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The Great Colchester Earthquake; The effects of the earthquake on the area of Eastern Essex south of the River Blackwater Archived 20 November 2008 at the Wayback Machine; Meldola, Raphael; White, William (1885). Report on the East Anglian Earthquake of April 22nd, 1884. Essex Field Club Special Memoirs. Vol. 1. London: Macmiillan & Co.
Parallels Desktop for Mac is a hypervisor providing hardware virtualization for Macintosh computers developed by Parallels, a subsidiary of Corel.. Parallels was initially developed for Macintosh systems with Intel processors, with version 16.5 introducing support for Macs with Apple silicon.
For a list of current programs, see List of Mac software. Third-party databases include VersionTracker , MacUpdate and iUseThis . Since a list like this might grow too big and become unmanageable, this list is confined to those programs for which a Wikipedia article exists.
Parallels may refer to: Circle of latitude (also parallels), an abstract east–west small circle connecting all locations around Earth at a given latitude; Parallels (company), a software company based in Bellevue, Washington Parallels Desktop for Mac, software providing hardware virtualization for Macintosh computers with Intel processors
Parallels International GmbH is a software company based in Bellevue, Washington.It is involved in the development of virtualization software for MacOS.The company has over 800 employees and offices in 14 countries, including the United States, Germany, United Kingdom, France, Japan, China, Spain, Malta, Australia, and Mauritius [4] [5] [3]
Parallels Workstation is the first commercial software product released by Parallels, Inc., a developer of desktop and server virtualization software.The Workstation software comprises a virtual machine suite for Intel x86-compatible computers (running Microsoft Windows or Linux) (for Mac version, see Parallels Desktop for Mac) which allows the simultaneous creation and execution of multiple ...
The 1884 Andalusian earthquake (Spanish: Terremoto de Andalucía de 1884) occurred on 25 December 1884 at 9:08 p.m in the south of Spain, and had an estimated magnitude of 6.7 M w. It shook a poor region where many of the houses were built without foundations, with lime or mud mortar, and with weak joints.
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