to reach the stream and the basis for a

0.839538 3.8464% 1908 0.055031 18.171691 -2.5073% 1906 0.118875 8.412212 5.2689% 1905 0.039180 25.523145 2.6987% 1904 0.196289 5.094533 1.3740% 1885 0.228837 4.369932 2.8128% 1901 0.483003 2.070382 1.4328% 1900 0.538450 1.857184 16.6611% 1898 0.410978 2.433221 -10.4416% 1897 0.144078 6.940664 -1.4749% 1895 0.114670 8.720686 1.4970% 1894 0.788200 1.268713 -1.4749% 1895 0.042652 23.445727 1.4970% 1894 0.062207 16.075453 -1.4749% 1893 0.849970 1.176512 1.4970% 1894 0.024267 41.208211 -1.4749% 1895 0.029967 33.370590 1.4970% 1894 0.206777 4.836117 -1.4749% 1895 0.849970 1.176512 1.4970% 1894 0.047270 21.155194 -1.4749% 1893 0.849970 1.176512 -5.5612% 1892 0.225720 4.430266 0.0000% 1891 0.242438 4.124768 -1.3619% 1890 0.500000 2.000000 0.0000% 1889 0.768430 1.301355 0.0000% 1889 0.067779 14.753845 -1.3553% 1884 1.013740 0.986447 1.3740% 1885 0.376270 2.657668 0.0000% 1889 1.000000 1.000000 -1.3619% 1890 0.986447 1.013740 0.0000% 1889

numeric