Material Culture of an Upper Coulee Rockshelter

1952 ◽  
Vol 17 (4) ◽  
pp. 352-359 ◽  
Author(s):  
John E. Mills ◽  
Carolyn Osborne

Though the number of recovered cultural remains are few, the authors believe that the brief description and analysis of these artifacts are important, as site 45GR2 is the first dry shelter to be excavated in the Columbia Plateau.The area itself falls into the Upper Sonoran life zone. The plateau above the coulee is generally treeless and is more or less well covered with bunch grass. Lupines and sunflowers are important parts of the flora. In the coulee, ground water is more available, and better stands and more species of grasses are present. Successful wheat farms and a few orchards indicate that the area must, at least during certain seasons, have had an extensive floral cover. Aspen, willow, alder, and cottonwoods are found near the springs. The draws support heavy stands of brushy growth, with sage being outstanding. Juniper (cedar) trees are found both on the plateau and in the coulee. The bottom of the coulee, at least during and after the spring and early summer rains, is swampy, and standing water was probably present in earliest times in some places throughout most of the year. Rodents, small carnivore, and bird populations are large. The mule deer was no doubt the largest game animal of importance.

Geology ◽  
1989 ◽  
Vol 17 (7) ◽  
pp. 606 ◽  
Author(s):  
Paul P. Hearn, Jr. ◽  
William C. Steinkampf ◽  
Duane G. Horton ◽  
G. Cleve Solomon ◽  
L. Doug White ◽  
...  

1989 ◽  
Vol 40 (1) ◽  
pp. 55 ◽  
Author(s):  
CM Burke ◽  
B Knott

Salinity, temperature, dissolved oxygen (DO), pH and total alkalinity (TA) were measured in four saline lakes of Yalgorup National Park, Western Australia, primarily over an 18-month period, July 1985 to January 1987, but also during 1987 and in 1988. These lakes are shallow (<3 m) ground-water sinks with no surface drainage. Rainfall and hence ground-water inflow to the lakes was highly seasonal and occurred mainly between May and October. Lakes Hayward, North Newnham and South Newnham were consistently hypersaline (e.g. Hayward 61-214 g L-1) and Hayward and North Newnham were stratified from autumn to early summer. The bottom layer of water in Hayward was usually supersaturated (to 430%) with respect to DO, because of the photosynthetic activity of the benthic microbial communities (BMC). South Newnham did not stratify in 1985, but did so briefly in 1987 after a BMC developed. The salinity of Lake Pollard varied from 19 to 51 g L-1 and the lake did not stratify at all. During spring, extensive growth of the charophyte Lamprothamnium papulosum across the sediments in Lake Pollard increased DO (from c. 100% to c. 140% saturation) and pH (from c. 8.5 to c. lo), but lowered specific TA (from 0.26 to 0.075 meq L-1 per unit salinity); later removal of the L. papulosum by swans reduced DO to 50% saturation and pH to 7.5, and increased specific TA to 0.15 meq L-1 per unit salinity. It is apparent that the processes controlling Hayward, North Newnham and South Newnham are similar and are based on the activities of the BMC. South Newnham is at an earlier stage of evolution. However, Pollard is controlled primarily by L. papulosum growth and its subsequent removal by swans; this indicates a different evolutionary path for this lake.


Sign in / Sign up

Export Citation Format

Share Document