a) is a contour plot of gravity anomaly computed via the
![](https://www.researchgate.net/publication/336848246/figure/fig1/AS:818937960873986@1572261433946/a-is-a-contour-plot-of-gravity-anomaly-computed-via-the-difference-between-gravity-at.jpg)
Download scientific diagram | (a) is a contour plot of gravity anomaly computed via the difference between gravity at the Geoid and normal gravity at the reference ellipsoid. The data in Table 1 were used for the plotting. The minimum and maximum contour values are 0.00001 and 0.00014. The contour were plotted in Surfer 11 software, applying kriging gridding method at 0.000001 contour interval. (b) is the surface plot of (a) with minimum and maximum values as 0.00001 and 0.00014 respectively. from publication: A Gravimetric Approach for the Determination of Orthometric heights in Akure Environs, Ondo State, Nigeria | An important component in position determination of any point is its height. Orthometric height determination has a significant role in geodesy, and it has wide-ranging applications in numerous fields and activities. Orthometric height is the height above or below the geoid | Nigeria, Global Positioning System and Gravity | ResearchGate, the professional network for scientists.
![](https://pubs.usgs.gov/ds/321/ilinoh_cba.jpg)
USGS Data Series 321: Illinois, Indiana, and Ohio Magnetic and Gravity Maps and Data: A Website for Distribution of Data
![](https://static.cambridge.org/binary/version/id/urn:cambridge.org:id:binary-alt:20230905150446-20745-mediumThumb-27892fig7_1.jpg?pub-status=live)
Isostasy and the Origin of Geological Features in the Continents and Oceans (Chapter 7) - Isostasy and Flexure of the Lithosphere
![](https://www.researchgate.net/publication/327444458/figure/fig3/AS:799100614217728@1567531841063/a-is-a-contour-plot-of-gravity-anomaly-computed-via-the-difference-between-gravity-at.jpg)
a) is a contour plot of gravity anomaly computed via the difference
![](https://www.kgs.ku.edu/Publications/Bulletins/237/Xia1/gifs/fig3.png)
KGS--Bulletin 237--Geophysical Model from Potential-field Data in Montgomery County, Kansas
![](https://www.researchgate.net/publication/336848246/figure/fig1/AS:818937960873986@1572261433946/a-is-a-contour-plot-of-gravity-anomaly-computed-via-the-difference-between-gravity-at.jpg)
a) is a contour plot of gravity anomaly computed via the difference
![](https://www.researchgate.net/profile/Tata-Herbert/publication/336848246/figure/fig3/AS:818937965056000@1572261434019/a-contour-plot-of-orthometric-height-via-gravimetric-geoid-and-ellipsoidal-height-and_Q320.jpg)
a) is a contour plot of gravity anomaly computed via the difference
![](https://i0.wp.com/mycartablog.com/wp-content/uploads/2012/01/surfer-data-color.png)
Visualization tips for geoscientists: Surfer
![](https://www.researchgate.net/profile/Tata-Herbert/publication/324872373/figure/fig1/AS:837108306571266@1576593581921/Login-for-Staffs_Q320.jpg)
Tata HERBERT B.TECH M.TECH and PhD in Surveying and
![](https://pubs.usgs.gov/ds/355/orcba.jpg)
USGS Data Series 355: Oregon Magnetic and Gravity Maps and Data: A Web Site for Distribution of Data
![](https://cdnintech.com/media/chapter/81073/1512345123/media/F1.png)
New Semi-Inversion Method of Bouguer Gravity Anomalies Separation
![](https://www.kgs.ku.edu/Publications/Bulletins/237/Xia1/gifs/fig13.png)
KGS--Bulletin 237--Geophysical Model from Potential-field Data in Montgomery County, Kansas
![](http://portal.amelica.org/ameli/journal/594/5943503004/5943503004_gf4.png)
Gravity Studies at the Cerro Machín volcano, Colombia