After nearly 11 years, I’ve finally decided to pull the plug on Usenet archive: Groupsrv.com.
The page you have requested no longer exists!
But don’t panic just yet!
I’ve coded this page in a way, that it’s monitoring each redirect & capturing data about the thread you’ve requested. Page you’ve requested is still available in Google’s Usenet Archive. You should be able to access it using following URL:
Note: I can’t guarantee that all Groupsrv.com pages can be found in Google Groups, but over 90% of the content should be there. If not, try the resources below!
Latitude! – surface. Latitude is an angle (defined below) which ranges from 0° at the Equator to 90° (North or South) at the poles. Lines of constant latitude, or parallels
Navigation! – along three or more axes enabling it to continually and accurately calculate the current latitude and longitude. Its advantages over other navigation
Earth! – of latitude from the equator. Earth’s surface can be subdivided into specific latitudinal belts of approximately homogeneous climate. Ranging from the
History of timekeeping devices! – and wristwatches. Atomic clocks are far more accurate than any previous timekeeping device, and are used to calibrate other clocks and to calculate the
Australia! – Australian Antarctic Territory. Apart from Macquarie Island, Australia lies between latitudes 9° and 44°S, and longitudes 112° and 154°E. The Great Barrier Reef