Lewis and Clark Line, Montana: Tectonic evolution of a crustal-scale flower structure in the Rocky Mountains

Author(s):  
James W. Sears ◽  
Kathryn MacDonald ◽  
Jeffery Lonn
Author(s):  
Ryan Hall

This chapter describes Blackfoot responses to increasing colonial activity on the northwest plains and Rocky Mountains between 1806 and 1821. Ascending the Missouri River to their south, the American expedition of Lewis and Clark circumvented the Blackfoot to open ties with Native nations in the intermountain West. British explorer David Thompson did the same in the north, accessing the mountains near the headwaters of the North Saskatchewan River. Blackfoot people responded to these invasions with a targeted campaign of diplomacy and conflict, including blockades of key mountain passes, that severely limited American, Canadian, and British ambitions in the region for a generation. These conflicts also led to an overly simplistic depiction of Blackfoot “hostility” that lingers to this day.


1991 ◽  
Vol 128 (6) ◽  
pp. 561-584 ◽  
Author(s):  
M. S. Ameen

AbstractThe folds in the Taurus–Zagros Belt of northern Iraq have generally been considered to be decollement buckle folds. This implies the presence of a decollement horizon at or near the base of the sedimentary cover, the ‘Infra-Cambrian Hormuz Salt’ and a passive role of the Precambrian basement in the tectonic evolution of the folded belt. Structural, stratigraphic, geophysical and remote sensing evidence suggests that forced folding, due to faulting in the basement, has played a significant role in the development of many of the folds in this region. This is clear from the substantial evidence of basement faulting, the lack of any convincing evidence for the presence of an extensive and regional decollement horizon (i.e. the Hormuz Salt) between the basement and the cover rocks, and the geometries of the folds and related mesostructures. The study shows that in the Taurus Foothills Zone, the folds are short, oval in plan shape, and arranged in an en echelon pattern along two sets of dislocation zones in the basement. However, the folds in the Zagros Foothills Zone are longer, linear and arcuate in plan shape. Many of the studied folds show similar features to those observed in the Rocky Mountains, U.S.A.


1987 ◽  
Vol 60 (1) ◽  
pp. 59-62 ◽  
Author(s):  
Philip Howard Gray

A preliminary attempt is made to identify the progress of the study of animal behavior, from native bears to imported apes, in the Rocky Mountain region. The survey includes naturalistic encounters, ethological observations, and laboratory studies, but is not a complete enumeration of animal research in the Rocky Mountains.


1988 ◽  
Vol 25 (1) ◽  
pp. 106-115 ◽  
Author(s):  
Trygve Höy ◽  
P. van der Heyden

The Reade Lake and Kiakho stocks are posttectonic mesozonal quartz monzonite porphyries that intrude dominantly Middle Proterozoic Purcell Supergroup rocks in southeastern British Columbia. K–Ar dates of hornblende from the Reade Lake stock range from 103 to 143 Ma. However, a U–Pb date of 94 Ma from zircon concentrates is interpreted to be the age of emplacement of the stock, suggesting the range and older K–Ar dates are due to excess 40Ar. A K–Ar date of 122 Ma for the hornblende from the Kiakho stock is believed to be a more reliable intrusive age.Both stocks cut across and apparently seal two faults that have played roles in the tectonic evolution of the Purcell anticlinorium and Rocky Mountain thrust belt. The Reade Lake stock cuts the St. Mary fault, an east-trending reverse thrust that crosses the Rocky Mountain trench and links with thrusts in the Rocky Mountains; the Kiakho stock cuts the Cranbrook fault, an older east-trending normal fault. Hence, the 94 Ma date on the Reade Lake stock constrains the latest movement on the St. Mary fault to early Late Cretaceous; and the 122 Ma date on the Kiakho stock appears to limit latest movement on the Cranbrook fault to Early Cretaceous. These faults and the intrusions are part of an allochthonous package, displaced eastward by underlying thrust faults during formation of the Purcell anticlinorium and more eastern thrusts in the Rocky Mountains.


Author(s):  
Donald Worster

Nostalgia runs all through this society—fortunately, for it may be our only hope of salvation. My own version, which I probably share with a few million others, takes me back to walk in pristine natural places on this continent. I dream of traveling with our second native-born naturalist, William Bartram (his father John was the first), a slightly daft Pennsylvania Quaker who botanized from the Carolinas down into Florida in the early 1770s. I would travel with him, “seduced by ... sublime enchanting scenes of primitive nature,” through aromatic groves of magnolia, sweet gum, cabbage palmetto, loblolly pine, live oak, the roaring of alligators in our ears. I would gaze with Thomas Jefferson through his elegant white-framed windows at Monticello toward the Blue Ridge Mountains, speculating about the prodigious country stretching west. Best of all, I imagine entering that west with Lewis and Clark in 1804–5, standing beside them on Spirit Mound in present-day South Dakota, beholding, as Clark put it in his execrable spelling, “a most butifull landscape; Numerous herds of buffalow were Seen feeding in various directions; the Plain to North N. W. & N.E. extends without interuption as far as Can be seen.” And I think what it must have been like for them warping and poling up the muddy Missouri River, penetrating farther into the vast open country of the unplowed, unfenced prairies when wolves still howled in the night; of heading into “the great unknown,” panting over the unpainted, unmined, unskiied Rocky Mountains and rafting down the uncharted, undammed Columbia to the gray-green drizzly shore of the Pacific Ocean. How much has been lost in our short years as a nation, how much have we to be nostalgic about. In the beginning of white discovery North America must have been a glorious place, brimming with exquisite wild beauty, offering to agriculturists some of the earth's richest soils, incredible stands of trees, booty on booty of mineral wealth. Think for a moment of the infinitude of animals that once teemed but are now diminished or gone. In the most comprehensive, detailed analysis yet offered, Frank Gilbert Roe estimated that forty million bison roamed the continent as late as 1830.


Sign in / Sign up

Export Citation Format

Share Document