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planimetric

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Journal Article

Planimetric Response of the Kerala Shoreline to the Monsoon of 1979 Available to Purchase

K. P. Thrivikramji
Published: 01 November 1987
Jour. Geol. Soc. India (1987) 30 (5): 414–422.
DOI: https://doi.org/10.17491/jgsi/1987/300509
... of Malabar are less severely eroded than those of Southern and Central Kerala. Copyright © 1987 Geological Society of India 1987 Geological Society of India JOURNA.L GEOLOGICAL SOCIETY OF INDIA Vol. 30. Nov. 1987, pP. 414 to 422 Planimetric response of the Kerala shoreline to· the monsoon of 1979 K. P...
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Journal Article

On the planimetric shape of Wreck Bay, Vancouver Island; discussion Available to Purchase

W. F. Tanner, P. H. LeBlond, J. M. Bremner
Published: 01 March 1976
Journal of Sedimentary Research (1976) 46 (1): 258–261.
DOI: https://doi.org/10.1306/212F6F2D-2B24-11D7-8648000102C1865D
View PDF for article title, On the <span class="search-highlight">planimetric</span> shape of Wreck Bay, Vancouver Island; discussion
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Journal Article

Relations between Planimetric and Hypsometric Variables in Third- and Fourth-Order Drainage Basins Available to Purchase

DAVID N. WILCOCK
Journal: GSA Bulletin
Published: 01 January 1975
GSA Bulletin (1975) 86 (1): 47–50.
DOI: https://doi.org/10.1130/0016-7606(1975)86<47:RBPAHV>2.0.CO;2
...DAVID N. WILCOCK Abstract Analyses of relief distribution and drainage distribution within individual drainage basins suggest that relative density (F/D 2 ), a dimensionless variable describing a planimetric characteristic of stream organization in a basin, is related to the hypsometric integral...
View PDF for article title, Relations between <span class="search-highlight">Planimetric</span> and Hypsometric Variables in Third- and Fourth-Order Drainage Basins
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Journal Article

On the planimetric shape of Wreck Bay, Vancouver Is Available to Purchase

J. M. Bremner, P. H. LeBlond
Published: 01 December 1974
Journal of Sedimentary Research (1974) 44 (4): 1155–1165.
DOI: https://doi.org/10.1306/212F6C62-2B24-11D7-8648000102C1865D
...J. M. Bremner; P. H. LeBlond Abstract The planimetric shape of Wreck Bay has been studied by fitting various segments of the bay to theoretical logarithmic spiral curves, and by using the characteristics of incident swell to estimate longshore sediment transport along the beach GeoRef, Copyright...
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(A) Planimetric and cross-sectional views of a sample channel stretch representing the boundaries of the active channel bed as mapped in 2009 and 2019, and the combined active channel (AC) footprint, together with the spatial partitioning of topographic change (i.e., aggradation and degradation) into in-channel and lateral change in alluvial sediment storage. (B) Planimetric and cross-sectional views of a sample canyon stretch representing the boundaries of the active channel bed (solid lines) and the canyon walls (dotted lines) as mapped in 2009 and 2019, and the combined active channel (AC) footprint, together with the spatial partitioning of topographic change into three geomorphic components: landslide-related (L), purely fluvial (F), and mixed (M). The latter represents a transition zone where landslide footprints (in 2009) and the active channel bed (in 2019) overlap.

(A) Planimetric and cross-sectional views of a sample channel stretch repre... Available to Purchase

Published: 22 June 2023
Figure 3. (A) Planimetric and cross-sectional views of a sample channel stretch representing the boundaries of the active channel bed as mapped in 2009 and 2019, and the combined active channel (AC) footprint, together with the spatial partitioning of topographic change (i.e., aggradation
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Shows (a) the planimetric shift of the streams and (b) systematic sampling points for RMS error calculation.

Shows (a) the planimetric shift of the streams and (b) systematic sampl... Available to Purchase

Published: 01 August 2017
Fig.2. Shows (a) the planimetric shift of the streams and (b) systematic sampling points for RMS error calculation.
Image
Planimetric map and measurement of apparent right-lateral offset of channel margin of glacial-fluvial unit 3b in Aplodontia slot trenches. Projection lines illustrate three estimates of right-lateral offset: blue lines show our best estimate, projected on same trend as channel margin in south slot trench; purple and orange lines illustrate estimates of minimum and maximum right-lateral slip, respectively. Note the numerous fault traces in the east wall (Fig. 5A) that coalesce into a simple single trace at the base of the west wall. See Supplemental Figure S4 (see text footnote 4) for detailed logs of slot trench walls.

