
Clouds
The Mountains Above Us
When my daughter and her family bought a house on a ridge looking directly into the Santa Ynez mountains, I was delighted. These are the canyons and mountains where my dad and grandfather used to explore and hunt when my dad was a boy. That first winter, when the rain clouds lifted, it revealed cliffs laced with waterfalls. In February, blooming chaparral dusted the mountains with white flowers and in April with blue blooms.
Chaparral is my favorite plant community, with its dense shrubs superbly adapted to long hot summers and short wet winters. The Santa Ynez mountains have their own climate, notably the sundowner winds which roar downslope raising temperatures and fanning fires. They are the western-most transverse range which is bent along the San Andreas fault, explaining why Santa Barbara faces south instead of west.
The mountain rocks are studded with fossils of sea creatures laid down from the millennia when the region lay under a warm sea. The rugged mountains cut off Santa Barbara from the north until late in the 19th century.
A Meager Winter
By Phila Rogers
The winter rains came late this year, with the first light rain falling the last day of February. Two robust storms followed the first week of March, giving us a seasonal total of eight inches. With only a scattering of rains since, that may be it until November.
We live in a Mediterranean climate characterized by a mild, wet winter and a hot, dry summer; a climate found only in southern and southwestern Australia, central Chile, coastal California, the Western Cape of South Africa and around the Mediterranean Basin. Despite extended periods of drought in the last decade, we had above-average rainfall for the last two years and our reservoirs are almost full.
I love our winter storms. Each one has its own personality. Some begin with a prelude of high wispy clouds made of ice crystals. Others sweep in on mid-level clouds and arrive on a counterclockwise wind from the southeast.
Here in Santa Barbara a winter storm brings the clacking of palm fronds and the pleasing odors of various sage. As an avid weather watcher, I wonder if spring will bring the May and June fogs or possibly something unusual, like a thunderstorm.
As the rainy season ends the landscape changes from green to gold. The grassland composed mostly of wild oats releases its seeds as the grass blades fade to a pale yellow. Fields of mustard grow tall and bloom with vivid yellow flowers. Many think of mustard as a native plant but in fact it arrived in California in the fur of long-horned cattle in the late 18th century. When the rains come again in the late fall, green will spread again across the landscape like a rising tide.
Illustration by Carol Anderson
In Celebration Of Clouds

I call it the landscape of the sky.
With my fading eyesight, the landscape around me is confused by haze, but the sky is brightly lit and clouds do not require precise vision.
The sky is best viewed while lying supine, a position kind to my tired bones. If I drift off, the landscape may have changed without me. Some clouds have dissolved altogether, reclaimed by the empty sky, while other small clouds may have been claimed by a larger one.
I must be imagining it but it seems to me the cloudscape is the boundary land between earth and outer space, or maybe even a border between living and dying.
Sometimes those high, thin, wispy clouds are the leading edge of an approaching storm. And when the clouds sink toward the earth heavy with moisture, I am glad.
When the storm has passed, the north wind drives the white-sailed galleons along the horizon, their cargo spent.

September 22, 2022
This is one of the noteworthy days of the year, the fall equinox and the first day of fall. Like the spring equinox six months from now, day and night are roughly equal in length. The Bewick’s Wren is singing a more joyous song and the Oak Titmouse sings a combination of their spring halleluiahs with their raspy call notes. Nothing will come of it, of course, and the days will continue to grow shorter by two minutes a day until we are jolted by darkness falling by 7 PM.
In Santa Barbara on the south coast, a 100 miles west northwest of Los Angeles, fall doesn’t really show up until October, when the California grapevine turns red on the fence and the winter birds show up in the coastal gardens.
Over the last few days, Bay Area birders are plucking my heart strings by reporting the first Golden-crowned Sparrows of the season. I remember those chilly mornings in the Berkeley Hills when I would walk up the street towards the pasture whistling their song. If they had arrived in the early morning hours after a long night’s flight, they answered me with one or two minor key notes. I would yelp with joy and dance a quick jig. When I returned home, I made an entry in my notebook, circling the date in red.
