Category: places

Seattle: Green Lake

Jason Kingcity, creeks, history, infrastructure, lakes, landscape, maps, parks, places, seattle, streams, washington2 Comments on Seattle: Green Lake

GREEN LAKE

I’ve been wanting to write about Seattle’s Green Lake, which is an addition to round out the post these small Seattle lake stories, and supplement the coverage of the larger lakes Union and Washington.  Green Lake has a special place for me, having lived close to it our entire time in Seattle, it’s been a place for fun, recreation, and even protest.  This really cool cross-time image from Then & Again shows the juxtaposition of the current with the old, and Green Lake spanning this , here with “…the majestic USS Macon gliding above Seattle’s Green Lake on August 22, 1934. The airship was traveling to its new station near San Francisco but took a leisurely route with time for a number of photo ops along the way.”

The history of the lake goes back to similar era to the smaller Bitter and Haller Lakes and the larger Lake Union and Washington, as mentioned on the Seattle Parks website: “Geologists say the Vashon Glacial Ice Sheet, which also formed Puget Sound and other area lakes, formed Green Lake 50,000 years ago. Dredgings of Green Lake have produced volcanic ash from an eruption of Glacier Peak that occurred about 6,700 years ago.”  The original lake was lowered 7-8 feet as park of early 20th Century Park improvements, and this 2014 article from Seattle Greenlaker  ‘Olmsted and the Origin of Green Lake Park‘ offers a good introduction to the modern incarnation of the park and this process. In that post, it links to this great map from 1907 from the National Association of Olmsted Parks, which shows the development of Green Lake Boulevard and the areas near the lake as part of this process, and the first evolution of Green Lake as part of the overall Park System.

Via Seattle Greenlaker – Caption: Courtesy Frederick Law Olmsted National Historic Site, National Park Service, 02714-21. Used with permission.

If you were, like me, temporarily disoriented for a bit, it helps to rotate this drawing so north is up, and the more familiar shapes and lobes of the lake become clearer. I’ve also highlighted the old shoreline (dashed line) and the new shoreline (solid line w/ blue fill), so it’s clearer where the drawdown left space for the trails and more usable open spaces, with amenities like Boat Houses and beaches.  The map also has information on the inlets and outlets, which I’ve highlighted below in a bit more detail for reference.

If you remember back a bit to my post of the exploration of Licton Springs, the sketch above is instructive, as this inlet #1 shows an inlet with a specific reference: the “Brook inlet box culvert 2’x6′ from Licton Min. Sprg.”, showing the subsurface connection to the spring that had been filled in previously but was still flowing from the north.  A Bathhouse is shown, which does not currently exist, but there is a swimming beach access which is still in place today, along with the splash play and some open spaces.

There is another pair of inlets #2 a bit further west, near Corliss Avenue, with a label “Inlet box 1 1/2′ x 2′” and near there is one with a note “Old Inlet 18″x18” wood box” which has a note “very little flow now – some sewerage seems to enter it now.”

The final inlet #3, is to the west, showing a connection to an “Inlet-brook, 6′ wide, 3″ deep” that comes from the northwest, running under the streetcar track in a culvert before coming into the lake.

On the opposite side of the Lake, heading southeast, there is the Outlet, which is marked #4, near 4th Avenue (a few blocks from the proposed boulevard which would become current day Ravenna Boulevard), which was the natural drainage of Green Lake into Ravenna Creek.  The reconfiguration of this zone and the shift of the shoreline created a larger area that now has sports fields, as well as a boat house and what is a popular beach access spot today.  This is also adjacent to the larger commercial zone which is the hub of activity adjacent to the lake.

 

These flows in and out correlates somewhat with the 1850s maps, but does closely align with the the USGS Topo Map from 1894 (see below) of Green Lake that identify three inlets from the north and the Ravenna outlet heading southeast – which does line up with the hydrology shown on these 1907 drawings.

Historical Topographic Map Collection

The formal plan as presented to the Seattle Parks Commission in 1910 mirrors much of the modern day condition, with the lowered water levels providing for perimeter trails, new plantings, a new island, some amenities such as beaches and boathouses, and the boulevard that rings the park (the western half of which was transformed with the routing of Aurora Boulevard (Highway 99).

 

And another version, this one from 1925 showing a more colorful version of this, “Proposed Plan for the Development of Green Lake” via the Seattle Municipal Archives Digital Collections.  This map dashes in the existing and proposed shorelines

I posted previously about the fun bathymetry maps, which included Green Lake. Another map I like is this one ‘Showing Depth Contours of Green Lake’ via the Seattle Municipal Archives Flickr page, which was done in 1938 as part of the Sanitary Survey by the WPA and featured in the “Report on Green Lake Algae Control”, which highlights perennial water quality issue . It reinforced that the lake is relatively shallow, with maximum depths no greater than 25′ feet on the western edge.  It also identifies some of the hydrology, including overflows, intake from the City resevoir, and to the west, a “permanent inlet from deep springs” which is a fascinating addition both due to it’s mystery and also it’s location, which is not shown on later maps but does appear in the 1950s map.

The history of the lake beyond that Olmsted plan has many facets and this Chronology is helpful to see the evolution.  There many tales (and History Link is a great resource here) that connect with Seattle history, such as in 1869, when David Denny “…kills what is likely the last elk in Seattle, near Green Lake. The elk weighs 630 pounds.”, or 1893 when a cold spell froze the lake completely over. including  of Hydroplane boat races in the 1930s, as well as a cleanup and redesign in 1936.  Lots of history and evolution I won’t get into here, as it’d take days, but my favorite lost part of the Green Lake history, which I only discovered by accident after visiting the park many times, is the Aqua Theater, built in 1950 on the south edge of the lake as a 5,500 seat performance venue, built in a little more than two months coinciding with the first of what is now an annual Sea Fair.

The venue hosted a range of events included the annual Aqua Follies, which included ” Water ballets, diving exhibitions and clown acts took place in the pool and on the stage behind. Many of the Aqua Follies mermaids were recruited in Minneapolis before June 1, and began practicing before Seattle area college students finished their school term.”  There were some notable music shows including 1969, which featured Led Zepplin and The Grateful Dead, which was one of the final shows at the venue before it was shut down.

The lake as a locus for recreation has stayed consistent over the years, with lots of walkers and joggers circling the 3 mile loop, along with water access via boat rentals, rowing, and use of adjacent open spaces sports fields, and even a Par 3 golf course.  Water quality issues are a perpeutual issue, but it doesn’t stop it from being the busiest park in the state of Washington, with over a million visitors a year.

