Everything about Geologic Map totally explained
A
geologic map or
geological map is a special-purpose
map made to show
geological features.
The stratigraphic contour lines are drawn on the surface of a selected deep
stratum, so that they can show the topographic trends of the strata under the ground. It isn't always possible to properly show this when the strata are extremely fractured, mixed, in some discontinuities, or where they're otherwise disturbed.
Strike and dip symbols consist of (at minimum) a long line, a number, and a short line which are used to indicate tilted beds. The long line is the strike line, which shows the true horizontal direction along the bed, the number is the dip or number of degrees of tilt above horizontal, and the short line is the dip line, which shows the direction of tilt.
History
The oldest preserved geologic map is the
Turin papyrus, made around 1150 BCE for
gold deposits in Egypt.
A fascinating story of the first modern geologic map is told in
The Map that Changed the World, by Simon Winchester. It's the story of
William Smith, a canal digger who created the first geologic map of Great Britain in 1819, but ended up in debtor's prison and lived homeless for 10 years until he was recognized for his work by King William IV in 1831. (Harper-Collins publishers, 2202. ISBN 0-06-093180-9)
Maps and Mapping across the globe
United States
In the
United States, geologic maps are usually superimposed over a
topographic map (and at times over other base maps) with the addition of a color mask with letter symbols to represent the kind of
geologic unit. The color mask denotes the exposure of the immediate
bedrock, even if obscured by soil or other cover. Each area of color denotes a geologic unit or particular
rock formation (as more information is gathered new geologic units may be defined). However, in areas where the bedrock is overlain by a significantly thick
unconsolidated burden of
till,
terrace deposits,
loess deposits, or other important feature, these are shown instead.
Stratigraphic contour lines,
fault lines, strike and dip symbols, are represented with various symbols as indicated by the map key. Whereas topographic maps are produced by the
United States Geological Survey in conjunction with the states, geologic maps are usually produced by the individual
states. There are almost no geologic map resources for some states, while a few states, such as
Kentucky, are extensively mapped geologically.
United Kingdom
In the
United Kingdom the term
geological map is used. The UK and
Isle of Man have been extensively mapped by the
British Geological Survey since 1835; a separate Geological Survey of Northern Ireland (drawing on BGS staff) has operated since 1947.
Two 1:625,000 scale maps cover the basic geology for the UK. More detailed sheets are available at scales of 1:250,000, 1:50,000 and 1:10,000. The 1:625,000 and 1:250,000 scales show both onshore and offshore geology (the 1:250,000 series covers the entire UK
continental shelf), whilst other scales generally cover exposures on land only.
Sheets of all scales (though not for all areas) fall into two categories:
» ::
Superficial deposit maps (previously known as
solid and drift maps) show both bedrock
and the deposits on top of it.
::
Bedrock maps (previously known as
solid maps) show the underlying rock, without superficial deposits.
The maps are superimposed over a topographic map base produced by
Ordnance Survey, and use symbols to represent fault lines, strike and dip or geological units,
boreholes etc. Colors are used to represent different geological units. Explanatory booklets (memoirs) are produced for many sheets at the 1:50,000 scale.
Small scale thematic maps (1:1,000,000 to 1:100,000) are also produced covering
geochemistry,
gravity anomaly,
magnetic anomaly,
groundwater, etc.
Further Information
Get more info on 'Geologic Map'.
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