199 results — type: Book Chapter
Silviculture
Abstract Silviculture is the art and science of managing forest stands to meet landowner goals and objectives; traditional examples of goals and objectives include managing for timber production, improved wildlife habitat, fuels reduction, and maintenance or improvement of forest health.
The Mountaineer Folsom Projectile Point Assemblage
which, following Aldenderfer (2006), we define as locations at elevations greater than 2,500 meters above sea level (e.g.,
Sage-Grouse
Abstract In this chapter, we summarize the ecology and conservation issues affecting greater ( Centrocercus urophasianus ) and Gunnison ( C . minimus ) sage-grouse, iconic and obligate species of rangelands in the sagebrush ( Artemisia spp.) biome in western North America. Greater sage-grouse are no
The Return of the Native: Northern Ute Removal from and Return to Colorado Ancestral Homelands
New views on late Paleozoic climate and tectonics in the Ancestral Rocky Mountains
Recent research in Pennsylvanian-Permian strata of the Fountain Formation adjacent to the Front Range uplift and the Cutler Formation adjacent to the Uncompahgre uplift (Colorado) has resulted in new hypotheses about the climate and tectonics of the Ancestral Rocky Mountains. The Fountain and the Cu
Natural History of <i>Diuraphis</i> (Homoptera: Aphididae) Species Occurring in Western Colorado
Three species of Diuraphis in addition to the Russian wheat aphid , Diuraphis noxia (Mordvilko), occur in western Colorado . Diuraphis (Holcaphis) tritici (Gillette), the western wheat aphid, and Diuraphis nodulus (Richards) were collected near Meeker (Rio Blanco County) in 1990. Both species were f
Insights Regarding the Dating of Ute Occupation in West Central and Northwest Colorado: A Perspective from the Colorado Wickiup Project
Blocks X and Y
which, following Aldenderfer (2006), we define as locations at elevations greater than 2,500 meters above sea level (e.g.,
Landscape, Science, and Social Reproduction
This chapter discusses the arc of Carolyn Merchant’s direct and indirect influences on work, particularly now forming a bridge between completed landscape history of Point Reyes National Seashore here in northern California, and developing a new focus on the history of the Rocky Mountain Biological
Block C
which, following Aldenderfer (2006), we define as locations at elevations greater than 2,500 meters above sea level (e.g.,
Groundwater Resources of Colorado’s San Luis Basin
The Environmental Context
which, following Aldenderfer (2006), we define as locations at elevations greater than 2,500 meters above sea level (e.g.,
G. K. Gilbert and ground water, or ‘I have drawn this map with much reluctance’
Gilbert’s studies of underground water were overshadowed by his magnificent reports on geologic structure and landforms. In fact, his 1896 publication on the underground water of the Arkansas Valley in eastern Colorado was called by W. M. Davis “for the most part a straightforward geological account
Invasion and restoration of western rivers dominated by Tamarix spp.
Fifty years ago, riparian habitats were not recognized for their extensive and critical contributions to wildlife and the ecosystem function of watersheds. This changed as riparian values were identified and documented, and the science of riparian ecology developed steadily. Papers in this volume ra
Paleokarst-Controlled Ore in Central Colorado
Abstract We propose that many Tertiary man to orebodies typical of Leadville and adjacent districts of Central Colorado (northern Sawatch range and Mosquito range) are modifications to pre-existing mineralized paleokarst cave systems (Tschauder and Landis, 1985; Landis and Tschauder, 1985). Major ka
The carbonatite complex at Iron Hill, Powderhorn district, Gunnison County, Colorado
Abstract The carbonatite complex at Iron Hill is located southeast of the town of Powderhorn along Cebolla Creek, Deldorado Creek, and Beaver Creek in Gunnison County, Colorado. To reach the complex, travel 9 mi (14.5 km)west of Gunnison on U.S. 50 to the intersection with Colorado 149, turn south o
Block A
which, following Aldenderfer (2006), we define as locations at elevations greater than 2,500 meters above sea level (e.g.,
Geology, Site Formation, and Geochronology
which, following Aldenderfer (2006), we define as locations at elevations greater than 2,500 meters above sea level (e.g.,
