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... Each cartographic unit is characterized in the map by a colour, indicative of the age or type of rock, that could have a superimposed pattern indicating the lithology or some geological process (figure 2). They are identified through the “epigraphs” or map unit labels. An epigraph is a code formed b ...
... Each cartographic unit is characterized in the map by a colour, indicative of the age or type of rock, that could have a superimposed pattern indicating the lithology or some geological process (figure 2). They are identified through the “epigraphs” or map unit labels. An epigraph is a code formed b ...
II. Subject Matter
... Parallel Lines- are lines in a plane which do not meet; that is, two lines in a plane that do not intersect or touch each other at any point are said to be parallel. Transversal- is a line that intersects two or more lines (in the same plane). When lines intersect, angles are formed in several locat ...
... Parallel Lines- are lines in a plane which do not meet; that is, two lines in a plane that do not intersect or touch each other at any point are said to be parallel. Transversal- is a line that intersects two or more lines (in the same plane). When lines intersect, angles are formed in several locat ...
3-3 Practice A Proving Lines Parallel
... �4 are a linear pair, so m�3 � m�4 � 180� by the Linear Pair Theorem. But the Angle Addition Postulate shows that m�4 � m�ACF � m�FCD, so by substitution m�3 � m�ACF � m�FCD � 180�. m�1 � m�ACF by the Alternate Interior Angles Theorem and m�2 � m�FCD by the Corresponding Angles Postulate. Therefore ...
... �4 are a linear pair, so m�3 � m�4 � 180� by the Linear Pair Theorem. But the Angle Addition Postulate shows that m�4 � m�ACF � m�FCD, so by substitution m�3 � m�ACF � m�FCD � 180�. m�1 � m�ACF by the Alternate Interior Angles Theorem and m�2 � m�FCD by the Corresponding Angles Postulate. Therefore ...
Unit 2.1 The Parallel Postulate and Special Angles
... two points of the plane lies entirely within the plane. Whereas the postulate that follows characterizes Euclidean geometry, the Perspective on Applications section near the end of this chapter discusses alternative geometries. Postulate 10, the Euclidean Parallel Postulate, is easy to accept becaus ...
... two points of the plane lies entirely within the plane. Whereas the postulate that follows characterizes Euclidean geometry, the Perspective on Applications section near the end of this chapter discusses alternative geometries. Postulate 10, the Euclidean Parallel Postulate, is easy to accept becaus ...
Parallel Lines with Cabri Jr
... Focus: This lesson will show students the relationships that exist with angles formed by parallel lines and transversals. Students will reinforce vocabulary that relates to these angles. This lesson uses the Cabri Jr. APP for the TI-83/84. The lesson can be used as a directed lesson or given to the ...
... Focus: This lesson will show students the relationships that exist with angles formed by parallel lines and transversals. Students will reinforce vocabulary that relates to these angles. This lesson uses the Cabri Jr. APP for the TI-83/84. The lesson can be used as a directed lesson or given to the ...
Parallel Lines and Transversals
... Parallel Lines and Transversals eight angles are formed. When a transversal intersects two lines, _____ These angles are given special names. Alternate Interior angles are between the two lines on the opposite sides of the transversal. Ex. 4 and 6, 3 and 5 Consectutive Interior angles between the t ...
... Parallel Lines and Transversals eight angles are formed. When a transversal intersects two lines, _____ These angles are given special names. Alternate Interior angles are between the two lines on the opposite sides of the transversal. Ex. 4 and 6, 3 and 5 Consectutive Interior angles between the t ...
Contour line
A contour line (also isoline, isopleth, or isarithm) of a function of two variables is a curve along which the function has a constant value. It is a cross-section of the three-dimensional graph of the function f(x, y) parallel to the x, y plane. In cartography, a contour line (often just called a ""contour"") joins points of equal elevation (height) above a given level, such as mean sea level. A contour map is a map illustrated with contour lines, for example a topographic map, which thus shows valleys and hills, and the steepness of slopes. The contour interval of a contour map is the difference in elevation between successive contour lines.More generally, a contour line for a function of two variables is a curve connecting points where the function has the same particular value. The gradient of the function is always perpendicular to the contour lines. When the lines are close together the magnitude of the gradient is large: the variation is steep. A level set is a generalization of a contour line for functions of any number of variables.Contour lines are curved, straight or a mixture of both lines on a map describing the intersection of a real or hypothetical surface with one or more horizontal planes. The configuration of these contours allows map readers to infer relative gradient of a parameter and estimate that parameter at specific places. Contour lines may be either traced on a visible three-dimensional model of the surface, as when a photogrammetrist viewing a stereo-model plots elevation contours, or interpolated from estimated surface elevations, as when a computer program threads contours through a network of observation points of area centroids. In the latter case, the method of interpolation affects the reliability of individual isolines and their portrayal of slope, pits and peaks.