Postcard circa 1950s – via Seattle Greenlaker – https://www.seattlegreenlaker.com/2017/06/green-lake-seattle/

HEADER: 1987 Aerial view of Green Lake – via Seattle Public Archives

Los Angeles River in Places Journal

Jason Kingcity, cultural, history, infrastructure, los angeles, maps, places, rivers, streams1 Comment on Los Angeles River in Places Journal

There is no shortage of articles written on the Los Angeles River, and I’ve covered some of the broader hidden hydrology work being done there in a previous post here, Beyond the LA River. I do however have a special affinity for the quality of scholarship on Places Journal, and an essay from May 2018, Willful Waters by USC’s Vittoria Di Palma and Alexander Robinson doesn’t disappoint.  This longform essay provides a great background and historical framework for anyone wanting to understand the river and it’s long and contentious history, as well as recent efforts of revitalization and reconnection.   It also comes with a great collection of historical imagery, which elevates our thinking out the past, present, and future river beyond the concrete ditch we tend to associate with the Los Angeles River.

I’d recommend the essay in its entirety, so I’ll just include a few snippets and comments I thought were compelling.  At first I was a bit confused about their allusion to the Thomas Cole series The Course of Empire in this context, but after some explanation, it’s an interesting framework in which to think about hidden hydrology, in terms of binaries such as life/death or sin/redemption, and as a “cyclical” journey from wildness through some sort of apex and back through destruction and desolation.  That narrative begins another cycle of  “revitalization” and “restoration”.  As the authors mention: ” If not for the galvanizing effect of a set of historical ideas — the belief that a site, destroyed and degraded by human industry, could be transformed into something evocative of its original condition through the power of “nature” guided by enlightened design — Los Angeles might have continued to forget that it ever was a river city.”

Los Angeles River in the early 20th century. [Security Pacific National Bank Collection, Los Angeles Public Library] – via Places
From a historical viewpoint, the idea of a soft, meandering river is hard to comprehend, but also is the origin of the city itself, supporting described as “…a stream trickling through a wide sandy bed.”  with “The river basin was overspread with springs, marshes, and shallow ponds (the very name of La Cienega Boulevard recalls the landscape’s original swampy character), and the debris from the mountains, deposited over centuries, created a layer of alluvial silt that in some areas lies 20,000 feet thick.”  This lack of structure meant lots of variability, which created unpredictable volatility during storms and “rain events” in which “…waters would rush down from the mountains, carrying gravel, silt, boulders, and trees.”  This factor would ultimately lead to the demise of the river itself.

Edward O.C. Ord and William Rich Hutton, Plan de la Ciudad de Los Angeles, 1849. [Los Angeles Public Library] – via Places
The other interesting idea was the concept of zanjas (irrigation ditches), in which there were miles built as shown in the above map:  Quoting John Shertzer Hitell, “The “zanjas, or irrigating ditches, run through the town in every direction.” They “vary in size, but most of them have a body of water three feet wide, and a foot deep, running at a speed of five miles an hour. They carry the water from the river to the gardens, and are absolutely necessary to secure the growth of the fences, vines, and many of the fruit trees.”   The image below showing how these canals were parts of the fabric of the city, enclosed but still open and visible, and enlivened the place, as mentioned in a reference to visitor Emma Adams, who commented on “…the soft murmuring of water as it glides through the zangas [sic] in some of the beautiful suburbs of the city is sweet music to the ear, a happy voice sending out joy and gladness. Wherever it is heard are sure to be seen verdure, flowers, and fruit.” In this way, the wild and unpredictable Los Angeles River was remade into a tractable urban water source.”

A canal, or zanja, on Figueroa Street, Los Angeles, ca. 1892. [Security Pacific National Bank, Los Angeles Public Library] – via Places
The manipulation of the river for utilitarian purposes followed many others before it, but foreshadowed larger interventions of control.  As the authors point out, “Los Angeles was shaped by a dual need to be at a safe distance from its unpredictable, flood-prone river, and in close contact with the river’s highly controlled, artificial reincarnation: the zanja madre and its network of ditches. This relationship between city, river, and ditch is illustrated by the map drawn up by Ord and the surveyor William Rich Hutton in 1849.  Agricultural lands occupy the area between the river and the city up on the Elysian Hills, with the southerly extension of both fields and city closely conforming to the route of the zanja madre. At the same time, the problematic nature of the flood-prone river is indicated by this inscription: “sand over which the River spreads its waters which are wasted.”  They go on to conclude that,“The zanja madre was, in other words, the Los Angeles River tamed and perfected by the improving force of human culture.”

Los Angeles River and the Fourth Street Bridge, 1931. [Herald-Examiner Collection, Los Angeles Public Library] – via Places
The river at the time was still natural in most places, but the canals soon depleted water levels, and created a trickle, which was the impetus for Mulhollad’s hyperbolic yet apt “Titanic Project to Give [the] City a River”.  After this change to more consistent supply, which included piped water from the Owens Valley some 233 miles away via aqueduct, the Los Angeles River only emerged during rain events, those “… “intermittent moments when it flowed with a violence that only intensified as galloping urbanization further hardened the city’s watershed. No longer valued as a natural resource, the ever-wilder river was now feared as a “predator,” able to roam and strike wherever it wished.”  This unpredictability and ensuing series of floods changed how people thought, thinking of the river as a “menace” and thus “perceptions of the river were changed irrevocably.”

Los Angeles River at Griffith Park, ca. 1898–1910. [California Historical Society Collection, USC] – via Places
The flooding was the final impetus to use new technology to “train” the “unruly dog” of a river, which seemed to be the particular bailiwick of the Army Corps of Engineers, and creating what amounted to a “water freeway” that we know today. In a few short years, the Corps“ …systematically transformed the Los Angeles River from an intermittent, meandering stream bordered by willows and cottonwoods into the concrete storm drain we see today.”  The authors point of the lesson of this today.

“In a textbook example of the triumph of reason and human agency over willful nature, the Corps created the ultimate Los Angeles fantasy of a river: a “water freeway.” That a drought-prone region would celebrate the speed at which water could be drained off to the ocean was an irony not then appreciated by either the military engineers or the public.”

Los Angeles River, San Fernando Valley, 1949. [Valley Times Collection, Los Angeles Public Library] – via Places
Perceptions changed in the 1970s, and the media, politicians, artists, and environmentalists rediscovered the river in a variety of ways.  A series of articles in the Los Angelse Times by Dick Roraback in 1985 entitled , ” “Up a Lazy River, Seeking the Source: Your Explorer Follows in the Footsteps of Gaspar de Portola.” provided a poignant story about the forgotten waterway, where “… the  author narrated his expedition from the river’s mouth to its putative source, chronicling the riparian habitats of its flora and fauna. Roraback’s picaresque tale turned the Los Angeles River into an incongruous backdrop for a cast of quirky urban characters (the blonde waitress, the salty sea dog, the mussel gatherer, the dog-walking divorcée) engaged in various activities, both licit and illicit, in the river and along its banks. By presenting the river as a neglected urban feature, the series brought its paradoxical charms to the attention of a large new audience, and, crucially, positioned the river as a postindustrial terra incognita — an attractive, slightly dangerous, and alluring urban landscape.”  