It would be a few more days before the little flocks worked their way into the neighborhood to settle into their winter territories. I wondered if these birds were the ones that had come last year and maybe several years before. The good news was that they remained until mid or late April, developing the bright yellow crown, before departing for the far north. During the winter you could count on them singing just before it started to rain.
As far as I know there are no golden crowns in this neighborhood or even in Oak Park. They are most often reported in weedy fields in open areas like the upper Elings Park.
A single mature male has spent the summer feeding with several Song Sparrows in a clearing near Los Carneros Lake. Apparently, it declined to join the others of its kind for the migration north in April. Was he damaged in some way or simply lacked the normal instinct, the irresistible urge to migrate?
Hearing the Western Tanagers on the move, I will start listening for our winter birds, though I know it’s probably too early. I arrived at Samarkand as a reluctant migrant from Northern California at this time nine years ago. It was during the lull between the seasons. I was disconsolate. I looked for one familiar bird. Finally, there it was — a California Towhee scratching in the leaves alongside the pathway.
Something did arrive early this year, a substantial rain but with hardly a sprinkle here. Elsewhere, it was enough to signal the annual nuptial flight of the termites when some of these subterranean creatures grow a pair of gossamer wings for a day’s fling above ground in the bright air. The queen ascends high in the sky pursued by ardent males eager to mate with her. Then as quickly as it began, it was all over and the termites resumed their lives in the dark with a pregnant queen, leaving behind a shimmering carpet of discarded wings.
I had assumed this early storm was like the ones to follow, moving down the coast from the north. But the cause was Hurricane Kay, an extensive, well-organized storm which had originated off the coast of Baja California, slowly weakening as it moved north to bring varying amounts of rain.
Nature sent us a consolation prize though — a double rainbow which felt more like a gateway to grander things.
Summer Monsoon
MONSOON SEASON
When webmaster George Dumas pushed the button to publish “Summer Doldrums,” I suggested that we take a month off as nothing much was going to happen during the summer months. Then, on the morning of June 24 I woke to a day that both felt and looked different. Cumulus clouds were heaped up against the backside of the Santa Ynez mountains and flotillas of small white clouds with lacy edges stretched across the sky. Listening to my weather radio, I learned that a monsoon brought violent storms to the Los Angeles basin and the surrounding mountains.
Monsoon season most often occurs in July and August and brings most of the annual rainfall to the Southwest. We were experiencing the edge of the first one today.
Most monsoons occur when the hot summer sun heats up the land and the wind shifts to the south drawing up the moist, unstable air from the Gulf of California or the Gulf of Mexico.
Along with rain came strong wind gusts and even some hail in Los Angeles. The electrical storms produced an estimated 3,600 lighting strikes, one igniting a brush fire in the Tehachapi and another tragically striking and killing a woman and her two dogs who were taking a morning walk along the San Gabriel riverbed. Fatal lightning strikes are rare with this being the first one of some 20 occurring each year.
Only the northern edge of the monsoon reached Santa Barbara. I spent the day outside with my camera, my eyes always on the sky. The air was silken, not too humid without any of that sharpness we associate with the typical onshore flow from the ocean. It was the kind of day that makes you feel like a different person.
Now, at almost 4 PM, the show is mostly over. The heaps of clouds over the highest mountain ridges have withdrawn or simply melted away leaving behind a few cloud fragments.
Although failing to bring us rain, the monsoonal visit was a delightful change from the usual coastal weather.
SUMMER SOLSTICE

It’s been several weeks since the Summer Solstice, but the days grow shorter so slowly at first that you’re not apt to notice. Because of the earth’s tilt toward the sun, the sun is directly over the Tropic of Cancer at a latitude of 23.5 degrees north. The Tropic of Cancer passes over Baja California as it circles the globe, or more precisely, over the small seaside town of Todos Santos, an hour’s drive north of Cabo San Lucas where a planted stick casts no shadow.
