Stream and Flood Hazards Flashcards
What are the two basic role of streams and rivers (larger
streams) within the Earth system.
drain
water off the landscape and to transport
sediment.
A stream may overflow its banks when the its
ability to carry water is overwhelmed by the
sheer volume of water flowing off the
landscape and create what is known as a
_______.
flood
It is described as the volume of water moving
through a channel over a given time interval,
commonly measured in units such as cubic
feet per second (ft3/s).
Stream discharge
It is a process where water flows through
stream channels.
Runoff
It is a process of water movement when precipitation reaching the land
surface moves downslope in thin sheets.
Overland Flow
These are two processes of water movement which allows water to return back
to the atmosphere.
Evaporation and plant transpiration (water
uptake by root systems and then released
through plant leaves)
It is described as the discharge of
groundwater into the surface environment; fairly
continuous unlike the sporadic input of water to a
stream and groundwater may travel anywhere
from a few days to thousands of years before
discharging into a stream channel.
Groundwater baseflow
_____________________ provide information about a
river or stream by simply plotting the discharge versus
time.
Stream hydrographs
It is the amount of time for water to move across
the landscape and into channels; will vary
depending on the distance between where the rain
is falling and the particular channel where discharge
is being measured.
Lag time
Continuous input of groundwater baseflow allows
streams in many areas to keep flowing at some
minimum level, often called _________________. This
contribution of groundwater baseflow keeps streams
from going dry between rain events, thus is critical in
maintaining the health of stream ecosystems.
baseflow conditions
High precipitation allows more water to infiltrate to
the water table which causes the water table in
humid regions to be higher than the streams channel,
thereby forcing groundwater to flow into streams.
Such streams are often referred as ________________
gaining stream.
______________ are a result of less deep infiltration in
arid areas resulting in a water table that is below the
level of most stream channels. Under these
conditions, the water in the stream will flow into the
groundwater system.
Losing streams
A ____________ is a network of stream channels where merging tributaries (smaller of any two merging channels) form progressively larger streams.
drainage system
This term is often applied to the larger stream that serves as the principal channel within a drainage system
River
The upper portion of the drainage system is called the ___________, whereas the ____________ is found in the lower part of the system where a river empties into an ocean, lake, or another river.
headwaters, mouth
True or False: Headwater streams are generally small and relatively fast
moving and occupy narrow valleys, but then evolve toward the mouth into gently flowing rivers that occupy
wider valleys.
True
Individual systems are separated from one another by a topographic high or crest in the landscape called a
_____________
drainage divide
Drainage divides are useful for mapping what hydrologists call a _____________ or watershed, which
represents the land area that collects water for an individual stream or river.
drainage basin
It is the largest river due to its average discharge at mouth of 7,750,000 ft³/sec.
Amazon
Among the top 10 largest rivers, this river has the highest annual sediment load (1,670,000,000 tons).
Ganges
Give some information about the Mindanao River Basin. (where it traverses, and what is the land area)
• 5 Provinces (Bukidnon, Maguindanao, North Cotabato, South Cotabato, Sultan Kudarat)
• 3 Regions: (X, XII, ARMM)
• 2 Cities: (Cotabato, and Koronadal)
• Land area: 21,503 km² (2nd largest river basin in the Philippines)
These are any smaller streams that feed larger streams within a
drainage basin.
Tributaries
A method of classifying or
ordering the hierarchy of
natural channels.
Strahler Stream Order (the other one is Shreve)
__________________ reflects downstream trade off between discharge
and slope in setting transport capacity (and thus ability to move
sediment and incise rock).
Longitudinal profile
The level below which a river or stream cannot incise.
Base level
The __________________________ for most streams is global sea level.
ultimate (or absolute) base level
True or False: Steep terrain tends to be poorly
dissected and thus have a low
drainage density.
False (highly, high)
Formula for Drainage Density
Drainage density = total stream channel length / area of the drainage basin
True or False:Gentle terrain tends to be less
well dissected, with substantial
hillslope convexities and low
drainage density
True
Enumerate all the DRAINAGE PATTERNS
Dendritic
Parallel
Trellis
Rectangular
Radial
Annular
Multibasinal
Contorted
A drainage patter most commonly formed on horizontally bedded and uniform sediments or on uniformly resistant crystalline rocks.
Dendritic
A drainage pattern that usually develops on moderate to steep slopes, but also where regional structure, such as outcropping resistant rock bands, are elongated and parallel. All forms of transition can occur this type and dendritic and trellis pattern.
Parallel
Drainage patterns that are most common on dipping or folded
sedimentary or weakly metamorphosed sedimentary rocks; also areas of joints and
faults which intersect with right angles and old sand dunes with parallel alignment
Trellis
A drainage pattern which usually have a more or less perpendicular turns mainly caused by criss-crossing
fractures.
Rectangular
A drainage pattern that occurs around domes or cones, and particularly common on volcanic areas.
Radial
Drainage patterns that develop around domes, where there exists alternating resistant and weak
beds, so that the major channels cut through the strike and the low order streams follow the dip of the rocks.
Annular
A drainage pattern that can occur in a variety of conditions where local
hummocks and depressions inhibit a continuous channel network. Irregular glacial deposits or erosional hollows due to solution of underlying
lithology, irregular thawing permafrost. Coastal dunes, delta plains, and wind eroded hollows.
Multibasinal
A drainage pattern that incised into rocks with complicated structural
patterns. Associated with crystalline metamorphic rocks with a history of intense folding, jointing, intrusions, alterations, and faulting.
Contorted
Types of stream according to whether they are water-holding or not.
• Perennial
• Intermittent
• Ephemeral
Types of river (large stream) according to its linear form.
• Straight
• Meandering
• Braided
It is the section of the river that is defined as either a gently or steeply sloping channel form. They can be
either smooth or irregular in shape
Cross-profile or “transverse”
It is the section of the river that is defined as either a graded or interrupted profile, with waterfalls and
lakes.
Length-profile or “longitudinal”