Further work by artists and others who started exploring the waterway, and ultimately went on to found the Friends of the Los Angeles River, started to think about the area in different ways, and through exploration,  began as a “…characterization of the river as a paradise lost, a place of discarded things and marginalized people, served to ignite a potent landscape imaginary. It also introduced the idea of the river as a space for environmental action. ”  This was aided by the Donald C. Tillman Water Reclamation Plant which added 20 million gallons of water per day, which had an effect of revitalizing the ecology of the river.  “This infusion of wastewater generated a verdant riverscape, which in turn, and somewhat improbably, inspired comparisons with the earlier paradise described by Father Crespí and sparked talk of a riparian rebirth. As the changing river increasingly evoked that lost, idealized waterway (particularly in the unpaved eleven-mile stretch known as the Glendale Narrows), it also inspired residents to take up walking, bike riding, bird watching, horseback riding, and even kayaking and canoeing…”

Los Angeles River, Glendale, with a bicycle path along the banks. [Creative Commons] – via Places
The kayaking wasn’t always for pleasure, as it was interesting to learn that a waterway has to be navigable to be eligible for the Clean Water Act, so a group of people in 2008 kayaked the length of the river to provide its navigability.  This meant that maybe “The fantasy of transforming the flood control channel into an arcadian waterway began to seem real. Kayaking has also become a powerful means of introducing visiting dignitaries to a vision of a newly green and civic river.”  The final part focuses on the long and winding road of Revitalization, including master plans in through the 1990s and more recently efforts by interdisciplinary design teams, government agencies, and non-profits.  These focused on ecology, hydrology, and recreation, amongst other factors, either as technical studies but more often than not art intervetions or designs.  One such example is the Piggyback Yard Feasibility Study (image below), done by Mia Lehrer + Associates, which “…integrates economic and hydraulic modeling with community design considerations, but such efforts such are still few in number and small in scale.”

Piggyback Yard Feasibility Study, Mia Lehrer + Associates. [Mia Lehrer + Associates] – via Places
The mix of design, art, tours, and other creative methods of interpretation, often using minimal intervention, hint at “…the remarkable activity generated by the Los Angeles River — which as yet remains largely a concrete channel bisected by a thin course of water — testifies to the profound power of the city’s desire for ecological redemption and urban rebirth, and to ways in which civic or even poetic acts have found purchase within a byzantine network of managerial interests.”

Endnote:

The post in Places referenced above is an excerpt from what sounds like a great book, River Cities, City Rivers published by Harvard University Press and edited by Thaisa Way.  Will track down and report on at some point on this book, but here’s a summary from the site:  “Cities have been built alongside rivers throughout history. These rivers can shape a city’s success or cause its destruction. At the same time, city-building reshapes rivers and their landscapes. Cities have harnessed, modified, and engineered rivers, altering ecologies and creating new landscapes in the process of urbanization. Rivers are also shaped by the development of cities as urban landscapes, just as the cities are shaped by their relationship to the river.  ¶  In the river city, the city river is a dynamic contributor to the urban landscape with its flow of urban economies, geographies, and cultures. Yet we have rarely given these urban landscapes their due. Building on emerging interest in the resilience of cities, this book and the original symposium consider river cities and city rivers to explore how histories have shaped the present and how they might inform our visions of the future.”

 

HEADER:  Los Angeles River, view from 6th Street Bridge, 2010. [Ian Rutherford] –  image via Places

 

 

 

 

Anne Whiston Spirn’s Legacy in Philadelphia

Jason Kingcase study, city, climate, creeks, cultural, design, ecology, history, infrastructure, landscape, maps, philadelphia, places, precedents, streams, watershedsLeave a Comment on Anne Whiston Spirn’s Legacy in Philadelphia

The most recent October issue of Landscape Architecture Magazine (LAM) has a great story on hidden hydrology inspiration Anne Whiston Spirn, FASLA, titled Where the Water Was, which highlights the “long arc” her work in West Philadelphia, namely the “water that flows beneath it.”

The aha moment is recounted in the article, the inspiration for the poem linked above “The Yellowwood and the Forgotten Creek“, as recounted in the article, she “was on her way to the supermarket, when she was stopped at a gaping hole where the street had caved in over the Mill Creek sewer.  “I looked down and saw this big, brown rushing river, and all this masonry that had fallen in. I thought, ‘My God, there are rivers underground. We’re walking on a river.'” (122)  Sprin’s work spans decades since that story in 1971, predominately around Mill Creek which was “buried in the brick sewer pipe in the 1880s”, morphing into the West Philadelphia Landscape Project (WPLP) [covered in brief on our post on Philadelphia here].  While I was inspired as a student and professional by her work on books like The Landscape of Landscape and The Granite Garden, her work on hidden streams was perhaps the most powerful for me, both as an object of study but more broadly to leverage this research into a vehicle for positive change.  As mentioned, the WPLP website “contains maps, historical documents, reports and studies.” including an updated interactive timeline, and some newer updated interactive mapping which is good to see, as much of the interface until late was a bit dated.

A long way from the preliminary maps in CAD as part of the early mapping in the late 1980s and early 1990s.  The sophistication and breadth of this work at the time is telling thought, and I remember seeing these for the first time in college and being amazed.  The article shows what many of us know, which is how much of what we take for granted in technology of mapping that’s available to us today, and how hard it was, physically and sometimes politically to get good information.  As Spirn mentions “You had to literally go out and field check.” (134)

The takeaways of this early work was to both connect the above ground with what was underground, both historically in predevelopment hydrology but also with sewer routing and burial of waterways.  As mentioned, the idea that is a constant with Spirn of “reading the landscape” was instilled as a way to understand the full picture of a site or district.  The connection of the physical features with the social is also evident as Spirn is quoted: “It’s a pattern of eastern old cities and across the U.S., where lower-income folks are living in the bottomlands… Many are literally called the Black Bottom.” (126)  From this analysis, the idea of mapping and using vacant lands was a way to solve the hydrological problems of flooding or sinkholes, but also to revitalize communities.

The Buried River from Anne Whiston Spirn on Vimeo.

How to do it was an issue, as recounted in the article, ideas where one thing, but changing minds into action was another.  McHarg’s Design With Nature inspired her writing The Granite Garden, not as an academic treatise, but rather “…to fill a void.  Scientific journals, historical documents, topographic maps, all sorts of materials contained a wealth of information for ecological designers, but no one had pulled it together in a comprehensive, understandable book that could guide designers as well as the public.”   (127)  This book influences generations of landscape architects in many ways beyond merely historical ecology, but in how we think and communicate.  For the project itself, Adam Levine (who is the mind behind the PhillyH20 project which i documented previously) found the 19th Century maps “that showed Mill Creek and its tributaries before the land was developed. Spirn’s students digitized those surveys and overlaid them on the city’s topographic maps, finally getting an accurate depth of fill along the floodplain. “We found it’s buried up to 40 feet in some areas…”” (134)

The actions were part of this research as well, and many interesting strategies came from the Vacant Lands report (see here), as well as a number of other projects, many of which took a long time to become reality, or came with ups and downs of poor implementation or.  The successes came, owing to the persistence of Spirn and her local compatriots in West Philadelphia, summed up in the article simply:

“Change is a bit like a buried creek. It’s hard to remember its origins. Its many branchings are invisible.” (137)

The legacy locally is a series of activists still working on landscape and community building.  Beyond that, there’s an army of landscape architects inspired by this project and her writings, and her life-long spirit of advocacy.  A great homage to a wonderful teacher and landscape hero.  Lots of great info in the article – which unfortunately isn’t available digitally at this time.

