The Kennamer Family

by John Robert Kennamer, Lorrin Garfield Kennamer

1924

"After careful study of all sources for two years, the authors are of the opinion that [their Kennamer] forefathers were of High Dutch descent and lived in Holland near where that State borders with present-day Germany. ... They came to this country before the Revolutionary War and settled in the Carolinas."--Page 13. Some later went to Alabama. "Hans Kennamer, with a large family, and his eldest son, Jacob, who was married, came to the Cove and settled among the Indians in 1798, or not later than 1805. This place is now know as Kennamer Cove. ... The records of Madison County, Alabama, show that Samuel, Stephen and Jacob Kennamer bought land in that county in 1809. ... It is a well-known fact that the sons of Hans Kennamer settled ... in the western part of Jackson County, the eastern part of Madison County, and the northern part of Marshall County. David and Abram resided in Madison County, while John Kennamer lived at the place wher Paint Rock, Alabama, now is. ... Hans Kennamer died and was buried in Pisgah Cemetery, in Kennamer Cove, Alabama."--Page 14-15. Nothing is know of his wife. Son Jacob Kennemer (ca. 1776-1856) " ... moved from Alabama to Giles County, Tennessee where he acquired ... land of Sugar Creek. ... He was married twice, but the names of his wives could not be ascertained. He was buried on Anderson Creek, in Lauderdale County, Alabama, near Foster's Mill."--P. 17-18. Also includes Kennamer, Kennemore, Canamore, Kennemur, Kennemer, Kenimer families of Georgia. Descendants and relatives lived in Alabama, Tennessee, Texas, California, Oklahoma, New Mexico, Missouri, Iowa, Georgia and elsewhere

Polar Remote Sensing

by Dan Lubin, Robert Massom

2006 · Springer Science & Business Media

The polar regions, perhaps more than any other places on Earth, give the geophysical scientist a sense of exploration. This sensibility is genuine, for not only is high-latitude ?eldwork arduous with many locations seldom or never visited, but there remains much fundamental knowledge yet to be discovered about how the polar regions interact with the global climate system. The range of opportunities for new discovery becomes strikingly clear when we realize that the high latitudes are not one region but are really two vastly di?erent worlds. The high Arctic is a frozen ocean surrounded by land, and is home to fragile ecosystems and unique modes of human habitation. The Antarctic is a frozen continent without regular human habitation, covered by ice sheets taller than many mountain ranges and surrounded by the Earth’s most forbidding ocean. When we consider global change as applied to the Arctic, we discuss impacts to a region whose surface and lower atmospheric temperatures are near the triple point of water throughout much of the year. The most consistent signatures of climate warming have occurred at northern high latitudes (IPCC, 2001), and the potential impacts of a few degrees increase in surface temperature include a reduction in sea ice extent, a positive feedback to climate warming due to lowering of surface albedo, and changes to surface runo? that might a?ect the Arctic Ocean’s salinity and circulation.