Planimetric map and measurement of apparent right-lateral offset of channel... Open Access

Published: 01 December 2014
Figure 8. Planimetric map and measurement of apparent right-lateral offset of channel margin of glacial-fluvial unit 3b in Aplodontia slot trenches. Projection lines illustrate three estimates of right-lateral offset: blue lines show our best estimate, projected on same trend as channel margin
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Planimetric map and measurement (with sources of uncertainties) of apparent right-lateral offset of distinctive bedrock fault zone in Boundary slot trench. See Supplemental Figure S5 (see text footnote 5) for detailed logs of slot trench walls.

Planimetric map and measurement (with sources of uncertainties) of apparent... Open Access

Published: 01 December 2014
Figure 9. Planimetric map and measurement (with sources of uncertainties) of apparent right-lateral offset of distinctive bedrock fault zone in Boundary slot trench. See Supplemental Figure S5 (see text footnote 5 ) for detailed logs of slot trench walls.
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The planimetric distribution of the faults at the bottom of Pliocene sequence (A, about 5.3 Ma) and Oligocene sequence (B, about 38 Ma), in Bohai Bay. Map C is the 3D seismic coherency time slice (800 ms) within the Neogene sequence of the area marked in Map A.

The planimetric distribution of the faults at the bottom of Pliocene sequen... Available to Purchase

Published: 01 July 2014
Figure 6 The planimetric distribution of the faults at the bottom of Pliocene sequence (A, about 5.3 Ma) and Oligocene sequence (B, about 38 Ma), in Bohai Bay. Map C is the 3D seismic coherency time slice (800 ms) within the Neogene sequence of the area marked in Map A.
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Planimetric map of lithologies and sample location points in the central Noranda area, Quebec.

Planimetric map of lithologies and sample location points in the central No... Available to Purchase

Published: 01 February 2010
Plate 28 Planimetric map of lithologies and sample location points in the central Noranda area, Quebec.
Image
Figure 3. Planimetric maps showing canyon of the side-valley tributary, upper- and lower-fan segments, and main axial valley channel floodplain at the four study sites. Cross section (XS) and core and auger sediment sample locations are indicated. (A) Sisters Gulch. (B) Hamilton Gulch. (C) Lost Gulch. (D) Buried Log Gulch. LF—lower fan, FP—floodplain. In A and B, south points up.

Figure 3. Planimetric maps showing canyon of the side-valley tributary, upp... Available to Purchase

Published: 01 July 2004
Figure 3. Planimetric maps showing canyon of the side-valley tributary, upper- and lower-fan segments, and main axial valley channel floodplain at the four study sites. Cross section (XS) and core and auger sediment sample locations are indicated. (A) Sisters Gulch. (B) Hamilton Gulch. (C) Lost
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Planimetric development of cliff top recession, average scenario.

Planimetric development of cliff top recession, average scenario. Available to Purchase

Published: 01 August 2001
Fig. 16. Planimetric development of cliff top recession, average scenario.
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—Planimetric map showing location of Pierce Canyon deposit, Black Range, Sierra County.

—Planimetric map showing location of Pierce Canyon deposit, Black Range, Si... Available to Purchase

Published: 01 October 1951
FIG. 4. —Planimetric map showing location of Pierce Canyon deposit, Black Range, Sierra County.
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—Planimetric, geologic, and assay map of ore beds of Bliss sandstone in part of south end of Caballo Mountains, Sierra County.

—Planimetric, geologic, and assay map of ore beds of Bliss sandstone in par... Available to Purchase

Published: 01 October 1951
FIG. 7. —Planimetric, geologic, and assay map of ore beds of Bliss sandstone in part of south end of Caballo Mountains, Sierra County.
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Summary of fault topology from virtual outcrop models, after Sanderson and Nixon (2015). (a) Sample windows and topology superimposed onto a planimetrically correct orthorectified outcrop model of Alltan Na Bradhan. Right, topological results plotted onto a ternary diagram (Sanderson and Nixon 2015). (b) Sample windows and topology superimposed onto a planimetrically correct orthorectified outcrop model of Cathair Dhubh. (c) Summary of node and branch classifications from outcrops shown. (d) Maximum magnification of model in (b) showing the resolution of the model and extreme density of fractures present including uninterpreted fractures below viewing resolution during interpretation.