HEADER:  Snapshot of Interactive Map of Mill Creek – via

Geoarchaeology and Lost Rivers

Jason Kingarchaeology, city, creeks, geology, history, landscape, london, maps, places, precedents, research, riversLeave a Comment on Geoarchaeology and Lost Rivers

Our understanding on the arc of history around hidden hydrology is informed with maps and accounts from early explorers and settlers to areas, augmented with records, diaries, and oral histories. Often this neglects and misses the valuable stories of indigenous inhabitants of areas, and leaves us with a significantly shorter timelines for reference. The role of archaeology is vital to unlocking the layers of hidden hydrology that don’t emerge from these illustrative written histories, so I was really intrigued with a recent tweet from the Museum of London Archaology (MOLA) (Twitter: @MOLArchaology) that told of their current work, called London’s lost river: the Tyburn.  From their site, the project is the result of “…a team of expert geoarchaeologists  whose work is helping us to understand London’s lost rivers. As an educational charity, we want to share what we’ve learnt, so please join us to explore the story of this long-lost river.”   

Using the interactive ESRI Story Map, MOLA developed a narrative to describe the process and some of the key findings.  Much of the work is conducted along with construction sites, which gives an opportunity to look below the surface while excavation is happening.  The River Tyburn flowed on the north bank of the Thames, and most famously, was routed and defined the space called Thorney that Westminster Abbey was located, seen in this view circa 1530.

The origins of the river are tied to the longer history of the Thames, which is illustrated (see header image) and reaches back to the last glacial period of 11,500 years ago.  From there in, “…this new epoch, known as the Holocene, the Thames began to take the shape we know today, but many channels still criss-crossed the river’s floodplain within the wide gravelly valley. One of  these channels was the Tyburn, which flowed into the Thames.”   In this zone, there are hundreds of sites, or ‘deposit logs’ that are recorded, and these are modelled to create a snapshot, particularly focusing on the depths of land (depicted below as green – high ground and purple – low ground.  From this model, “projected possible courses for the River Tyburn, following the lowest-lying areas of the modelled 11,500-year-old topography.” with a caveat that “the river would have migrated over time.”

Drilling down (literally) into the specificity of the deposits shows the ranges of material and how it can inform, looking at “ancient flora and fauna” and focusing on things like Diatoms, Pollen, and fossils of things like “Ostracods, the remains of small crustaceans, can indicate salinity, water depth, temperature, water acidity/alkalinity”.

Below is “…a cross section, or transect, running north–south from Westminster to Vauxhall Bridge, along the north bank of the Thames. This connects deposit sequences recorded in trenches and boreholes, and helps us look at these sequences over wide areas.”

They also connect their study with the work of Barton and Myers 2016 book ‘The Lost Rivers of London‘ (see here for a post on the same), which speculated on a number of scenarios for the Tyburn, and various routes.  There’s some graphic things I’d change here (namely it’s hard to read the Barton and Myers layers) but the concept is interesting, to overlay varying studies and ‘proof’ the concepts of routing. In essence, does the data reflect the speculation on routes, either reinforcing or disputing what was speculated?  The below map is a composite of this

There’s links to some coverage in London Archaeologist, such as a 2014 article in which “… Tatton-Brown and Donovan used historic documents and maps to suggest that the medieval waterways separating Thorney Island from Westminster were man-made and that the Vauxhall Bridge route was the original and only course of the river.”  The 3D views of the route and the illustration of the provide a speculative view of the area.  From the site:  “Our topographic model supports Barton and Myers’s suggestion that discussing two distinct branches (towards Westminster and towards Vauxhall Bridge) is an over-simplification of what was probably a more complex delta-like network, as shown [below] (artist Faith Vardy).  This geoarchaeological study provides a baseline for reconstructing the evolving landscape; when combined with historical records and archaeology, even more detailed models could be created. The research done by others, such as Tatton-Brown, which focuses on later periods, may be supported by geoarchaeological work undertaken in the future.”

The concept of geoarchaeology is pretty fascinating as well, and worthy of some further exploration.  In the interim, you can check out the MOLA site for what their team does, which focuses on using “…auger or borehole surveys and interpret the archaeological soils and sediments retrieved, allowing us to reconstruct past landscapes and environments.”  The reason for this particular subset is to pick up “…where the archaeology is too deeply buried for traditional excavation techniques to succeed. It is also a cost-effective archaeological evaluation tool and geoarchaeological deposit modelling, which maps buried landscapes and deposits.”  This is relevant as the surface remnants of these, but the underground deposits, so they work in a “…wide range of depositional environments, including alluvial floodplains, fluvial environments and estuarine/intertidal zones. Using palaeo-environmental proxy indicators, such as pollen and diatoms, we reconstruct past environments. Our specialists also use a range of sedimentological techniques.”

These techniques don’t answer every questions, but coupled with expertise and interdisciplinary research, enables us to see further, and deeper than previousl.  The role of archaeology and geoarchaeology in hidden hydrology is vital, as shown above. While we often rely on maps, photos, sketches, and written histories to reconstruct places,

HEADER:  Artist’s reconstruction of a cold climate, braided river, such as the Late Glacial Thames (artist Faith Vardy) – via

Denver Drainage Unearthed

Jason Kingcity, creeks, daylighting, denver, design, infrastructure, parks, places, rivers, streamsLeave a Comment on Denver Drainage Unearthed

A recent article in the Denver Post “Denver accelerates “daylighting” of lost waterways, “undoing history” with decades-long re-engineering effort” discusses some exciting new work on restoring hidden hydrology and “Re-opening of buried waterways” in the area to manage stormwater runoff and create habitat.  The context:

“Old Denver pulsed with H2O, water that snaked through the creeks and irrigation canals crisscrossing Colorado’s high prairie before 150 years of urban development buried most of them or forced them into pipes.”

A similar story to many cities across the globe, “…developers focused on filling in creeks to make way for the construction of railroads, streets, smelters and housing — all laid out across a grid imposed on the natural landscape.”  This can be remedied today “…by reconstructing the urban landscape where possible, they’ll slow down water, filter it through vegetation to remove contaminants, control storm runoff and nourish greenery to help residents endure the climate shift toward droughts and rising temperatures.”

