Silas Watson Ford (1848-1895), telegrapher and paleontologist born in Glenville, New York, in 1848, made significant contributions to Cambrian paleontology from 1871 to 1888. The focus of his work was the allochthonous Taconic rock that lies east of the Hudson River in easternmost New York. His discovery of a ‘Primordial’ fauna in this region was instrumental in helping to resolve the uncertainty surrounding the age of this older portion of the Taconics. While most of his papers were published in the American Journal of Science, a series of seven papers on the ‘Silurian Age’ was published by the New York Tribune in 1879. For this work he was subsequently awarded an honorary master’s degree by Union College.

Ford was hired by his contemporary, Charles Doolittle Walcott (1850-1927), to work for the U.S. Geological Survey from 1884 to 1885. Highly regarded by James Hall (1811-1898), James Dwight Dana (1813-1895), Joachim Barrande (1799-1883), and many other prominent geologists of the time, he was often consulted for his expertise in collecting and describing Cambrian-age fossils.

While Walcott’s career continued to flourish, Ford faded into obscurity after 1888. Plagued by personal problems, he was forced to give up his personal library, his fossil collection, and finally, his career. He died in 1895 at the age of 47, with his passing virtually unnoticed by his professional colleagues.