Because of the slow heating of the land by the sun, the highest temperatures will be several weeks later in mid-July.
Within the Arctic Circle, at the Summer Solstice, the sun will shine for 24 hours while darkness will prevail at the south pole.

[Photo by Jodi Turley]
Over the millennia, various cultures have celebrated the Summer Solstice in different ways. Here in Santa Barbara we have a parade with imaginative handcrafted floats, bands (emphasis on drums ) and costumed dancers moving to the beat. For me, butterfly wings glowing in the sunlight epitomizes summer.
FOLLOW BLOG BY EMAIL
Enter your email address over on the right to follow this blog and receive notifications of new posts by email.
SKY WATCHER
After a rainless January and February, we were excited to learn that a storm was moving our way. I read that it was being carried down the coast by our old friend the “jet stream,” that fast-moving river of air moving from east to west which circulates around the globe often delivering weather systems to our coast. Or at least it used to.
The possibility of a storm deserved a morning sky watch. Soon after sunrise, I stepped outside on my balcony and aimed my camera at the sky and would continue to do so at hourly intervals until noon. As a long-time sky watcher (or storm watcher) in the Bay Area, the evidence was not encouraging.
Though winter storms generally form in the Gulf of Alaska and move down the West Coast, the winds that accompany them blow counterclockwise, so approaching storms are preceded by winds from the southeast. This morning the wind blew consistently from the northeast and was cold and dry, rather than moist and mild.
What I loved about most winter storms was the buildup that preceded the arrival of the storm itself. From my Bay Area hilltop house, I could scan the horizon from the south of San Francisco north past Mt. Tamalpais to Sonoma County. Not much escaped my attention.
The classical winter storm usually begins with high cirrus clouds often in fantastical shapes like wispy feathers. The clouds spread across the sky from north to south. At some point the wind begins, fluky at first before settling into gusts from the southeast growing in strength as the clouds thickened and lowered.

After years of living in Berkeley, I knew the wind direction without looking. An early October storm carried the strong, acidic odor of cooking tomatoes coming from the Heinz catsup plant in southwest Berkeley. If the wind was blowing from the northwest, it would carry the strong petroleum odors coming from the Chevron distillery in Richmond.
In Santa Barbara, where I have lived for 10 years, I smell mostly the odor of cooking tortillas and the scent of flowers. Sometimes the alarming smell of burning chaparral tells me there is a fire in the mountains. When the wind blows from the northwest during in the long summer, the air smells vaguely like ammonia or slightly salty of kelp drying on the beach. It feels heavy and damp.
I’ve often wondered why I am so exhilarated just before a storm. I dash around, bringing in outdoor furniture, rolling up outdoor shades and tying them tight. Hankering for the feel of soil, I plant that final sixpack of pansies ahead of the rain.
Now I’ve learned the likely cause of this joyous energy – negative ions. Negative ions associated with clouds and wind facilitate the transfer of oxygen to the cells. No wonder I’m so exhilarated. After a storm has passed, denied this extra oxygen, I descend into what I’ve always thought of as a post-storm slump.
None of this energy was associated with today’s morning’s storm watch which began with a few isolated clumps of white clouds and a wind that never shifted around to the southeast. Instead of the air warming as it usually does with an approaching storm, the wind rattling in the dry foliage was cold and odorless. By noon the clouds had mostly disappeared leaving only a few shards to help color the sunset.
Later I learned that the storm track was inland, bringing a dusting of snow to the higher coastal peaks while delivering generous, dry fluffy snow to the Sierra. I was disappointed after high hopes for a good rain, but I did enjoy the variety – a welcome relief from the still warm air from sunup to sunset.
