Topographic Maps and Landscape Processes Notes
Topographic Maps
- Definition: Maps that represent the elevation and shape of the land using contour lines.
Key Features of Topographic Maps
- North Arrow: Indicates true north direction in relation to the map.
- Magnetic Declination: The angle between true north and magnetic north, affects navigation accuracy.
- Map Scale: Essential for interpreting distances on a map.
- Fractional Scale: A ratio (e.g., 1:24,000) representing map distance to actual distance.
- Graphical Scale: A visual representation of scale, usually as a bar.
- Longitude & Latitude: A coordinate system for pinpointing locations.
- Longitude: Lines running north-south.
- Latitude: Lines running east-west.
- Township-Range-Section: A system dividing land into squares for surveying.
- Equator & Prime Meridian: Define the geographical coordinate system; Equator at 0° latitude, Prime Meridian at 0° longitude.
- Parallels: Lines of latitude that run parallel to each other.
- 7.5 Min Quadrangle: A type of topographic map covering a specific area (7.5’ of latitude and longitude).
Contour Lines and Analysis
- Contour Interval: Vertical distance between contour lines, indicates elevation change.
- Index Contour: Thicker contour lines labeled with elevation values for easier navigation.
- Law of V’s / Streams: Contour lines form a ‘V’ shape crossing streams, with V pointing upstream.
Landscape Analysis Criteria
- Landform: The shape of Earth's surface (mountain, valley, etc.).
- Material: Types of rocks or sediments present in an area.
- Age: Relative or absolute age of the landform.
- Process: Geophysical forces (e.g., erosion, deposition) that formed the land.
Soil and Mass Wasting
Bedrock vs. Regolith
- Bedrock: Solid rock beneath soil.
- Regolith: Loose rock and soil overlaying bedrock.
Types of Material
- Colluvium: Material moved by gravity, typically found at the base of slopes.
- Alluvium: Sediments deposited by running water.
- Drift: Glacial deposits, including till and outwash.
- Lacustrine: Sediments from lake environments.
- Anthropogenic: Landforms made by human activities.
Mass Wasting Types
- Creep: Slow movement of soil downhill.
- Slide: Rapid movement along a surface.
- Flow: Material movement resembling fluid motion.
- Debris Flow: A saturated landslide of water, soil, and rock.
- Mudflow: Fast movement of fine sediment and water.
- Landslide: Rapid downhill motion of rock or soil.
- Rock Fall: Free-fall of rock from steep slopes.
- Solifluction: Slow soil movement in cold regions.
- Slump: Rotational movement of earth down a slope.
Rivers and Fluvial Processes
- Channel: The main path of a river’s flow.
- Floodplain: Flat land adjacent to a river that floods during heavy rains.
- Terrace: Step-like landforms indicating previous river levels.
- Flood Discharge: Increased water flow during floods.
- Normal Discharge: Average flow in a river.
River Types
- Meandering: Rivers with curves and bends.
- Braided: Rivers with multiple interconnected channels.
- Oxbow Lake: A lake formed from an abandoned meander.
Water Transport in Rivers
- Bedload: Heavy particles transported along the riverbed.
- Suspended Load: Light particles carried within the water column.
- Dissolved Load: Minerals dissolved in river water.
Drainage Patterns
- Dendritic: Tree-like branching pattern.
- Trellis: Parallel streams with right-angle tributaries.
- Radial: Streams radiating outward from a central point.
- Watershed: Area draining into a single river system.
- Drainage Divide: A ridge separating watersheds.
Hydrologic Cycle
- Precipitation: Water comes from the atmosphere as various forms (rain, snow).
- Evaporation: Liquid water converted to vapor.
- Infiltration: Water filtering into the ground.
- Runoff: Water flowing overland to water bodies.
- Transpiration: Water expelled from plants into the atmosphere.
Key Water Storage Types
- Soil Moisture: Water held in soil.
- Groundwater: Water below Earth’s surface.
- Surface Water: Found in lakes and rivers.
Glaciers Basics
- Types of Glaciers:
- Alpine: Found in mountainous areas.
- Continental: Large ice sheets such as Antarctica.
- Glacial Ice Formation: Snow compresses into firn, then ice.
- Movement: Driven by gravity through basal slip and internal flow.
Erosional Effects
- Plucking and Abrasion: Processes where glaciers erode landscapes.
- Striations: Marks on bedrock caused by glaciers.
- U-shaped Valleys: Formed by glacial carving compared to V-shaped valleys carved by rivers.
Depositional Features
- Moraines: Accumulation of debris pushed by glaciers.
- Drumlins: Hills formed by glacier movement.
- Kettles: Depressions formed by melting ice blocks.
Coastal Geomorphology
- Coast vs. Ocean: Coasts are land areas adjacent to oceans.
- Tides: Caused by gravitational pull, including spring and neap tides.
- Erosional vs. Depositional Coasts:
- Erosional: Features like cliffs and sea stacks.
- Depositional: Beaches, bars, and coastal wetlands.
Beach Dynamics
- Longshore Drift: Movement of sand along the shore.
- Swash and Backwash: Movement of water up and down the beach after waves break.
Summary of Key Concepts
- Understanding contour lines and their implications for elevation and landscape features is crucial for interpreting topographic maps.
- A solid grasp of fluvial processes informs how rivers shape landscapes and affects watershed management.
- Awareness of hydrologic cycles plays a critical role in water resource management and environmental science.
- Glacier dynamics provide insights into historical climate change and contemporary sea-level issues.
- Coastal processes are key to understanding landform development and coastal management practices.