DENVER, CO – AUGUST 27: Newly planted grasses grow along Montclair Creek on August 27, 2018 in Denver, Colorado. The City of Denver is working on restoring the creek to help with future flooding. (Photo by RJ Sangosti/The Denver Post)

It’s heartening to see this large of a paradigm shift, and engineers, such as Bruce Uhernik, whom quoted saying:

“We’re just trying to take back that space and make waterways more natural and more beautiful. Why would people not want something to be more natural? This is being responsible — not just to what the city and people need, but to the environment’s needs. Birds. Fish. Trees that should be growing along these corridors. All these work in unison. If you break the chain, things fall off course.”

I appreciate some of the language, but the term “undoing history” is a bit strange to me as I always think of projects like this, in any form, as redoing history.  I guess it’s your take on what is history: the original pre-development condition that needs to be restored, or the interventions and filling as the history that needs undoing.  As mentioned, there’s plenty of history as “Historic Denver maps from the late 1800s show multiple irrigation canals and curving dotted lines denoting unnamed waterways, including a creek that flows through the Montclair Basin from Fairmount Cemetery toward north Denver industrial areas where smelting and rendering plants were located along the South Platte.”  

Either way, it’s a cool project, and has some unique components and context, much of which can be found in the Denver Public Works ‘Green Infrastructure Implementation Strategy‘, a document broad interventions for stormwater and habitat.  The prevalence of creeks is seen in the map of Recieving Waters (page 7) shows that while there are a number of urban creeks, they are impacted by residential, commercial, and industrial development throughout the region,

 

A series of maps in the report outlines pollutants of concern like Fecal bacteria and E.coli, Total Suspended Solids (TSS), Nitrogen, Phosphorous.  This map (page 21) shows subbasin level designations of Nitrogen, which is elevated by human activity, and can lead to algae blooms, and issues with aquatic species.

A focus on the urban core includes the Platte to Park Hill (Part of area 20 above (City Park/Park Hill), which integrates a number of systems.  As mentioned in the report:  “Stormwater Systems is taking a
comprehensive green infrastructure approach to better protecting people and property against fooding while improving water quality and enhancing public spaces.  Four projects are part of the Platte to Park Hill… Collectively, the  four coordinated projects will increase neighborhood connectively, add new park and recreation spaces, provide critical food protection, and improve water quality.” (page 54)  The Globeville Landing Outfall project is one of these segments, as part of the strategy, using open channel design, which “…will help clean storm water naturally when possible and will move the water to its ultimate destination, the South Platte River.”  A rendering of the plan:

The 39th Avenue Greenway (also seen in the header) also includes open channels for flood control and storm events.  The opportunity to layer community function with these facilities is key, as they are “…designed using a community-focused approach to provide the following benefits in addition to flood protection… “ which includes new open space, bike/walking trails, and more.  A rendering shows this integration.

An additional article from the Denver Channel provides a bit more perspective in video form on the Montclair Creek Project, including the “gray to green” approach “correcting past mistakes” focusing on the daylighted river weaving through a golf course and some more urban parts of the City, along with a greenway as mentioned above prior to outlet into the South Platte River.  The funds for the project, which were not insubtantial at $300 million, were voter-approved, with “daylighting of old waterways that were forced into pipes and buried during the industrial revolution in favor or streets, railroads and homes.”  

HEADER: Image of the 39th Avenue Greenway and Open Channel  – via the ‘Green Infrastructure Implementation Strategy‘ (page 55)

A First Map of Portland?

Jason Kingcity, creeks, general, history, maps, oregon, places, portland, rivers3 Comments on A First Map of Portland?

There’s a plethora of early maps of Portland, many of which I’ve recently included and cataloged here for reference.  One of those maps I’d never seen before recently, oddly, is this sketch-map made by William Clark (yes, he of Lewis & Clark expedition fame) from April 3, 1806, featuring a sketch of the Multnomah River, “given by several different Tribes of Indians near its entrance into the Columbia.”  The original link comes from this Oregon Encyclopedia article on the Wapato (Wappato) Valley Indians, found whilst researching native settlements in Portland, notably those around the important confluence of the Willamette and Columbia but getting a feel for pre-settlement use of waterways. The map is found in Volume Four of the Original Journals of the Lewis and Clark Expedition, 1804-1806, which constitutes the return trip of the Corps of Discovery from Fort Clatsop on the Oregon Coast back towards the east.  The entry and fold-out map includes a remarkable amount of information including natural and hydrological features, as well as references to many of the tribes as alluded to in the title.

It’s amazing to see the detail of the map and density of information, in what I assume was field drawn, probably in a canoe, fending off bears while simultaneously collecting plant samples.  I jest, but I’m constantly amazed at the ability of early explorers to represent places quickly and with much    For me, at least, it was much easier to conceptualize graphically if you rotate the map so north is facing up, so the subsequent enlargements flip this over.  This enlarged view shows the key features at the confluence, perhaps not drawn to scale, but remarkably accurate, including to the east, both the Washougal River (noted as Teal) and the Sandy River (noted as the Quick Sand). There are also notes on the various encampments on river banks, such as the Nechacolee and Nechacokee around Blue Lake in Portland on the south bank, Shoto up around modern day Vancouver Lake to the north and many more smaller encampments of the local Multnomah and Kathlamet tribes. To the west, around Wappato Island (modern day Sauvie Island) which was home to Multnomah, Clannahqueh, Cathlahcommahtup and others on Sauvie Island on the Columbia River, and around the other side of the island, known as the Multnomah Channel. See this additional post from the Oregon Encyclopedia for Lewis & Clark’s estimate of the Portland Basin Chinookian Village tribal populations here as well for more detail.

The same zone taken from a Google Earth image shows the general location of and features. The fidelity of the geography is a bit off (it’s a sketch map) but it’s all there.

Further south, the geography is a bit more sparse, but does include the upriver span of the Willamette (called here the ‘Multnomah River’) and it’s connection to the Clackamas River (heading east) including encampments of Clackamas along that river, and perhaps mis-estimating a bit how far away Mt. Jefferson actually was (see below)… and ‘The Falls’ which denotes Willamette Falls, which was an important settlements along this important confluence,  and Charcowah, and Cushhooks near the Falls….

The same view of current day area, again with a bit of misalignment of the rivers, which probably comes from the map being adapted from a drawing done by a local tribal elder, but the general features there.

The text supplements the map somewhat, with stories of meeting a group of Shah-ha-la Nation and showing them the Multnomah:

“we readily prevailed on them to give us a sketch of this river which they drew on a Mat with a coal, it appeared that this river which they call Mult-nó-mah discharged itself behind the Island we call the image canoe island, as we had left this island to the south in decending & assending the river we had never seen it.  they informed us that it was a large river and runs a considerable distance to the south between the Mountains.”

