Water in the foreground with the reflection of the bushes and pine trees to the left. A hill rises to the left behind the pine trees. There is a bank to the right and further on a stand of pine trees that reaches mid-centre. A very cloudy sky hides most of the mountain in the background.
Water in the foreground with the reflection of the bushes and pine trees to the left. A hill rises to the left behind the pine trees. There is a bank to the right and further on a stand of pine trees that reaches mid-centre. A very cloudy sky hides most of the mountain in the background.
A figure in centre front, dressed in a buckskin shirt, blue pants and a floppy hat, is pulling a laden sled, the trail vanishes into the distance, a mountain range in background, a mountainside with trees to the right, a full moon is in the top left of picture in a dark sky
A figure in centre front, dressed in a buckskin shirt, blue pants and a floppy hat, is pulling a laden sled, the trail vanishes into the distance, a mountain range in background, a mountainside with trees to the right, a full moon is in the top left of picture in a dark sky
One felt patch, circular, white background embroidered with “Banff Hockey Club” and image of hockey player with mountains in background. Embroidery in purple and yellow.
One felt patch, circular, white background embroidered with “Banff Hockey Club” and image of hockey player with mountains in background. Embroidery in purple and yellow.
Fossilized colonial coral, middle Devonian in age. Common throughout North America. Species: Pachyphyllum. Warm shallow ocean environment. Limestone matrix. Has undergone weathering. Coral structure is well defined. Small crinoid fragments exposed on one side. Recrystallization of the rock is occur…
Fossilized colonial coral, middle Devonian in age. Common throughout North America. Species: Pachyphyllum. Warm shallow ocean environment. Limestone matrix. Has undergone weathering. Coral structure is well defined. Small crinoid fragments exposed on one side. Recrystallization of the rock is occurring is some areas, calcite crystals growing in the vugs (cavities). These types of coral fossils are very common in Western Canada and could have been collected locally.