CONTEMPLATING GLACIERS - ART EXHIBIT

In this monumental piece, Jan masterfully captures the ephemeral and intricate beauty of cryoconite. Spanning an expansive 48 inches by 156 inches, this ink on paper work presents a captivating exploration of the microscopic particles that play a significant role in glacial ecosystems. 

Jan's meticulous use of black ink on a pristine white background creates a striking visual contrast that mirrors the interplay between light and shadow found in natural environments. Each organic shape and pattern within the composition is rendered with extraordinary precision, inviting viewers to delve into the delicate complexity of cryoconite formations. 

This piece transcends mere scientific illustration, transforming cryoconite into a profound commentary on the interconnectedness of natural elements. 

The elongated format of the artwork emphasizes the vastness of the subject, akin to a panoramic survey of a glacial landscape. It is through this lens that invites us to consider the minute yet impactful interactions within our environment. The dense, almost hypnotic array of shapes within the composition suggests a dynamic process of formation and dissolution, reflecting the continuous and ever-changing nature of glacial surfaces. The artwork’s monochromatic palette enhances the textural details, drawing attention to the intricate structures that comprise cryoconite.  

Jan's work bridges the realms of art and science, offering a visual symphony that is both aesthetically captivating and intellectually stimulating. This piece serves as a poignant reminder of the delicate balance within our natural world and the often-overlooked phenomena that contribute to its beauty and complexity. Through this intricate depiction of cryoconite, we are challenged  to reflect on the broader environmental implications and the subtle yet profound impact of these microscopic particles. The artwork stands as a testament to the power of detailed observation and artistic expression in deepening our understanding of the world around us. - Jessica Turner, Curator

Cryoconite is a powdery windblown dust made of a combination of small particles from erosion, ash, soot and microbes. These deposits build up on snow, glaciers, or ice caps. Their dark colour absorbs solar radiation, melting the snow or ice beneath the deposit, creating a cryoconite hole. Cryoconites may contain dust from far away continental deserts or farmland, particles from volcanic eruptions or power plant emissions, ash from forest fires, and soot. A recent study found that combustion of petroleum was a major contributor of dust particles on the Athabasca Glacier. During the summer cryoconite holes frequently contain water, providing a niche for cold-adapted micro-organisms like bacteria, algae and micro-animals like rotifers and tardigrades. The dark particles decrease the reflectivity, or albedo of ice, increasing absorption of heat. Cryoconite is constantly being added to snow and ice formations along with snow. It is buried within the snow or ice, but as the snow or ice melts increasing amounts of dark matter is exposed on the surface, accelerating melting. - Sourced from Wikipedia

Record Nine Metres of Melt Observed on Alberta's Athabasca Glacier