"Annual flood" means a discharge (Q) or
flood flow event that occurs at a high frequency, i.e., there is a greater than
a 50% chance of a flood stage (
(5) "Aquatic life"
means all organisms that, as a part of their natural life cycle, live in or on
waters. Aquatic life is synonymous with "Aquatic Biota" as defined in the
Vermont Water Quality Standards.
(6) "Bank full width" means the top surface
width of the stream channel at a discharge corresponding to a water stage that
occurs at a frequency of every one to two years (Q1.5 to Q2, i.e., there is a
50 to 66% chance of this high flow occurring in a given year). Bank full widths
are measured from the crest of the right streambank to the crest of the left
streambank for streams in equilibrium condition, from field scour and
deposition indicators of bank full stage for incised channels, or, when field
measurements are not available, as calculated from reference data such as the
Vermont Hydraulic Geometry Curves [n1].
[n1 http://www.anr.state.vt.us/dec/waterq/rivers/docs/rv_hydraulicgeocurves.pdf]
(7) "Berm" means a linear fill of earthen
material on or adjacent to the bank of a watercourse that constrains waters
from entering a "flood hazard area" or "river corridor," as those terms are
defined in
10 V.S.A. §§
752(3) and (11). For the
purposes of this Rule, the Secretary shall classify linear fill as a regulated
berm when earthen material is pushed or excavated from a stream bed or adjacent
lands into a raised barrier between a watercourse and adjacent lands.
(8) "Buffer zone" means an undisturbed area
consisting of trees, shrubs, ground cover plants, duff layer, and generally
uneven ground surface that extends a specified distance horizontally across the
surface of the land from the top of the bank of an adjacent river or stream, as
determined by the Agency.
(9)
"Channelized" means the condition of a stream channel that has been
straightened, bermed, dredged, and/or armored by human activity.
(10) "Channel incision" means an area of
stream bed exhibiting vertical erosion or headcutting.
(11) "Channel roughness" means the frictional
resistance, and its moderating effect on flow velocities, provided by: the
sizes of instream material on stream beds and banks (i.e., channel boundaries);
the undulations of stream bed forms; and the sinuous features along the channel
planform.
(12) "Dam" means any
artificial structure on a stream or at the outlet of a pond or lake, which is
utilized for holding back water by ponding or storage and may include any
penstock, flume, piping, or other facility for transmitting water downstream to
a point of discharge, or for diverting water from the natural watercourse to
another point for utilization or storage.
(13) "Degrading channel bed" means the
erosion of instream bed materials and a lowering of the channel bed elevation
that occurs at the reach scale with an increase in stream power, brought about
by a change in channel dimensions, slope, and/or roughness
characteristics.
(14) "Dredge"
means lowering the elevation of the stream bed profile or any clearing,
deepening, widening, or excavating, either temporarily or
permanently.
(15) "Emergency
protective measure" means an action necessary to preserve life or to prevent
severe imminent damage to public or private property, or both.
(16) "Equilibrium condition" means the width,
depth, meander pattern, and longitudinal slope of a stream channel that occurs
when water flow, sediment, and woody debris are transported by the stream in
such a manner that it generally maintains dimensions, pattern, and slope
without unnaturally aggrading or degrading the channel bed elevation.
(17) "Fill" means any placed material that
raises, either temporarily or permanently, the surface elevation of the stream
bed, floodplain, or river corridor, or extends the limits of the
streambank.
(18) "Flood hazard"
means those hazards to public safety or property from inundation
damages.
(19) "Flood hazard area"
means the land in the floodplain within a community subject to a one percent or
greater chance of flooding in any given year.
(20) "Flood flowage" means any waters,
sediment, and debris associated with a high discharge or flood flow event (Q1.5
or greater).
(21) "Floodplain
connectivity" means that geomorphic condition in which flows, at or greater
than the annual flood stage (Q1.5), will spill out of the stream channel and
onto the floodplain.
(22) "Fluvial
erosion hazards" means those hazards to public safety or property related to
the erosion or scouring of stream beds and banks during high flow conditions of
a river.
(23) "Geomorphic
condition" means the degree of departure, if any, from the dimensions, pattern,
and profile associated with the naturally stable channel that result from the
unique set of natural stream processes or dynamic equilibrium conditions of a
stream or river segment.
(24)
"Geomorphic sensitivity" means the potential of a river, given its inherent
characteristics and present geomorphic conditions, to be subject to a high rate
of fluvial erosion and other river channel adjustments, including erosion,
deposit of sediment, and flooding.
(25) "Headcutting" means the erosive process
of stream bed particles being washed off a steepened area of a stream bed,
deepening the channel and resulting in a loss in vertical and floodplain
connectivity.
(26) "Horizontal
streambank alignment" means the location of the channel margins, or boundaries
along right and left streambank lines from upstream to downstream, which may be
altered by streambank fill and excavation activities.
