358 



Miscellanies. 



closed waters at the bottom of old pits. We Tiave altogether l^ept 



out of view the experiments of Spasky and Kupfler on the artesian 



wells of Vienna, as there is certainly some mistake, or rather, as 



Professor Bischof remarks, some militating cause, and he conjectures 



'' that the depths of these springs are not equal to the lowest point of 



the course of the spring, but that the springs rise from a still greater 

 depth." 



Rudcrsdorf (Magnus and Erman,) 



Latter observations, . • • 



Still more recent, ; • • • 



Erzgebirge (Bischof,) from observations on enclos- 

 ed waters, ..•.-• 

 Monk Wearmouth, . . • -, . 

 *] Cornwall, from springs, 



' Cornwall, from enclosed waters, 



Uralian Mountains, from a comparison of the most 



authentic observations in these regions, 

 Riidersdorf, from rising springs, ... • 



Paris, Well at Port St. Ouen, \ ... 



Departments du Nord, S We" of Marquette, . 



et du Pas de Calais, 

 Sheerness, . 



u 



Aire, 



St. Vincent, 



Tours, . ... 



Geneva (De la Riveet Marcet,) 

 Paris, Slaughterhouse of Grenelle, 



Average, 



Feet. 



in every 48.3 



51.2 



" 54.1 



ct 



(( 



(C 



cc 



61.8 

 59.7 

 54.8 

 52.7 



(( 



u 



t« 



ct 



(( 



ii 



a 



a 



ti 



a 



55.4 



54.4 



72.1 



61. 



41. 



47. 



41. 



41.8 



50. 



57.1 



for every 53.1 



Jameson's Journal, April to July, 1839. 



■+ 



32. Notice of rewarJcahle Agitations of the Sea at the Sandwich 

 Islands, on the 1th November, 1837; by T. Chas. Byde Rooke, F- 

 R. C. S. — On the evening and night of the 7th November, a most re- 

 markable commotion of the sea was witnessed at Hanolulu, in many 

 respects similar to that witnessed at these islands in Mav, 1819. One 

 inch and a half of rain had fallen during the previous twenty four 

 hours ; the wind was fresh from the N. E., squally at intervals. The 

 atmosphere was clear and cool. Therm. 74.5; the barometer had 

 gradually fallen during the four previous days, but this evening had 

 again risen to 30.06, at six o'clock, when the alarm was given that 

 the sea was retiring. The first recession was the greatest, something 

 more than eight feet; but being unprepared to make observations at 

 the moment, the exact fall was not measured. The reefs surrounding 

 the harbor were left dry, and the fish aground were mostly dead. 



Copied and reduced from Professor Bischofs paper on Thermal Springs 



