Howell, Mich. street scene

verso: Things reached a fever pitch in 1915 as the Wolverine Paved Way was nearing completion. A brick road from Detroit to Lansing would be finished and the town's main street would finally be paved. In this photograph autos had started from Lansing and picked up others in all the small towns on the way to Howell for the big celebration. As you can see, they didn't worry about parking. They stopped their cars in the street and left them. Before Prohibition, Howell was known as the fun city of Southern Michigan, and there is said to have been 13 bars in the main four blocks of town. All the travelling men made it a point to stay over in Howell whenever possible. It was said that you could not fall down on the main street of town without falling into the doorway of a bar. This probably explains the empty cars after a long dusty trip. Notice, too, that about half the cars are still right hand drive.

Ann Arbor Mayor William E. Brown & members of the City Council, 1957 (inc. Towsley, Maslon, Burns, Menafee)

2 scans - 1of 2 includes inscriptions in margins, 2o2 detail of photo alone

Traffic and the city plan.

Mode of access: Internet.

A redevelopment plan for the central business district : a part of the master plan for the City of Muskegon /

Cover title: Central business district redevelopment plan.

The municipal code of the city of Detroit, containing the city charter and the compiled ordinances.

Cover title.

Official proceedings of the Board of Education of the City of Grand Rapids, Michigan.

Description based on: May 6, 1912 to May 5, 1913.

Proceedings of the City Commission.

Mode of access: Internet.

Raman microscopic study of the Li amphibole holmquistite, from the Martin Marietta Quarry, Bessemer City, NC, USA

The Raman spectrum of holmquistite, a Li-containing orthorhombic amphibole from Bessemer City, USA has been measured. The OH-stretching region is characterized by bands at 3661, 3646, 3634 and 3614 cm–1 assigned to 3 Mg–OH, 2 Mg + Fe2+–OH, Mg + 2Fe2+–OH and 3 Fe2+–OH, respectively. These Mg and Fe2+ cations are located at the M1 and M3 sites and have a Fe2+/(Fe2+ + Mg) ratio of 0.35. The 960–1110 cm–1 region represents the antisymmetric Si–O–Si and O–Si–O stretching vibrations. For holmquistite, strong bands are observed around 1022 and 1085 cm–1 with a shoulder at 1127 cm–1 and minor bands at 1045 and 1102 cm–1. In the region 650–800 cm–1 bands are observed at 679, 753 and 791 cm–1 with a minor band around 694 cm–1 attributed to the symmetrical Si–O–Si and Si–O vibrations. The region below 625 cm–1 is characterized by 14 vibrations related to the deformation modes of the silicate double chain and vibrations involving Mg, Fe, Al and Li in the various M sites. The 502 cm–1 band is a Li–O deformation mode while the 456, 551 and 565 cm–1 bands are Al–O deformation modes.