The Ink Pots—a group of karst springs in the Rocky Mountains near Banff, Alberta

1969 ◽  
Vol 6 (4) ◽  
pp. 545-554 ◽  
Author(s):  
R. O. van Everdingen
Keyword(s):  
Rocky Mountains ◽  
National Park ◽  
Fine Sand ◽  
Spring Water ◽  
Karst Springs ◽  
Short Contact Time ◽  
Banff National Park ◽  
Algae Growth ◽  
Chemical Character ◽  
The One

The Ink Pots are a group of springs in Banff National Park. The one feature that makes these springs of more than passing interest is the greenish milky appearance of two of the ponds in the group. This difference in appearance of the water cannot be explained by dissolved or suspended chemicals, or by algae growth. It can be explained by differences in flow velocity, which cause differential suspension of fine sand and silt. Temperature and chemical character of spring water from the Ink Pots indicate, respectively, shallow circulation and a relatively short 'contact' time.

Forest fire's influence on yellow hedysarum habitat and its use by grizzly bears in Banff National Park, Alberta

1999 ◽  
Vol 77 (10) ◽  
pp. 1513-1520 ◽  
Author(s):  
David Hamer
Keyword(s):  
Forest Fire ◽  
Rocky Mountains ◽  
National Park ◽  
Ursus Arctos ◽  
Fibre Content ◽  
Grizzly Bears ◽  
Canadian Rocky Mountains ◽  
Prescribed Burns ◽  
Banff National Park ◽  
Root Quality

Hedysarum (Hedysarum spp.) roots are a primary food of grizzly bears (Ursus arctos) in the Front Ranges of the Canadian Rocky Mountains. I studied the effects of recent forest fire on yellow hedysarum (H. sulphurescens) habitat by comparing root density, mass, fibre content, ease of digging, and use by grizzly bears in and adjacent to two prescribed burns that were conducted in Banff National Park, Alberta, in 1986 (Cascade Valley) and 1990 (Panther Valley). Digging was 12-14% easier in burned than in forested habitat. In the Cascade burn, yellow hedysarum roots were significantly more abundant and heavier than in the adjacent forest. This burn was intensively dug by grizzly bears between 1995 and 1997, but no diggings were found in the adjacent forest. In the Panther burn, no significant differences in root quality or mass were found. Bears dug few roots in the burn and did not dig in the adjacent forest. Their use of these two burns demonstrates prescribed fire's potential to create important yellow hedysarum digging habitat for grizzly bears in Banff National Park.

scholarly journals Dendroglaciological investigations at Hilda Creek rock glacier, Banff National Park, Canadian Rocky Mountains

2002 ◽  
Vol 53 (3) ◽  
pp. 365-371 ◽  
Author(s):  
Rae Carter ◽  
Sean LeRoy ◽  
Trisalyn Nelson ◽  
Colin P. Laroque ◽  
Dan J. Smith
Keyword(s):  
Tree Ring ◽  
Rocky Mountains ◽  
National Park ◽  
Ground Surface ◽  
Canadian Rocky Mountains ◽  
Rock Glacier ◽  
Tree Ring Chronology ◽  
Cross Sectional ◽  
Engelmann Spruce ◽  
Banff National Park

Abstract Dendroglaciological techniques are used to provide evidence of historical rock glacier activity at Hilda Creek rock glacier in the Canadian Rockies. The research focuses on the sedimentary apron of the outermost morainal deposit, where excavations in 1997 uncovered six buried tree boles that had been pushed over and entombed by distally spilled debris. Cross-sectional samples cross- dated with a local Engelmann spruce tree-ring chronology were shown to have been killed sometime after 1856. Based on the extent of the excavation, the data indicate that Hilda Creek rock glacier has continued to advance along the present ground surface at a rate exceeding 1 cm/year.

Evidence for a Neoglacial advance of the Boundary Glacier, Banff National Park, Alberta

1985 ◽  
Vol 22 (11) ◽  
pp. 1753-1755 ◽  
Author(s):  
James S. Gardner ◽  
Norman K. Jones
Keyword(s):  
Rocky Mountains ◽  
National Park ◽  
Direct Evidence ◽  
Canadian Rocky Mountains ◽  
Radiocarbon Dates ◽  
Banff National Park

Direct evidence for an early Neoglacial advance in the Canadian Rocky Mountains is presented. Radiocarbon dates from buried peat and tree remains at Boundary Glacier suggest limiting dates for this advance of between 3800 and 4200 years BP. These data from Boundary Glacier are consistent with previously published dates for the onset of the Neoglacial and an early Neoglacial advance.

