The continental shelf is the term for part of a continent that extends outward from the landmass beneath shallow seawater. The drop-off point of a continental shelf is called the shelf break. From this point, the continental goes down to the deep ocean floor.
Magnetic compass failure in higher latitudes is primarily caused by the convergence of lines of magnetic force at the magnetic poles. This convergence results in the magnetic compass needle becoming unreliable and unstable, making it difficult to determine accurate directions. In addition, the Earth's magnetic field becomes weaker at higher latitudes, further contributing to compass inaccuracies.
Differentiate term by term. d/dx[X2 + 2X) = 2X + 2 slope(m) = 2 ------------------
the slope is 2, the number in front of the 'x' term
The other term for slope is gradient
The term for the part of a continent that extends beyond the shoreline beneath relatively shallow seawater is the continental shelf. It is an underwater extension of the continent that slopes gently from the shore to the ocean depths.
3x + y - 4 = 0 y = -3x + 4 The slope is equivalent to the coefficient term of 'x', also known as 'm'. Therefore, the slope is -3.
The equation y = mx + c, is the equation of a line in slope-intercept form. The m term is the slope or first order deriviative (dy/dx) of the line, and the c term is the y-axis intercept.
It is its slope or gradient.
solve each equation in terms of y and the slope is the value in front of the x term; the slope of one of them is the negative inverse slope of the other p/q = 3/2
Yes, the slope of a line is the coefficient of the x-term in the line.
The coefficient of the x term gives the gradient of the slope.