Clark takes a party to explore, and encounters huts from various tribes, along with harvesting of wappato and roots via canoes along the rivers, and found the hidden entrance to the Willamette (which he refers to as the Multnomah River, along with the tribes on Wappato Island and noted the depth of the.  He mentions that he “…can plainly see Mt. Jefferson” which may allude to it’s proximity on the one map.  As he continued to explore he mentions being “satisfyed of the size and magnitude of this great river which must water that vast tract of Country between the western range of mountains and those on the sea coast and as far S. as the Waters of Callifonia…” which if not totally true, does allude to the size of the Willamette drainage in at least draining a fair portion of NW Oregon.  He continues by visiting a long house, and learns the constant refrain of deaths from small pox and starvation. He asks for a map of the area and the people from one of the elders.  “I provailed on an old man to draw me a sketch of the Multnomar River and give me the names of the nations resideing on it which he readiliy done, and gave me the names of 4 nations who reside on this river two of them very noumerous. The first is Clark-a-mus nation reside on a small river… the 2.d is the Cush-hooks who reside on the NE side below the falls.”

They note the entrance to the Multnomah river being “142 miles up the Columbia river” from the Pacific, include the sketched map, and then are off, up-river, continuing eastward.

An excerpt of the journal, the specific passage of which is available via this Oregon Encyclopedia post here as well.

Ice Age: New York

Jason Kingarchaeology, city, geology, history, landscape, new york, places4 Comments on Ice Age: New York

The New York Times did a recent story on How the Ice Age Shaped New York with a tagline “Long ago, the region lay under an ice sheet thousands of feet thick. It terminated abruptly in what are now the boroughs, leaving the city with a unique landscape.”  This resonated with me and reminded me of posts about Minnesota’s Lake Agassiz, as well as the Waterlines presentation last year by Dr. Stan Chernicoff on Seattle’s own geological history and how the ice age covered the city with a deep layer of ice ground away over time and as it melted 10-20,000 years ago, influenced and left many traces on cities.

New York City experienced similar issues, with a two-mile thick ice layer forming over two million years back, covering the area region encompassing much of the city and all of Manhattan, with the terminal moraine reaching the zone bisecting parts of Staten Island and Long Island, until warming and retreat 18,000 years ago.

The story of many areas is the same, the depth and weight of ice shifting bedrock, and creating waterways, kettle ponds and lakes, as well as retreat leaving glacial erratics and other rubble strewn through the zones.  However it’s more distinct in New York City, as pointed out in the article:  “While the line of glacial debris across the northern United States is often poorly delineated, the hilly ridge around New York City tends to be quite prominent. Its maximum height is roughly 200 feet, about that of a tall apartment building.”

The ridges and hills determined where people settled, as they avoided these areas and found flatter ground, and I remember the specific outcrops left in place in Central Park as features, but perhaps also to avoid having to blast or remove them. (see header image above)  The article mentions that many place names are derived from this rises, appended with Hills, Heights, and Slope and also its usage in local building materials.  The proximity of the terminal moraine to New York City is unique, but that glacial history has been forgotten over time.  As mentioned:

“Despite the ridge’s prominence and early allure for scientists, it turned out to be no rival for skyscrapers and urban distractions. The moraine that shaped the city was all but forgotten. “Clearly, it’s not on the radar,” said David E. Seidemann, a professor of geology at Brooklyn College. “The educational system here doesn’t emphasize earth science. And there’s so much else to do. I’ll go to a Yankees game over geology any day.”

But the hidden remnants paint a fascinating picture, capture by geologist and environmental educator from the American Museum of Natural History, Sidney Horenstein, who also does tours of these phenomena.  He found documents showing that geologists working in the 1800s found in terms of the variation of hill to flatland geology: “Ridges, mountains and even flatlands are typically rooted in rocky strata, such as the bedrock that underlies Manhattan and makes it ideal for erecting skyscrapers. But early investigators found the hilly ridges to be composed of clay, silt, sand, pebbles, cobbles and boulders, all jumbled up together.”

The walk through reports (such as the fascinating Natural History of New York published in 1842) established a chronology of more focused work on things like history of glacial floods, and fills in gaps on geological processes, even showing the emergence of terms to describe processes, like ‘Ice Age’ which was starting to be more widely used in the 1880s.

A 1902 USGS large-format map provided some spatial information as well

The maps used colors to show variations of geology amidst the emerging city grid, and identified the terminal ridge. As the article points out:

“At first, the city used the stony ridge for woodlots and rain catchments. Slowly, the uses expanded to reservoirs, recreational areas and, in time, neighborhoods in which buildings and houses were built on strong footings and foundations for stability.  Today, despite the wide development of the ridge’s lower slopes, a Google Earth view of New York City — a composite of images from April, June and September — shows the glacial relic as an intermittent band of green.”

A larger image of one of the maps  from the folio is seen below, via NYC99 gives an indication of the rich data available – click to enlarge (image source from Texas A&M Library).

Similar to the Missoula Floods that broke through a massive ice dam and carved out the Columbia River basin, New York also had a flood termed ‘biblical’, as glacial retreat happened around 13,000 years ago, where a “... towering wave of destruction crashed down through the Hudson gorge and proceeded to smash the southern end of the local moraine to smithereens.”

It’s interesting to draw parallels between how the glacial impacts are similar on the east and west coasts, but also how they differ due to variations of geology and topography.  The hidden history isn’t just hydrology, but a combination of physical and biological processes working in tandem, over millennia. We’ve done much to erase and obscure, but traces remain, indications of these long and large processes are tucked away under our feet, waiting to attract our gaze.

“…millions of people live on or near the glacial ridge. In all, it runs for roughly 30 miles beneath New York City. Invisibly, it links three boroughs, offering mute testimony to the power of vanished ice.”

 

HEADER:  Umpire Rock in Central Park – this and all other images, unless noted, via NY Times  

Flowing South to Portland

Jason Kingcity, creeks, explorations, general, history, maps, oregon, outreach, places, portland, projects, seattle, washingtonLeave a Comment on Flowing South to Portland

Some news on the project front, which partially explains the slow output on this end lately in terms of hidden hydrology updates:  I’m moving from Seattle back to Portland.  As regular readers know, the project origins are firmly rooted in Portland, including plenty of documentation and expansion of ideas around Tanner Springs Creek (seen below), and maybe I will finally track down one of those elusive ‘I Kayaked Tanner Creek‘ t-shirts of legend.  Anyway, happy to announce this news, and Portland folks, let me know if you’re interested in some exploring in coming months.

There’s also a plethora of other areas to explore, and also to compare and contrast the unique dichotomy of Portland as a river city and Seattle as more of a ocean & lake city, and what that means/meant for development.  On that note, one item I’ve not announced is some of the work figuring out the best format for a Hidden Hydrology Atlas that will span both Seattle and Portland – so stay tuned for more of this as technology and funding aligns.  For now you can see the early version of the online example of interactive maps I’m testing out using a combination of Mapbox and my GIS database of information.  Early days, but the potential is there, and it will expand into something more comprehensive and multi-media.

