both ends to the mayne
              <lb/>
            </s>
          </p>
          <p>
            <s xml:space="preserve"> 2. Every strong westerne winde did bring into the
              <lb/>
            Harbor where he wintered, so much water, that the
              <lb/>
            Neap-tydes were æquall to the Spring-tydes,
              <lb/>
            notwithstanding that the Harbor was open only to the E. N. </s>
          </p>
          <p>
            <s xml:space="preserve"> 3. In coming out of the harbor, shaping his course,
              <lb/>
            directly North, about, 60, degrees, he found a
              <lb/>
            strong race of a tyde, setting due East & West,
              <lb/>
            which in probabilitie could be noe other thing, than the
              <lb/>
            tyde coming from the West, and retourning from
              <lb/>
            the </s>
          </p>
        </div>
      </text>
    </echo>
Impressum