THE CLEM ATE OF BRISBANE. 
159 
* Prunus insititia, 164. Dudley Castle Hill. S.G. 
P. domestica, 164. In the hedges near Battenhall, but doubtful if 
wild. 
* P. Cerasus, 164. Wild cherry tree. (Must be P. Avium , L.) On 
Rosebury Rock, Knightwick, and Ankerdine Hill. A solitary 
tree appearing on Helbury Hill, near Worcester, when the 
wood was cut down. S.G. 
* Spiraea Filipendula, 165. At the west end of Perry Wood, and on 
the Old Hills, but rather rare. Hedges at Brookend, near 
Kempsey. S.G. 
* Agrimonia Eupatoria, 164. Frequent by road sides in various 
places. 
* Sanguisorba officinalis, 153. Very rare. In moist ground at the 
south-west side of Nunnery Wood. S.G. Not uncommon in 
the north of the county. “ Fairly common between Madresfield 
and the Rhydd.” Mr. Toiondrow. 
Alchemilla arvensis, 153. Lanes about Henwick, and Malvern 
Hills. 
* A. vulgaris, 153. Lane leading to Henwick Mill. Also in fields at 
Grimley and Alfrick. L.M. 
{ Tormentilla reptans, 166. Near Cowleigli Park, north of Malvern. 
Probably a Hereford record. 
* Potentilla argentea, 166. On the sand rock between Bromsgrove 
and Droitwich. On a similar rock near Holt, &c. L.M. 
\* P. verna, 166. On the rocks of the Herefordshire Beacon, Malvern. 
Mr. Lees. L.M. A Hereford record. 
* Comarum palustre, 166. On Hartlebury Common, and in pools 
about Bromsgrove Lickey. 
(To be continued.) 
REMARKS AS FOOTNOTES TO 
“THE CLIMATE OF BRISBANE.” 
The highest percentage of relative humidity, viz., 100, 
or absolute saturation, usually occurs in the early morning 
before sunrise, and the lowest percentage in the afternoon. 
The most striking meteorological event during the year 
was the heavy rainfall of January 21st, 18305 inches, or 
1,848J tons per acre falling within 24 hours. This fall 
occurred during the passage of cyclonic disturbance from the 
neighbourhood of New Caledonia; and the disastrous floods 
resulting in the south-eastern portion of the colony form a 
prominent feature in the history of Queensland. 
Much valuable information relating to the distribution of 
pressure over Eastern Australia may be gathered from the 