Dendrogeomorphological assessment of movement at hilda rock glacier, banff national park, canadian rocky mountains

2004 ◽  
Vol 86 (1) ◽  
pp. 1-9 ◽  
Author(s):  
Taylor Bachrach ◽  
Kaj Jakobsen ◽  
Jacquie Kinney ◽  
Peter Nishimura ◽  
Alberto Reyes ◽  
...  
Keyword(s):  
Rocky Mountains ◽  
National Park ◽  
Canadian Rocky Mountains ◽  
Rock Glacier ◽  
Banff National Park

scholarly journals Characteristics of the Bergschrund of an Avalanche-Cone Glacier in the Canadian Rocky Mountains

1983 ◽  
Vol 29 (101) ◽  
pp. 55-69 ◽  
Author(s):  
Gerald Osborn
Keyword(s):  
Mass Transfer ◽  
Field Study ◽  
Rocky Mountains ◽  
Exploratory Study ◽  
National Park ◽  
Rotational Flow ◽  
Canadian Rocky Mountains ◽  
Void Space ◽  
Banff National Park ◽  
Shallow Part

AbstractField study of the bergschrund of a small avalanche-cone glacier at the base of Mt Chephren, in Banff National Park, has been carried out as part of a general exploratory study of glacier-head crevasses in the Canadian Rockies. The bergschrund consists of a wide, shallow, partly bedrock-floored gap, underneath which extends a nearly verticalRandkluft, and a small, offset, subsidiary crevasse (or crevasses). The following observations regarding the behavior of the bergschrund and ice adjacent to it are of particular interest: (1) topography of the subglacial bedrock is a control on the location of the main bergschrund and subsidiary crevasses, (2) the main bergschrund and subsidiary crevasse(s) are connected by subglacial gaps between bedrock and ice; the gaps are part of the “bergschrund system”, (3) snow/ice immediately down-glacier of the bergschrund system moves nearly vertically downward in response to rotational flow of the glacier, allowing the bergschrund components to keep the same location and size from year to year, (4) an independent accumulation, flow, and ablation system exists in the snow/ice up-glacier of the bergschrund system. (5) most of the void space in the bergschrund system is maintained through the winter, although the wide, shallow part of the main bergschrund fills up with snow, (6) some mass transfer of snow/ice occurs across the bergschrund system, (7) displacement across the bergschrund due to flow of the main glacier body results in significantly more snow being deposited each winter down-glacier of the bergschrund than up-glacier of it.

Lower Cambrian acritarchs from Scotland, Norway, Greenland and Canada

1982 ◽  
Vol 72 (4) ◽  
pp. 257-285 ◽  
Author(s):  
C. Downie
Keyword(s):  
New Species ◽  
Rocky Mountains ◽  
Lower Cambrian ◽  
National Park ◽  
Russian Platform ◽  
New Genera ◽  
East Greenland ◽  
Banff National Park

ABSTRACTAssemblages of acritarchs are described from the Fucoid Beds of Skiag Bridge, Knockan Cliff and Skye in NW Scotland, and Holmia Shales of the Mjøsen area of Norway, the Bastion Formation of Ella Ø in East Greenland, the Lower Cambrian of the Burin Peninsula in Newfoundland and from the Gog Formation of the Rocky Mountains of Banff National Park, Alberta. These are shown to be correctable on the basis of acritarchs and with the Lower Cambrian successions of the Russian Platform. Twenty-one genera and fifty-three species of acritarchs and one tasmanitid are described. These include the new genera Skiagia and Volkovia, and thirteen new species, Acrum cylindiferum, Micrhystridium coniferum, M. ellaensis, M. ellipticum, M. flexispinosum, M. gogensis, M. minutum, M. ordensis, Multiplicisphaeridium ? waltoni, Skiagia brevispinosa, S. scottica, Revinotesta ordensis and Evittia irregulare. A number of recombinations have also been made.