Summary of fault topology from virtual outcrop models, after Sanderson and... Open Access

Published: 17 February 2023
Fig. 10. Summary of fault topology from virtual outcrop models, after Sanderson and Nixon (2015) . ( a ) Sample windows and topology superimposed onto a planimetrically correct orthorectified outcrop model of Alltan Na Bradhan. Right, topological results plotted onto a ternary diagram
Journal Article

Empirical Analysis of Landslide Runout in Late Pleistocene Glacial Strata in the Eastern Salish Lowland, Washington Available to Purchase

Mark P. Molinari, Carla R. Woodworth, Cody R. Gibson, Michelle Deng
Published: 17 February 2025
Environmental & Engineering Geoscience (2025) 31 (1): 51–65.
DOI: https://doi.org/10.21663/EEG-D-24-00046
... that the volume ( V ) and planimetric area ( A ) data for these landslides plot within the scatter of landslide data points used by Griswold and Iverson (2008) to develop the best-fit power-law relationship ( A = 20 V 2/3 ) for planimetric area of non-volcanic debris flows. The landslides from the 2014–2017...
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Image
Bar graphs to show statistical analysis of results in Experiment 2; bentonite clays only; asterisk denotes statistical significance (p &lt; 0.05); graphs show means while statistics were conducted on medians. A) Comparison of impression depths before and after rewetting of surface in Experiment 2 (N = 8). B) Comparison of impression planimetric areas before and after rewetting of surface (N = 8). C) Effects of factors on impression depth difference (N = 24 for two variables, N = 16 for three variables). D) Effects of factors on planimetric area difference (N = 24 for two variables, N = 16 for three variables).

Bar graphs to show statistical analysis of results in Experiment 2; bentoni... Available to Purchase

Published: 01 July 2010
in Experiment 2 ( N = 8). B) Comparison of impression planimetric areas before and after rewetting of surface ( N = 8). C) Effects of factors on impression depth difference ( N = 24 for two variables, N = 16 for three variables). D) Effects of factors on planimetric area difference ( N = 24 for two
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Bar graphs to show statistical analysis of Experiment 1. Asterisk denotes statistical significance (p &lt; 0.05); graphs show means while statistics were conducted on medians. A) Comparison of impression depth before and after drying in Experiment 1 for bentonite only (N = 8). B) Comparison of planimetric area before and after drying (N = 24 for bentonite, N = 12 for kaolinite). C) Effects of experimental factors on impression depth difference (after drying minus before drying) (N = 36 for two variables, N = 24 for three variables). D) Effects of experimental factors on planimetric area difference (after drying minus before drying) (N = 36 for two variables, N = 24 for three variables).

Bar graphs to show statistical analysis of Experiment 1. Asterisk denotes s... Available to Purchase

Published: 01 July 2010
) Comparison of planimetric area before and after drying ( N = 24 for bentonite, N = 12 for kaolinite). C) Effects of experimental factors on impression depth difference (after drying minus before drying) ( N = 36 for two variables, N = 24 for three variables). D) Effects of experimental factors
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Bar graphs to show statistical analysis of results in Experiment 2 after drying of the rewetted surfaces, bentonite clays only; asterisk denotes statistical significance (p &lt; 0.05); graphs show means while statistics were conducted on medians. A) Comparison of impression depths before and after drying of rewetted surface (N = 8). B) Comparison of impression planimetric areas before and after drying of rewetted surface (N = 8). C) Effects of factors on impression depth difference (after drying minus before drying) (N = 24 for two variables, N = 16 for three variables). D) Effects of factors on planimetric area difference (after drying minus before drying) (N = 24 for two variables, N = 16 for three variables).

Bar graphs to show statistical analysis of results in Experiment 2 after dr... Available to Purchase

Published: 01 July 2010
before and after drying of rewetted surface ( N = 8). B) Comparison of impression planimetric areas before and after drying of rewetted surface ( N = 8). C) Effects of factors on impression depth difference (after drying minus before drying) ( N = 24 for two variables, N = 16 for three variables
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- Orthophoto mosaic of Museo di Zoologia whit representation of different forms of degradation on the façades of building. On the bottom right, the planimetric plan is shown (for the location see the Fig. 2).

- Orthophoto mosaic of Museo di Zoologia whit representation of different f... Available to Purchase

Published: 01 October 2021
Fig. 9 - Orthophoto mosaic of Museo di Zoologia whit representation of different forms of degradation on the façades of building. On the bottom right, the planimetric plan is shown (for the location see the Fig. 2 ).