Presentation on theme: "Astronaut Video: Sarychev Volcano Eruption Lithology – rock type of surface rocks and bedrock Structure – folding, faulting and deformation of rocks."— Presentation transcript:
Astronaut Video: Sarychev Volcano Eruption
Lithology – rock type of surface rocks and bedrock Structure – folding, faulting and deformation of rocks Landforms – terrain features formed by natural processes that appear similar wherever they are found (Way 1973); Can be erosional or depositional Drainage patterns – the aggregate of flow channels regardless of whether water is in them now Soils – soil types as expressed on the surface and organized into standard classification schemes
Devil’s Tower (Igneous rock protruding from eroded sedimentary strata) (Air Photo Courtesy Louis Maher, Jr.)
Lithological Units Igneous - rock formed directly from molten mass: intrusive (granite) or extrusive (basalt) are common examples. Sedimentary – sediment deposited and lithified (turned to rock) after being transported by water, wind and/or gravity: sandstone, siltstone, shale, limestone are common examples Metamorphic - formed by action of heat or pressure on previously existing rock: gneiss, schist, slate, and quartzite are common examples
Igneous Rocks (basalt flows) at Craters of the Moon, ID (Air Photo Courtesy Louis Maher, Jr.) What kind of rock is this? What clues are you using?
Sedimentary Rocks (badlands) in South Dakota (Air Photo Courtesy Louis Maher, Jr.) What kind of rock?
Metamorphic Rock from Grand Canyon (not an air photo!) (Courtesy American Geological Institute) What kind of rock? What’s the scale of this photo?
Lithology is an important aspect of geologic mapping Interpretation of lithology from air photos requires knowledge of relationship between the lithology and: Climate Topography Drainage pattern Jointing and faulting Texture Vegetation Photointerpretation clues: tone, size, context, shape, etc. Photointerpreters must be trained to understand these relationships on photos and in the field
Affects the way rocks weather. Affects the associations of vegetation with particular rock types Affects soil formation from rock parent material Affects erosional patterns All of these influence the appearance of different rocks in photos.
Drainage patterns are easy to see on aerial photographs Offer clues to many other geologic characteristics of an area (e.g., topography, bedrock, surface texture and hardness, jointing, etc.) Obvious importance for hydrologic mapping, modeling and management Often influence human land use
Drainage patterns Dendritic: horizontal sediment or uniformly (homogeneous) resistant bedrock; gentle slope Parallel: moderate to steep slopes fine textured deposits or fractured bedrock or in areas of parallel elongate landforms Trellis: dipping or folded bedrock Rectangular: jointed or faulted bedrock Radial: volcanoes, domes, basins Annular: domes or basins Multibasinal - flat-lying glacial terrain; karst (limestone) terrain Contorted: metamorphic rocks disc.gsfc.nasa.gov/.../ geo_images_4/Fig4.1.gif Originally from Howard, 1967 A. DendriticB. Parallel
Rectangular drainage on Volga River (caused by faulting) (Satellite image) What kind of drainage is this? What causes it?
Dendritic drainage pattern (Photo courtesy Michael Collier) Type of drainage?
Topography: flat to hilly Drainage: parallel or internal Photo tone: dark or sometimes spotted Gully type: none (not erosive) Igneous Rocks (basalt flows) at Craters of the Moon, ID (Air Photo Courtesy Louis Maher, Jr.)
Topography: flat or table like (mesas, etc.) but can be highly eroded Drainage: dendritic Photo tone: light and banded (can vary considerably) Gully type: none to deep depending on steepness Sedimentary rocks (sandstone) at Castle Valley, UT (Air Photo Courtesy Louis Maher, Jr.) Where is this? Can you name these features?
Geologic structures are any features caused by deformation of rock (folding, faulting, etc.) Structure is important for trapping hydrocarbons, controlling water flow, understanding stratigraphy, etc. Includes: Strike and dip Folds (e.g., anticlines, synclines, domes, basins, etc.) Faults (e.g., normal, reverse, horst and graben, etc.) Joints Unconformities
Sheep Mountain anticline in Bighorn Basin of Wyoming (Air Photo Courtesy Louis Maher, Jr.) Can you name this Wyoming feature?
Sandstone jointing in Arches National Park (Air Photo Courtesy Louis Maher, Jr.) Type of rock? What are the linear features?
Angular Unconformity (Photo by James St. John, Flickr Creative Commons, flickr: jsj1771) What is this called?
Interpreter looks for changes in tone and texture that represent boundaries between geologic units Works best where vegetation cover is minimal But…can sometimes see changes in underlying strata related to changes in overlying vegetation Can sometimes enhance edges with digital filters Can use stereo techniques to measure elevation changes for calculating dip angles
Geologic map of Wyoming’s Casper Arch (Image Courtesy NASA.)
Geologic structure in California (Image Courtesy of NASA)
Definition of landforms varies with discipline Geologist may have different view than soil scientist or hydrologist Creating a landform key is important aspect of aerial interpretation Landforms are strongly influenced by underlying geology and climate
Coastal and oceanic (e.g., fjord, ismuth, beach, etc.) Erosional landforms (e.g., canyon, cuesta, gully, etc.) Fluvial (river related) landforms (e.g., braided channel) Mountain and glacial landforms (e.g., cirque, peak, etc.) Slope landforms (e.g., terrace, cuesta, plain) Volcanic landforms (e.g., cinder cone, lava flow) Depositional landforms (e.g., alluvial fans) Etc. (there are many ways to think about landforms)
Glacial moraine near Pinedale, Wyoming (Air Photo Courtesy Louis Maher, Jr.) What kind of landform? Where?
Great Sand Dunes, Colorado (Air Photo Courtesy Louis Maher, Jr.)
Identifying landforms on aerial photography uses many clues Topography Drainage pattern Drainage texture Photo tone and texture Vegetation patterns Land use patterns Scale of landform determines scale of imagery necessary to map. Landforms occur across scales.
Soils can be mapped at a wide range of scales and precision 1 st order surveys are most detailed and 5 th order are least Lower (1 st, etc.) order surveys require detail found in air photos Almost all soil mapping requires a combination of field survey and remote sensing Typical project uses manually interpreted aerial photography followed by field work to label the interpreted units
Small plot level1 st order1:8,000 scale Detailed soil map2 nd order1:20,000 scale Soil association map 4 th order1:250,000 scale Statewide soil map5 th order1:1,000,000 scale
Soil survey on air photo (From Wikipedia)
Aerial photography is widely used for various aspects of geology Choice of air photos depends on scale, spectral requirements, etc. Air photo interpretation for geology usually requires a coupled field component Interpreters must have comprehensive knowledge of a broad set of indicators that give clues to underlying geology