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The Stenkvista runestone in Södermanland, Sweden, with its Thor's hammer. The Stenkvista runestone, designated as runic inscription Sö 111 in the Rundata catalog, is a memorial runestone located near the church at Stenkvista, which is two kilometers east of Skogstorp, Södermanland County, Sweden, which was formerly part of the historic Södermanland, and which features a depiction of Thor's ...
Another interesting class of runestone is rune-stone-as-self promotion. Bragging was a virtue in Norse society, a habit in which the heroes of sagas often indulged, and is exemplified in runestones of the time. Hundreds of people had stones carved with the purpose of advertising their own achievements or positive traits. A few examples will ...
To help clear up some of that choice paralysis, we've created a handy guide to compare two popular countertop options: quartz and granite. While both are excellent choices, one may be a better fit ...
A geologist's hammer, rock hammer, rock pick, geological pick, or informally geo pick is a hammer used for splitting and breaking rocks. In field geology, they are used to obtain a fresh surface of a rock to determine its composition, bedding orientation, nature, mineralogy , history, and field estimate of rock strength.
A-type granite is a particular category of the S-I-A-M or 'alphabet' system which classifies granitoids and granitic rock by their photoliths or source. [1] [2] The 'A' stands for Anorogenic or Anhydrous, as these granites are characterized by low water content and a lack of orogenic or transitional tectonic fabric. [3]
HRAs, QSEHRAs, and ICHRAS. Understanding the differences in eligible expenses between HRAs, QSEHRAs, and ICHRAs can help businesses determine which type of plan best fits their needs.
Motorists entering Manhattan’s busiest neighborhoods will now have to pay up to $9 in congestion charges, as New York City’s first-in-the-nation Congestion Relief Zone officially launched Sunday.
I-type granites are a category of granites originating from igneous sources, first proposed by Chappell and White (1974). [1] They are recognized by a specific set of mineralogical, geochemical, textural, and isotopic characteristics that indicate, for example, magma hybridization in the deep crust. [2]