Part A
Geologic Map Basics
Geologic maps show the distribution of different rock units and structures (like faults and folds) at the surface. These maps are the fundamental medium by which a geologist describes and interprets the geology and geologic history of an area. I like to view geologic maps as unique earth science portraits drawn by a scientist-artist. Traditionally, a geologic map is created by a field geologist who hikes across an area and describes the composition and distribution of various rock types encountered. A geologic map begins to take shape as different map units are drawn and labeled on a topographic base map. Figure 3-2 shows a geologic map for an area of the Grand Canyon in Arizona. This activity is very time-consuming and may take days, weeks, months, or years, depending on the size of the area, complexity of the geology, the difficulty of the terrain, etc. Data can also be collected remotely, like from an orbiting satellite or automated rover. This is how we have mapped the geology of most of the Moon and several other planetary bodies.
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Figure 3-2. A color geologic map of an area of the Grand Canyon. |
Map Content
There are many types of geologic maps, and the layout and content can vary widely. These maps may be in color or black & white, small or large in size, very simple or highly detailed, hand-drawn or digital, etc. Most maps will include some or all of the components highlighted in Figure 3-3.
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Figure 3-3. Typical content of a geologic map. |
Let's review a few of the more important items:
Title & author(s) - Maps should be titled, with the authors listed.
Map scales - As with topographic maps, graphical and ratio scales are typically included so the reader can understand distances and areas represented on a geologic map. Remember from Lab 2, a ratio scale is simply a comparison of map distances with actual "real world" distances.
Topographic base map - Geologic maps are commonly constructed on a topographic base, but not always. If present, the topographic contours are typically printed lighter than the geologic lines. When topo base maps are included in the map, a contour interval may also be listed. Geographic location of the map area may also be included.
North arrow - All maps should include a north arrow to show orientation of geographic north. Some will show the difference between geographic north and magnetic north (a.k.a. the magnetic declination).
Spatial coordinate markings or grids - Many maps will include coordinate information (latitude/longitude, UTM, etc.) allowing determination of precise locations on the map.
Explanation of Map Units - All maps should have a description of the geologic map units (e.g., names, ages, symbols, etc.) so the reader knows what the different units represent. Map units are listed from oldest (at the bottom) to youngest (at the top). Brief descriptions of the map units and special map symbols are commonly present. If you see a symbol on the map that you do not recognize, then look in the explanation!
Map Units - The core data of any geologic map lies in the distribution of map units, each having distinctive physical characteristics. A fundamental map unit is a Formation, which is a rock unit (e.g., the Galeros Formation) with unique characteristics (such as color, texture, rock type, and/or age) that can be distinguished from other units in the field. A formation must be mappable, meaning that it must cover a large enough area to be shown on a geologic map. A lesser unit is called a Member (e.g., the Carbon Canyon Member of the Galeros Formation) , and several members combined can make a formation. Alternatively, several similar formations can be joined together into a larger Group (e.g., the Chuar Group), and groups can likewise be joined into a Supergroup (e.g., the Grand Canyon Supergroup). Rock formations are typically named after the locations (type localities) where the rock unit was first described or is best represented, but can also refer to the composition of the rock unit or just simply be a name.
Map unit boundaries are delineated by contacts. Solid line contacts mean that the location of the map unit boundary is relatively sharp or well-located, whereas a dashed contact may imply a gradational or less well-located boundary. Dotted contacts represent the inferred location of unit boundaries that are covered by overlying material. There are other types of contacts, depending on the type of the geologic feature present (e.g., rock units, faults, etc.). Remember, contacts are not contour lines (which are related to elevation).
Map Unit Symbols - Map units have labels or symbols that identify them. The exact symbols used on different maps can vary widely, but with most map unit symbols, the first letter is capitalized and typically represents the geologic age of the formation, whereas the second (lower case) letter is descriptive of the formation name, rock composition, etc. For example, the Hickey Formation has the map unit symbol Tbm, where "T" is the age of the formation (Tertiary Period, 66-2.58 Ma), "b" is basalt (the main rock type of the formation), and "m" is middle Miocene (a more specific age description). The symbols are printed on the geologic map and in the map unit explanation.
Correlation of Map Units - While the Explanation of Map Units is a text list typically written in age order, some maps will include a Correlation of Map Units, which is a very helpful graphic that shows the age relations of the various map units.
Explanation of Map Symbols - Many other symbols can be used on geologic maps and a key to their explanation is important in understanding the map. Common symbols include different types of map unit and fault contacts, rock orientation symbols (strike and dip), special geologic features (dikes, quartz veins, etc.), sample locations, etc.
Geologic Cross Sections - Maps may include one or more geologic cross sections, which are basically topographic profiles between two or more points on the map that include an interpretation of the geology in the subsurface. The geometry of units below the surface is inferred from the orientation of rock units at the surface. Subsurface geology can also be described from canyon wall exposures, well log data, and various geophysical methods (seismic, gravity, etc.). These figures can be highly interpretive, but are very helpful in visualizing distribution of rock units below the surface. The locations of cross section lines or endpoints are marked on the map. Geologic units may be projected above the profile surface to better show the orientation of geologic structures.
Other data - Maps may include other kinds of data, like location diagrams, data tables, photo imagery, stratigraphic columns, references, etc.
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Example 1 |
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Is a ratio scale included on this map? |
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Yes It's above the map scale at the bottom center of the map |
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Example 2 |
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Map unit Ta includes what kinds of rocks? |
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Andesitic volcanic rocks |
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Example 3 |
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What is the map unit symbol for Quaternary talus? |
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Qt |
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Example 4 |
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Are the location of rock data samples included on this map? |
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Yes Sample locations, ID, and type of data are all included |
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Example 5 |
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What map unit caps Black Mesa in the western part of cross section A-A'? |
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Tbm |
Geology of the Black Canyon City and Squaw Creek Mesa Quadrangles
Now that you've reviewed the layout of a geologic map, let's look more closely at the geology of central Arizona.
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Figure 3-4. The Geology of the Black Canyon City and Squaw Creek Mesa Quadrangles, central Arizona. |
Answer Quiz Me! questions A01 through A20 using the Geology of the Black Canyon City and Squaw Creek Mesa Quadrangles, central Arizona (see the PDF link below).
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Geology of the Black Canyon City and Squaw Creek Mesa Quadrangles, central Arizona |
Author & Map Scale
Explanation of Map Units
Correlation of Map Units
Geologic Map
Cross Sections