(27) "Hydrologic regime" means the timing,
volume, and duration of flow events throughout a defined period of time, which
may be influenced by the climate, soils, geology, groundwater, watershed land
cover, connectivity of the stream, riparian, and floodplain network, and valley
and stream morphology.
(28)
"Instream materials" means all gradations of sediment from silt to boulders;
ledge rock; or large woody debris, as these materials exist in the bed of a
watercourse, within the banks of a watercourse, or enter as placed-fill in the
bed or on the banks of a watercourse.
(29) "Imminent threat" means there is a risk
to life or a risk of severe property damage within the next 72 hours.
(30) "Improved property" means a habitable
structure, the property immediately surrounding a habitable structure, public
utility or transportation infrastructure, and private bridges or culverts and
associated infrastructure providing primary access to a habitable structure.
For the purposes of this Rule, a habitable structure means any enclosed roofed
structure; residential, commercial, or industrial; public or private, that is
fit for people to enter and utilize.
(31) "Intermittent stream" means a seasonal
stream that only flows for part of the year.
(32) "Large woody debris" means any piece of
wood within a watercourse with a diameter of ten or more inches and a length of
ten or more feet that is detached from the soil where it grew.
(33) "Longitudinal stream bed profile" means
the slope or vertical drop of the stream bed from upstream to downstream in
relationship to adjacent floodplain features.
(34) "Next flood threat" means those risks to
life or of severe damage to improved property posed by the next annual
flood.
(35) "Outstanding resource
water" means any waters designated by the Secretary as having exceptional
natural, recreational, cultural, or scenic values, pursuant to
10 V.S.A. §
1424a.
(36) "Perennial stream" means a watercourse
or portion, segment, or reach of a watercourse, generally exceeding 0.5 square
miles in watershed size, in which surface flows are not frequently or
consistently interrupted during normal seasonal low flow periods. Perennial
streams that begin flowing subsurface during low flow periods, due to natural
geologic conditions, remain defined as perennial. All other streams, or stream
segments of significant length, shall be termed intermittent. A perennial
stream shall not include the standing waters in wetlands, lakes, and
ponds.
(37) "Q" means discharge, or
the volume rate of water flow.
(38)
"River corridor" means the land area adjacent to a stream or river that is
required to accommodate the dimensions, slope, planform, and buffer of the
naturally stable channel and that is necessary for the natural maintenance or
natural restoration of dynamic equilibrium conditions, as that term is defined
in
10 V.S.A. §
1422, and for minimization of fluvial erosion
hazards, as delineated by the Agency in accordance with the DEC Flood Hazard
Area and River Corridor Protection Procedures [n2].
[n2 Available at:
http://dec.vermont.gov/sites/dec/files/documents/dec-fharcp-2014-12-5.pdf]
(39) "Secretary" means the Secretary of the
Agency of Natural Resources or the Secretary's authorized
representative.
(40) "Sediment
regime" means the size, quantity, sorting, and distribution of sediments, which
may differ between stream types due to their proximity to different sediment
sources, their hydrologic regime, their stream, riparian and floodplain
connectivity, and valley and stream morphology.
(41) "Significant flooding event" means a
flood greater than the annual flood where flood flowages may result in
significant erosion and depositional processes, i.e., a flooding event that may
be in the order of a five-year recurrence interval (Q5 or a 20% chance of
occurring in any given year).
(42)
"Stream" means the full length and width, including the bed and banks, of any
watercourse, including rivers, streams, creeks, brooks, and branches, which
experience perennial flow.
"Stream" does not include ditches or other constructed
channels primarily associated with land drainage or water conveyance through or
around private or public infrastructure.
(43) "Stream bed erosion" means a stream
process whereby stream power is sufficient to move even the largest stream bed
sediments and transport the quantity of sediment flowing from upstream, leading
to a deficit of sediment and a lowering of the vertical stream bed
profile.
(44) "Stream bed
deposition" means a stream process whereby stream power is insufficient to move
or transport the size and quantity of sediment flowing from upstream, leading
to a buildup of sediment and a raising of the vertical stream bed
profile.
(45) "Stream forms" means
the width, depth, meander pattern, and longitudinal slope of a stream channel
that vary little within a narrow range of values at the stream reach-scale,
when larger-scale stream processes remain unchanged.
(46) "Stream processes" means the hydrologic,
sediment, and large woody debris regimes of a particular stream reach and is a
term used to describe stream channel hydraulics, or the erosion and deposition
of instream materials by the power of flowing water, which may result in the
vertical and lateral movement of stream bed and banks, and may change or be
changed by stream forms and channel roughness.
(47) "Vertical stream channel movement" means
changes to the vertical stream bed profile caused by reach-scale changes in
stream processes.
(48)
"Watercourse" means any perennial stream. "Watercourse" shall not include
ditches or other constructed channels primarily associated with land drainage
or water conveyance through or around private or public
infrastructure.
(49) "Width to
depth ratio" means the channel width divided by the mean channel
depth.
(50) "Windrowing" means
pushing and berming instream materials to the stream channel margins.