Letter - E.C. Schmon to Arthur A. Schmon, 11 April 1916

A letter from Eleanore Celeste Schmon to Arthur A. Schmon in the year 1916. She discusses her letter writing, a luncheon at the McCrackens and her work with the Red Cross. It is labelled the 84th letter.

Letter - E.C. Schmon to Arthur A. Schmon, 11 & 12 September 1918

Eleanore Celeste describes Arthur's departure for service one year ago. She also discusses a friend, Dick Hart, who was thought to have been a casualty of a torpedoed ship, but is now thought to be safe. She mentions that she will visit Mother Schmon and had played tennis with Gus. The letter is labelled number 159.

384.85-385.0 DE # 11

Mainly coarse grained with a separate fine grained clay domain occurring throughout the sample. The coarse grained domain contains clasts that range from small to medium in size. The clast shape ranges from angular to sub-angular. Grain crushing is abundant in this sample, along with lineations, and minor amounts of rotation.

11 PTA002.1

Dark brown sediment with clasts ranging from small to large in size. Clast shape ranges from angular to rounded. Rotation structures and necking structures are common throughout this sample. Lineations, grain crushing, and comet structures are also abundant in the sample. Some grain stacking can also be seen.

11 PTA002.2

Dark brown sediment with clasts ranging from small to large in size. Clast shape ranges from angular to rounded. Lineations and rotation structures are abundant in this sample. Grain crushing can be commonly be seen throughout. Grain stacking and comet structures are present in minor amounts.

11 PTA004

Dark brown sediment with clasts ranging from small to large in size. Clast shape ranges from angular to sub-rounded. Many grains in this sample are fractured and/or weathered. Lineations are abundant throughout this sample. Rotation structures and necking structures can also be seen mainly around/between large clasts. Crushed grains and comet structures are also present in minor amounts.

11 PTA007

Dark brown sediment with clasts ranging from small to large in size. Grain shape ranges from angular to rounded. Lineations can commonly be seen throughout the sample. Many clasts are fractured and/or weathered. Necking structures, some rotation structures, and minor amounts of grain crushing can also be seen.

11 PTA008

Greyish-brown sediment with clasts ranging from small to large in size. Grain shape ranges from angular to rounded in shape. Many grains appear to be fractured or weathered. Lineations and rotation structures are abundant within this sample. Grain crushing and stacking can also be seen in this sample. Comet structures are also present in minor amounts.

11 PTA0010A

Greyish brown sediment with clasts ranging from small to large in size. Clast shape ranges from angular to rounded. Many grains in this sample are fractured. Rotation structures and lineations are the most common micro-structures that can be seen in this sample. Grain crushining, grain stacking, and comet structures can also be seen.

11 PTA0011

Dark grey sediment with clasts ranging from small to large size. Grain shape ranges from angular to rounded. Many grains are fractured and weathered. Necking structures, along with rotation structures, are very common in this sample. They can be seen between many of the larger aggregates. Lineations and grain crushing are also present throughout.

11 PTA0012

Dark grey sediment with clasts ranging from small to large in size. Grain shape ranges from angular to rounded. Many grains are fractured and/or weathered. Edge-to-edge grain crushing is abundant in this sample, and some crushed grains can also be seen. It also contains lineations and rotation structures throughout. Minor amounts of comet structures can also be seen.

11 PTA0013H

Dark grey sediment sample with clasts ranging from small to large in size. Clast shape ranges from angular to rounded. Lineations and grain crushing are the most abundant. Necking structures and rotation structures can also be seen throughout the sample mainly between/surrounding larger aggregates. A few comet structures can also be seen.

By-Laws No. 1 through 11

The by-laws are signed by George Barnes and include the first two which state the name of the company is the Ontario Grape Growing and Wine Manufacturing Company and the second by-law states that the place of business is at Barnesdale, St. Catharines, Ontario.