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1. Sign in to Desktop Gold. 2. Click the Settings button at the top. 3. Click Mail on the left side. 4. Click the Font and Text tab. 5. Next to Default Read Mail Zoom, select your preferred zoom level from the menu.
1. Sign in to Desktop Gold. 2. Navigate to a webpage. 3. In the bottom right corner you can see the current zoom setting. 4. Click the + and -buttons to adjust your zoom level.
With simple keyboard shortcuts, you can zoom in or out to make text larger or smaller. In an instant, these commands improve the readability of the content you're viewing. • Zoom in - Press Ctrl (CMD on a Mac) + the plus key (+) on your keyboard. • Zoom out - Press Ctrl (CMD on a Mac) + the minus key (-) on your keyboard. Zoomed too far?
Thumbnails (18 pre-defined sizes from 50×50–800×800 pixels), fullscreen, slideshow, zoom, fit (several options), view IPTC and Exif info, hex view, histogram (also RGB); Format detection with offer to rename, set wallpaper, EXE/SCR creation, Burn slideshow to CD; directory tree
Page zoom in LibreOffice Writer. The level of page zoom, expressed as a percentage, can often be accessed using a slider. Other methods include a drop-down menu from with a zoom level can be selected, pinch-to-zoom on touchscreen devices, mouse wheel scrolling (often in combination with holding down a key on the keyboard), or keyboard shortcuts (such as CTRL + +/-).
Compiz-Fusion window manager has a highly configurable plugin named "Enhanced Zoom Desktop" GNOME has gnome-mag, which as of 2015 forms part of GNOME Shell [3] KDE has KMagnifier (KMag) The Microsoft Windows operating system has included the "Magnifier" application since Windows 98 (released in 1998). It can integrate with a mouse-button toggle.
To view multiple windows in AOL Desktop Gold, you'll want to resize and position them appropriately on your screen. You can also save the window size and position for the next time you sign in to Desktop Gold.
While in principle aspheric surfaces can take a wide variety of forms, aspheric lenses are often designed with surfaces of the form = (+ (+)) + + +, [3]where the optic axis is presumed to lie in the z direction, and () is the sag—the z-component of the displacement of the surface from the vertex, at distance from the axis.