While I did get to explore a number of Seattle hidden streams, there’s so much more to do and lots to document for Ravenna, Yesler, and Green Lake, and hopefully coming back up to do more investigations.  In the interim, one of my explorations I documented here in Seattle from last summer, Licton Springs, was the departure point for an essay I wrote recently for The Nature of Cities that was just published this week. Read ‘Map and Explore: Hidden Hydrology’ for some thoughts on exploring our places and connecting with our culture, geography and ecology.

So, stay tuned as projects, posts, and explorations will all pick up over the summer months.  And as always, thanks for reading.  See you all in Portland soon.

-Jason

Atlas for the End of the World

Jason Kingcase study, history, landscape, maps, parks, photography, places, precedents, researchLeave a Comment on Atlas for the End of the World

The Atlas for the End of the World is a great model for a compendium of research and mapping on a focused topic, which has relevance to my endeavor here at Hidden Hydrology.  While the content, scale and goals are different, the structure of information in the format of the ‘atlas’ and the combination of mapping, data, and critical inquiry through essay all resonate as a great precedent.

The project was conceived by Richard Weller from The University of Pennsylvania (UPenn), with collaborators Claire Hoch and Chieh Huang.  A summary of the project, launching in 2017, comes from the site:

“Coming almost 450 years after the world’s first Atlas, this Atlas for the End of the World audits the status of land use and urbanization in the most critically endangered bioregions on Earth. It does so, firstly, by measuring the quantity of protected area across the world’s 36 biodiversity hotspots in comparison to United Nation’s 2020 targets; and secondly, by identifying where future urban growth in these territories is on a collision course with endangered species.  By bringing urbanization and conservation together in the same study, the essays, maps, data, and artwork in this Atlas lay essential groundwork for the future planning and design of hotspot cities and regions as interdependent ecological and economic systems.”

Some background on the project is found in both Précis which provides a roadmap to the site, as well as an essay “Atlas for the End?” which alludes to the first modern atlas of Ortelius, the Theatrum Orbis Terrarum (Epitome of the Theater of the World) and the dawn of a new, albeit already populated, world, ready for exploration and exploitation.  As mentioned: “In 1570, when Ortelius published his atlas, the European imagination could literally run wild with whatever might be ‘out there’. Now, a mere 450 years later, that vast, mysterious world of diverse peoples and species is completely colonized and irreversibly altered by the material and conceptual forces of modernity. Whereas Ortelius marked out modernity’s territorial beginnings, this atlas—by focusing on the remaining habitat in the world’s 36 biodiversity hotspots —rakes over its remains.”

The extensive essay lays a formidable foundation for the research, touching on the impacts of the past 450 years and the loss of biodiversity through urbanization, and the identification of hotspots, as well as how cities play a huge role.  As quoted:

“Although it is not yet well monitored, it is increasingly appreciated that the metabolism of the contemporary city, no matter how divorced it might feel, is interconnected with the sources and sinks of the broader landscape. It follows then that environmental stewardship is as much a matter of urban design as it is landscape ecology. As Herbert Giradet insists, it is in cities “that human destiny will be played out and where the future of the biosphere will be determined. There will be no sustainable world without sustainable cities”.7“

The themes touch on the foundations of the shift towards the Anthropocene, and our changing ideas about nature, stewardship, and it’s relationship to the profession of landscape architecture, touching on McHarg’s environmental ethics of the 1960s and also discussing the work of biologist Daniel Janzen and work on restoration of biodiversity using a metaphor of the garden.  “Janzen’s ‘garden’ is not an idyllic scene constructed for contemplation, nor does it trade in images of pristine wilderness. Wildland “gardenification” as he refers to it, is just damn hard work. As Janzen explains, it involves “fencing, planting, fertilizing, tilling and weeding … bioremediation, reforestation, afforestation, fire control, proscribed burning, crowd control, biological control, reintroduction, mitigation and much more.”36 Janzen’s garden is a continual work in progress.”

The ideas continue in discussions on the role of protected and connected ecosystems, and metrics, in this case, using the Convention on Biological Diversity (CBD).  From the text: “The overarching framework for the project of protecting and reconstructing a biodiverse global landscape is provided by the United Nations Strategic Plan for Biodiversity 2011-2020. The key mechanisms of this plan are brokered and administered through the Convention on Biological Diversity (CBD), one of the three ‘Rio Conventions’ emerging from the UN Conference on Environment and Development (the ‘Earth Summit’) held in Rio de Janeiro in 1992. The primary objective of the CBD is that “[by] 2050, biodiversity is valued, conserved, restored and wisely used, maintaining ecosystem services, sustaining a healthy planet and delivering benefits essential for all people”.   To this end, the focus on hotspots provides a locus for where these values intersect globally, as represented with ideas of protection (and lack there of) and the ability to access massive quantities of data collected through remote sensing and being able to map it using available technologies (while cautioning against the objectivity of mapping as a practice).

A concluding essay “Atlas for the Beginning” talks about the shift to our new reality of the Anthropocene.  A globe view shows “What’s left: the world’s protected areas as of 2015” which illustrates a bleak view of the fragility of the worlds ecosystems.  The takeaway is a research agenda that includes more data and analysis, as well as developing methods of action, including a  “…longer term research agenda is to establish a knowledge sharing network of demonstration design projects across the hotspots which bring landscape architects, environmental planners, conservationists, economists and local communities together to focus on areas of conflict between biodiversity and development. These SEED (systemic, ecological and economic design) projects will show how landscape connectivity can be achieved and how urban growth can be directed in ways that support all forms of life.”

The use of data visualizations, or datascapes, allows for unique comprehensibility of issues, as seen above. “The datascapes show that if the global population were to live (in material terms) as contemporary Americans do, there would be a major discrepancy between levels of consumption and what the earth, according to today’s technologies, can reasonably provide.” One such visual on Carbon Forest (below) shows the theoretical sequestration potential and equivalent size of forest to accommodate current populations, or, in actual numbers, “The 216 billion metric tons of CO2 emitted by a hypothetical global population of 10 billion such Americans would require 9.9 trillion trees to sequester its emissions. 2

“

The series of world maps are both beautiful and informative, spanning a range of topics both physical and social… a wide array of topics.

Each comes with a short blurb and reference.  The map on Ecoregions is described as: “The World Wildlife Federation defines an ecoregion as “relatively large units of land or water containing a distinct assemblage of natural communities sharing a large majority of species, dynamics, and environmental conditions” 1. An ecoregion is a biome broken down even further. There are 867 ecoregions comprising the world’s terrestrial and marine ecology. Nearly half of the world’s terrestrial ecoregions (391) are within the hotspots.”