Magnetites from a new unidentified tephra source, Banff National Park, Alberta

1979 ◽  
Vol 16 (6) ◽  
pp. 1294-1297 ◽  
Author(s):  
G. R. Brewster ◽  
R. L. Barnett
Keyword(s):  
Titanium Oxide ◽  
National Parks ◽  
Electron Microprobe ◽  
Rocky Mountains ◽  
National Park ◽  
Volcanic Ash ◽  
Canadian Rocky Mountains ◽  
Banff National Park

Electron microprobe examination of glass-encased magnetites present within surficial volcanic ash deposits located in Banff and Jasper National Parks revealed five distinct magnetite populations. Three of the magnetite populations represented the Mazama, St. Helens Y, and Bridge River volcanic units previously identified in this area of the Canadian Rocky Mountains. The remaining two magnetite groups are characterized by glass-encased magnetites which have titanium oxide concentrations of 11.59 and 10.33%, values considerably higher than those characteristic of either Mazama, St. Helens Y, or Bridge River volcanic units. The high-titanium magnetites are of unknown provenance, and although the section provided no means for dating these volcanic groups, their distribution within the section suggests that they are older than Bridge River, and one group may predate Mazama.

scholarly journals Characteristics of the Bergschrund of an Avalanche-Cone Glacier in the Canadian Rocky Mountains

1983 ◽  
Vol 29 (101) ◽  
pp. 55-69 ◽  
Author(s):  
Gerald Osborn
Keyword(s):  
Mass Transfer ◽  
Field Study ◽  
Rocky Mountains ◽  
Exploratory Study ◽  
National Park ◽  
Rotational Flow ◽  
Canadian Rocky Mountains ◽  
Void Space ◽  
Banff National Park ◽  
Shallow Part

AbstractField study of the bergschrund of a small avalanche-cone glacier at the base of Mt Chephren, in Banff National Park, has been carried out as part of a general exploratory study of glacier-head crevasses in the Canadian Rockies. The bergschrund consists of a wide, shallow, partly bedrock-floored gap, underneath which extends a nearly vertical Randkluft, and a small, offset, subsidiary crevasse (or crevasses). The following observations regarding the behavior of the bergschrund and ice adjacent to it are of particular interest: (1) topography of the subglacial bedrock is a control on the location of the main bergschrund and subsidiary crevasses, (2) the main bergschrund and subsidiary crevasse(s) are connected by subglacial gaps between bedrock and ice; the gaps are part of the “bergschrund system”, (3) snow/ice immediately down-glacier of the bergschrund system moves nearly vertically downward in response to rotational flow of the glacier, allowing the bergschrund components to keep the same location and size from year to year, (4) an independent accumulation, flow, and ablation system exists in the snow/ice up-glacier of the bergschrund system. (5) most of the void space in the bergschrund system is maintained through the winter, although the wide, shallow part of the main bergschrund fills up with snow, (6) some mass transfer of snow/ice occurs across the bergschrund system, (7) displacement across the bergschrund due to flow of the main glacier body results in significantly more snow being deposited each winter down-glacier of the bergschrund than up-glacier of it.

scholarly journals The Smart Forest Conundrum: Contextualizing Pitfalls of Sensors and AI in Conservation Science for Tropical Forests

2021 ◽  
Vol 14 ◽  
pp. 194008292110147
Author(s):  
Dipto Sarkar ◽  
Colin A. Chapman
Keyword(s):  
Tropical Forests ◽  
National Park ◽  
Critical Discussion ◽  
Research Field ◽  
Kibale National Park ◽  
Conservation Science ◽  
Field Station ◽  
Data Production ◽  
Global Corporations ◽  
The One

The term ‘smart forest’ is not yet common, but the proliferation of sensors, algorithms, and technocentric thinking in conservation, as in most other aspects of our lives, suggests we are at the brink of this evolution. While there has been some critical discussion about the value of using smart technology in conservation, a holistic discussion about the broader technological, social, and economic interactions involved with using big data, sensors, artificial intelligence, and global corporations is largely missing. Here, we explore the pitfalls that are useful to consider as forests are gradually converted to technological sites of data production for optimized biodiversity conservation and are consequently incorporated in the digital economy. We consider who are the enablers of the technologically enhanced forests and how the gradual operationalization of smart forests will impact the traditional stakeholders of conservation. We also look at the implications of carpeting forests with sensors and the type of questions that will be encouraged. To contextualize our arguments, we provide examples from our work in Kibale National Park, Uganda which hosts the one of the longest continuously running research field station in Africa.

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