Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

“The Silent Flag in the New Fallen Snow”: Sara Jeannette Duncan and the Legacy of the South African War

View through CrossRef
The South African War (1899-1902) was the largest war involving Canadian soldiers between Confederation and the First World War. It ignited controversies in Canada that echoed throughout the twentieth century. The war is integral to Sara Jeannette Duncan’s The Imperialist (1904) and Cousin Cinderella (1908), two of only a few Canadian novels to depict the war’s political and cultural impact on Canada. Although Duncan’s novels are typically read as works of late-Victorian social realism, this essay argues that the novels, published in the wake of the South African War, are also quintessential postwar novels concerning ideology and conflict in the nascent twentieth century.
University of Toronto Press Inc. (UTPress)
Title: “The Silent Flag in the New Fallen Snow”: Sara Jeannette Duncan and the Legacy of the South African War
Description:
The South African War (1899-1902) was the largest war involving Canadian soldiers between Confederation and the First World War.
It ignited controversies in Canada that echoed throughout the twentieth century.
The war is integral to Sara Jeannette Duncan’s The Imperialist (1904) and Cousin Cinderella (1908), two of only a few Canadian novels to depict the war’s political and cultural impact on Canada.
Although Duncan’s novels are typically read as works of late-Victorian social realism, this essay argues that the novels, published in the wake of the South African War, are also quintessential postwar novels concerning ideology and conflict in the nascent twentieth century.

Related Results

Characteristics of Taiga and Tundra Snowpack in Development and Validation of Remote Sensing of Snow
Characteristics of Taiga and Tundra Snowpack in Development and Validation of Remote Sensing of Snow
Remote sensing of snow is a method to measure snow cover characteristics without direct physical contact with the target from airborne or space-borne platforms. Reliable estimates ...
Influence of cohesion on drifting snow investigated in cold wind-tunnel 
Influence of cohesion on drifting snow investigated in cold wind-tunnel 
<p>Aeolian transport of particles occurs in many geophysical contexts such as wind-blown sand or snow drift and is governed by a myriad of physical mechanisms. Most o...
Snow representation in seasonal forecasts and climate simulations: sensitivities of seasonal snow simulation and impact on frozen soils
Snow representation in seasonal forecasts and climate simulations: sensitivities of seasonal snow simulation and impact on frozen soils
Snow cover is a critical component of the Earth's climate system, covering up to 44 % of the Northern Hemisphere's land during winter and influencing energy exchange, water storage...
Dynamic Snow Distribution Modeling using the Fokker-Planck Equation Approach
Dynamic Snow Distribution Modeling using the Fokker-Planck Equation Approach
<p>The Fokker-Planck equation (FPE) describes the time evolution of the distribution function of fluctuating macroscopic variables.  Although the FPE was...
Dynamic identification of snow phenology in the Northern Hemisphere
Dynamic identification of snow phenology in the Northern Hemisphere
Abstract. Snow phenology characterizes the cyclical changes in snow and has become an important indicator of climate change in recent decades. Changes in snow phenology can signifi...
Revisiting NASA's Operation IceBridge Snow on Sea Ice Radar Measurements in the Arctic
Revisiting NASA's Operation IceBridge Snow on Sea Ice Radar Measurements in the Arctic
Snow on sea ice plays a critical role in modulating ice mass changes in response to anthropogenic warming, with significant implications for ocean mixed layer processes, the surfac...
A snow reanalysis for Italy: IT-SNOW
A snow reanalysis for Italy: IT-SNOW
Quantifying the amount of snow deposited across the landscape at any given time is the main goal of snow hydrology. Yet, answering this apparently simple question is still elusive ...
Saltation layer of cohesive drifting snow observed in a wind tunnel
Saltation layer of cohesive drifting snow observed in a wind tunnel
<p>Aeolian transport of particles occurs in many geophysical contexts such as wind-blown sand or snow drift and is governed by a myriad of physical mechanisms. Most o...

Back to Top