azimuthal survey - определение. Что такое azimuthal survey
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Что (кто) такое azimuthal survey - определение

MAP PROJECTION
Lambert azimuthal projection; Azimuthal equal-area projection; Lambert net; Schmidt plot; Lambert asimuthal projection; LEAA projection; Lambert Azimuthal Equal Area; Lambert azimuthal equal area; Azimuthal equal area; Laea; Lambert azimuthal map projection
  • The Lambert azimuthal equal-area projection with [[Tissot's indicatrix]] of deformation.
  • Animation of a Lambert projection. Each grid cell maintains its area throughout the transformation. In this animation, points on the equator remain always on the <math>z=0</math> plane.
  • In this animated Lambert projection, the south pole is held fixed.
  • Lambert azimuthal equal-area projection of the world. The center is 0° N 0° E. The antipode is 0° N 180° E, near [[Kiribati]] in the [[Pacific Ocean]]. That point is represented by the entire circular boundary of the map, and the ocean around that point appears along the entire boundary.
  • cross section]]al view of the sphere and a plane tangent to it at ''S''. Each point on the sphere (except the antipode) is projected to the plane along a circular arc centered at the point of tangency between the sphere and plane.

Survey vessel         
  • oceanographic]] research, June 2011
  • Clintons ''Northern Storm'' in the harbour of [[Ystad]] 7 July 2021.
  • Hydrographic vessel Marshal Gelovani
TYPE OF RESEARCH VESSEL
Survey ship; Survey ships; Autonomous survey vessel
A survey vessel is any type of ship or boat that is used for underwater surveys, usually to collect data for mapping or planning underwater construction or mineral extraction. It is a type of research vessel, and may be designed for the purpose, modified for the purpose or temporarily put into the service as a vessel of opportunity, and may be crewed, remotely operated, or autonomous.
Geological survey         
SYSTEMATIC INVESTIGATION OF THE GEOLOGY IN A REGION FOR THE PURPOSE OF CREATING A GEOLOGICAL MAP OR MODEL
Geological Survey; National Geological Survey; Geological surveys
A geological survey is the systematic investigation of the geology beneath a given piece of ground for the purpose of creating a geological map or model. Geological surveying employs techniques from the traditional walk-over survey, studying outcrops and landforms, to intrusive methods, such as hand augering and machine-driven boreholes, to the use of geophysical techniques and remote sensing methods, such as aerial photography and satellite imagery.
Survey marker         
  • Reference marker for triangulation station in upper photo
  • A cotton spindle spike in [[Tel Aviv]] pavement, used as a marker for public area [[cadastral surveying]].
  • Marker for triangulation station, indicated by triangle in center
OBJECT PLACED TO MARK A POINT
Survey markers; Survey monument; Survey monuments; Surveyor marks; Surveyor's marks; Geodetic mark; Geodetic marker; Survey mark; Land survey marker; Geodesy marker
Survey markers, also called survey marks, survey monuments, or geodetic marks, are objects placed to mark key survey points on the Earth's surface. They are used in geodetic and land surveying.

Википедия

Lambert azimuthal equal-area projection

The Lambert azimuthal equal-area projection is a particular mapping from a sphere to a disk. It accurately represents area in all regions of the sphere, but it does not accurately represent angles. It is named for the Swiss mathematician Johann Heinrich Lambert, who announced it in 1772. "Zenithal" being synonymous with "azimuthal", the projection is also known as the Lambert zenithal equal-area projection.

The Lambert azimuthal projection is used as a map projection in cartography. For example, the National Atlas of the US uses a Lambert azimuthal equal-area projection to display information in the online Map Maker application, and the European Environment Agency recommends its usage for European mapping for statistical analysis and display. It is also used in scientific disciplines such as geology for plotting the orientations of lines in three-dimensional space. This plotting is aided by a special kind of graph paper called a Schmidt net.