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Charles Richter

Seismologist and physicist (1900–1985)

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Charles Richter, 1900-1985. c.1970
en:Caltech photograph · Public domain

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Through Seismology, Earthquake and Seismic wave

Childhood and education

Richter was born in Overpeck, Ohio, on April 26, 1900. Richter had German heritage: his great-grandfather was a Forty-Eighter, coming from Baden-Baden (today in Baden-Württemberg, Germany) in 1848 in the wake of the German revolutions of 1848–1849. Richter's parents Frederick William and Lillian Anna (Kinsinger) Richter, were divorced when he was very young.

Richter was enrolled in the Hobart Boulevard Elementary School. In his early life, he had faced being isolated and without getting time to play with other children. He faced problems of getting along with other children, and had difficulties in properly adjusting to his school. At 13 years old, Richter's mother admitted him to a special preparatory school that was attached to the University of Southern California. With his new school admission, Richter's grades and interest improved, and he kept examples of his school papers such as assignments, tests and exercises. He began his college work at the University of Southern California when he was 16 years old. Just one year later, he transferred to Stanford University, where he studied the field of chemistry.

He grew up with his maternal grandfather, who moved the family (including his mother) to Los Angeles in 1909. After graduating from Los Angeles High School he attended Stanford University and received his undergraduate degree in 1920. In 1928, he began work on his PhD in theoretical physics from California Institute of Technology, but before he finished it, he was offered a position at the Carnegie Institute of Washington.

At this point, he became fascinated with seismology (the study of earthquakes and the waves they produce in the earth). Thereafter, he worked at the new Seismological Laboratory in Pasadena, under the direction of Beno Gutenberg. In 1932, Richter and Gutenberg developed a standard scale to measure the relative sizes of earthquake sources, called the Richter scale. In 1937, he returned to the California Institute of Technology, where he spent the rest of his career, eventually becoming professor of seismology in 1952. "I wasn't supposed to do routine work on earthquakes,'' he recalled in an interview years later. ''But someone had to find out where they originated and how big they were, so I did it."

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