Morphologically, these anomalies correspond to the subvertical tensile faults.
Yu. O. Kuzmin 2018, 'Recent anomalous deformation of the ground surface in fault zones: shear or tensilefaulting?', Geodinamika i Tektonofizikahttps://www.gt-crust.ru/jour/article/view/633. Retrieved from DOAJ CC BY 4.0 (https://creativecommons.org/licenses/by-sa/4.0/legalcode)
Fields and bunches of kimberlite pipes are concentrated within boundaries of conducting subvertical zones.
Е. В. Поспеева 2017, 'Conducting lithospheric heterogeneities as a criterion of predictive assessment forpromising diamond areas (on the example of Siberian kimberlite province)', Zapiski Gornogo Institutahttp://pmi.spmi.ru/index.php/pmi/article/view/5235. Retrieved from DOAJ CC BY 4.0 (https://creativecommons.org/licenses/by-sa/4.0/legalcode)
Main faults have east – west direction and are subvertical.
Magda Čarman, Borut Petkovšek, Tomaž Budkovič 2009, 'Geology of Pletovarje motorway tunnel (Slovenia)', Geologijahttp://www.geologija-revija.si/dokument.aspx?id=1052. Retrieved from DOAJ CC BY 4.0 (https://creativecommons.org/licenses/by-sa/4.0/legalcode)
Some of these fractures are subvertical and due to contraction, and coincide with the columnar jointing of the ignimbrites.
Arribas, A., Figueroa, E. 1985, 'Las mineralizaciones de uranio en las rocas volcánicas de Macusani. Puno (Perú)',Estudios Geologicoshttp://estudiosgeol.revistas.csic.es/index.php/estudiosgeol/article/view/714/758. Retrieved from DOAJ CC BY 4.0 (https://creativecommons.org/licenses/by-sa/4.0/legalcode)
In this paper temperature changes in a subvertical zone over a hydrocarbon deposit and outside its contour are analyzed.
Vagif G. Gadirov, Lev V. Eppelbaum 2015, 'Density-thermal dependence of sedimentary associations calls to reinterpreting detailedgravity surveys', Annals of Geophysicshttp://www.annalsofgeophysics.eu/index.php/annals/article/view/6672. Retrieved from DOAJ CC BY 4.0 (https://creativecommons.org/licenses/by-sa/4.0/legalcode)
Spines are dense and low volume and contain small skeletal shaped pores, and subvertical zones of sigmoidal pores.
Emma Rhodes, Ben M. Kennedy, Yan Lavallée, Adrian Hornby, Adrian Hornby, Matt Edwards,Gustavo Chigna 2018, 'Textural Insights Into the Evolving Lava Dome Cycles at Santiaguito Lava Dome, Guatemala',Frontiers in Earth Sciencehttp://journal.frontiersin.org/article/10.3389/feart.2018.00030/full. Retrieved from DOAJ CC BY 4.0 (https://creativecommons.org/licenses/by-sa/4.0/legalcode)
Longitudinal colouration around the entire shell circumference supports vertical or subvertical life orientation in both described species.
Štěpán Manda, Vojtěch Turek 2015, 'Colour patterns on Silurian orthocerid and pseudorthocerid conchs from Gotland – palaeoecologicalimplications', Estonian Journal of Earth Scienceshttp://www.kirj.ee/public/Estonian_Journal_of_Earth_Sciences/2015/issue_1/earth-2015-1-74-79.pdf. Retrieved from DOAJ CC BY 4.0 (https://creativecommons.org/licenses/by-sa/4.0/legalcode)