Aerial cameras and their use for aerial photography are the simplest and oldest of sensors used for remote sensing of the Earth’s surface. Cameras are framing systems that acquire a near-instantaneous “snapshot” of an area of the surface. The camera uses a lens to focus on reflected light from the real world onto the film.

Oblique aerial photography:

Photographs taken at an angle are called oblique photographs. If they are taken from a  low angle earth surface- aircraft, they are called low oblique and photographs taken from a high angle are called high or steep oblique.

Vertical aerial photograph:

Vertical photographs are taken straight down. They are mainly used in photogrammetry and image interpretation. Pictures that will be used in photogrammetry are traditionally taken with special large-format cameras with calibrated and documented geometric properties.

Aerial photographs are often combined. Depending on their purpose it can be done in several ways, of which a few are listed below.

Vertical aerial

Orthophotos:

Vertical photographs are often used to create orthophotos, alternatively known as orthophotomaps, photographs, which have been geometrically corrected to be usable as a map.

Single-lens mapping (metric) cameras:

The lens cone assembly consists of a single, expensive, multiple-element lens.

Multiple-lens (multiple band) cameras:

Photographs taken simultaneously in several regions (bands) of the EM spectrum.

Panoramic cameras:

Use a rotating lens (or prism) to produce a narrow strip of imagery perpendicular to the flight line.

Digital Cameras:

It uses an area array of solid-state charge-coupled device (CCD) detectors.