 

Another interesting subsection is a feature Flora & Fauna, with “the photography of Singaporean artist Zhao Renhui, Director of the Institute for Critical Zoologists, from his 2013 artwork Guide to the Flora and Fauna of the World 1. The guide presents a catalogue of curious creatures and life-forms that have evolved in often unexpected ways to cope with the stresses and pressures of a changed world.”  The species are both amazing and somewhat disturbing, such as the bionic AquaAdvantage salmon (below), “…a genetically modified salmon that can grow to its adult size in 16 to 18 months instead of three years. The AquaAdvantage salmon has been modified by an addition of a growth hormone regulating gene from a Pacific Chinook salmon and a promoter gene from an ocean pout.”

Read more on the project via this post on the ASLA Blog, as well as a relevant article by Weller from the innaugural issue of LA+ Journal, entitled ‘World Park‘

All images and text: © 2017 Richard J. Weller, Claire Hoch, and Chieh Huang, Atlas for the End of the World, http://atlas-for-the-end-of-the-world.com 

HEADER:   Hotspot Cities: cities of 300,000 or more people projected to sprawl into remnant habitat in the world’s biological hotspots

Washington Water Toponyms

Jason Kingcreeks, landscape, language, maps, places, rivers, streams, washington, watershedsLeave a Comment on Washington Water Toponyms

I’ve been inspired by the work many others have done to capture the qualities of coverage of waterways at national scale both in the US and the UK, and beyond the mapping, appreciate their investigations into the unique distribution of place names, or toponyms.  The language of the waterways informs more local hidden hydrology endeavors, and understanding regional vernacular variations provides a snapshot into our varied relationships with water.  While a glance at the Pacific Northwest via these other maps shows that the predominant name for waterways is probably going to be either creek or river, I wanted to dive a bit deeper to see what other names are used to denote waterways.  To accomplish this, I spent some quality time with the USGS National Hydrography Dataset (NHD) to unlock a bit of the secrets of regional variations.

For starters, the NHD is an amazing resource of information, pulling together a comprehensive collection of data on flowlines, watershed basins, and more and the ability to get data from a variety of formats for small to large basins and states.  From their site, the purpose of the data is to: “define the spatial locations of surface waters. The NHD contains features such as lakes, ponds, streams, rivers, canals, dams, and stream gages, in a relational database model system (RDBMS). These data are designed to be used in general mapping and in the analysis of surface water systems.”  The first steps are a bit daunting, as the State of Washington included data with over 1.3 million flowlines, seen below in aggregate. The flowlines aren’t any one single waterway, but are the individual segments that make up each creek.

While the data preserves local basins shapes by sprawling outside state lines, I wanted to make this unique to Washington, so needed to clip it to the state boundary.  This ended up being a bit of a task for my rather slow computer to crank out the clipping, so I had to think of some alternatives to simplify the dataset.  Interestingly enough, over 80 percent of the flowlines (around 1.1 million of them) are unnamed, and while I’m sure are perfectly lovely bits of creek and river, they don’t help in our purpose in terms of deriving place names.  Eliminating them also serves the dual benefit of reducing the size of our working dataset quite a bit.  After trimming to the state boundaries, we ended up with a nice workable set of around 170,000 flowlines that have names, seen below.

Per the NHD FAQ page, “Many features also are labeled with the geographic name of the feature, such as the Ohio River. The feature names must be approved by the Board of Geographic Names (BGN) in order to qualify for inclusion in the NHD.”  More on the BGN and the wonderful assortment of place names that exist in these lists beyond their descriptor (which is perhaps the fuller idea of toponyms), in this case we break down the list and see what comes to the top.   Not surprising, but the use of the terms Creek and River dominate the landscape of Washington, accounting for 98% of all named flowlines.

Of the totals, creeks truly dominate, with around a 75% chance that a trickle of water in the state will be referred to as a creek.  The larger, less numerous rivers make up 23% of all flowlines, and the map above paints a wonderful portrait of the density of waters.  Separated out by type, you see the branched structures of trunk and stem that pumps water through most of the mountainous west side of the state, with the larger, drier plains to the east more open.  All total the combined length of these equals over 30,000 linear miles.

1. CREEKS

2. RIVERS

So we live in a creek and river area of the world.  Amidst these dominating toponyms are a distributed layer of types of flowlines that make up the remainder of the story of Washington, that final 2 percent, emphasized in a darker blue below.

The secondary naming of these includes the most common, isolated and color coded, with a legend denoting the eight most common alternative flowline names.

The relative percentage as a portion of that slim 2% of state flowlines, include:

  1. Slough (30%)
  2. Fork (16%)
  3. Canal (16%)
  4. Ditch (9%)
  5. Wasteway (4%)
  6. Branch (4%)
  7. Run (4%)
  8. Stream (3%)

The remaining 14% are composed of small portions that include Lateral, Brook, Drain, Slu (a variation of Slough), Gulch, Channel, Siphon and it’s alternative spelling Syphon, Washout, Waterway, Swale, Glade, Pass, Gate, and Range.  Many of these as we see, are geographically located towards the center of the state where agricultural landscape has created larger modifications and creation of waterways (described in the NHD data under the names like Artificial Path, Canal Ditch, and Connector).  There’s a split between more traditional waterway name variations (i.e. Slough, Fork, Branch, Run, Stream) and those that mostly utilitarian, capturing the poetry of industrialization (i.e. Wasteway, Ditch, Canal, Siphon, Lateral).  Removing the background landform, you see the composite of the different stream types as a whole, with creek/river in blue and the remainder by color.

For a more local view, the NHD data is a bit less sparse, not capturing the same amount of complexity is smaller urban waterways, plus without the other water bodies like lakes the geography seems somewhat off.  The purple to the west in the Olympic Pennisula shows a density of flowlines referred to as streams, and the darker red denotes a number of local sloughs that exist in local river systems.  It’s harder to see, but you can catch the Ship Canal in this group, and the slightly lighter red fork in the center is the infamous Duwamish Waterway, the lower stretch that runs through Seattle and ‘lost’ its designation as a river – interestingly enough it’s the only flowline in the state with that moniker.

I was expecting the dominance of creeks and rivers in the nomenclature, but was also really surprised that these combined to make up so many of the collective flowlines. Perhaps early settlers and place-namers lacking a bit of creativity.  It was also a good surprise to find a wealth of other place names in Washington, albeit many used to describe man-made features, including the most poetic name of wasteway, but enough fun to find an occasional branch, fork, brook, and run, which are more common elsewhere in the United States, per the other US maps.

These are pretty basic graphics exported from GIS just to give a feel for the data, so I’d like to play around more with representation, perhaps some sort of heatmap.  Also I’m eyeing Oregon for a comparison, and maybe wanting to dive into the waterbodies as well beyond linear flowlines, so more fun to come.  Who knows, an atlas of the whole country with a top ten of their most common names of each state.  Or maybe not…

HEADER:  Excerpt of River and Stream Composite Map – data from ESRI, NOAA, USGS – Mapping by Jason King – (all maps in post same attribution, © Jason King, Hidden Hydrology, 2018)