TWO BOOKS FOR THE SKY WATCHER
The first book, sumptuously illustrated with clouds from around the world is titled: “The Cloud Collector’s Handbook,” by Gavin Pretor-Pinney. It is the official publication of The Cloud Appreciation Society. The Brits do love their weather. Some photos and descriptions are of familiar clouds. One is so rare you have to travel to the north-east corner of Australia to see it.
The second book is “Reading the Clouds: how you can forecast the weather,” by Oliver Perkins. He is another Brit, a sailor for whom knowing the weather is critical. One reason for “having your head in the clouds” is that they are full of valuable and interesting information.
Where I Live
(Excerpts from my book The Best for Last)
Early November
The resident hawk
Repeats its urgent calls.
Where is the rain?
The temperature is above eighty.
Night falls with red skies
Color caught by the high cirrus clouds
Too thin for rain.
With darkness comes
The cricket stridulations,
The final notes of the fading season
After midnight I step out on my porch,
Looking high to the south.
Orion waits, trailed by Sirius,
The hunter’s faithful dog.
Venus will soon separate itself from the rising sun
And before month’s end will shine alone
In the eastern sky.
Once I’d imagined spending my final years
In the town where I was born
In a tiny house of my own design
One room only
With alcoves for bathing, sleeping, fixing tea
A steep roof with a skylight or two
A generous porch under a sheltering eave
High in the Berkeley Hills,
But instead, my final years
Will be spent in Santa Barbara
in a spacious apartment
One of many apartments
For elders like myself,
Close to family,
a hedge against loneliness.
The geographer in me
Wants to tell you
That Santa Barbara is located
At the southern end of central California.
Maybe 50 miles below Pt Conception
Where the coast bends inland
Thanks to the San Andreas Fault
Flexing its muscles.
So now the coastal mountains run
From east to west,
and most confusing of all
You look south if you want to see the ocean.
For me, the ocean has always been to the west,
And the direction of the setting sun
Where if you sail far enough
You’ll bump into China.
The high Santa Ynez Mountains to the North
shield the town from certain cold draughts.
But in downpours, the mountains
Shed all manner of debris
From silt to sandstone boulders
As big as cars.
Now as an amateur geologist,
I’ll tell you that this knoll
I call home, is surrounded
By flatter land referred to
As an alluvial fan,
Crossed by creeks that
Only show up when it rains.
Locals brag about the mild climate
Forgetting about those vehement moments
Of gale-force winds
Called sundowners.
Or what about the microbursts
Which have been known to knock a plane
Out of the sky?
And there’s nothing mild about my landscape.
Never still — it twists, heaves and cracks.
Worse, it is said that all the commotion
Is bringing Los Angeles ever closer.
Once we were covered by a warm sea
With dinosaurs wandering the shallows.
Later mountains rose up,
Full of seashells.
Now it seems that our future is drought.
I look out the east-facing windows
Down into Oak Park with its
Pale limbed-sycamores and faded foliage.
It’s a peoples’ park
With mariachis on the weekend
Shouting children,
Birthdays with piñatas
Quinceaneras, sometimes a funeral
Look up to the first ridge
To St. Anthony’s towers
And to the two rosy domes
Of the old mission.
Higher yet is the bulk
Of the Santa Ynez mountains
and the conical shape
Of my mountain – Montecito Peak
See how the angled sun
Deepens the canyons.
Slide your eyes sideways
To where the mountains
Slip into the blue line of the sea.
Now face south
Over our native garden
Bordered oaks from the park
To the silent creek bed.
I look for hummingbirds, bush rabbits
and worry about coyotes
The east hills, called the Mesa
Holds off the fog
Until after dark,
when the hills are breached.
Oh yes, my garden off the front door
The narrow porch of a garden,
Hung with red geraniums
And softened by pots of ferns
I lie in my bed beneath the windows
Hoping for wind to move the chimes.
I lift my head at dawn.
Do I see the silhouette of the mountains
Against the lightening sky?
Or are we cocooned in the fog
That drips from trees
Almost as welcome as rain.
And what is the first bird this morning?
The clink of the towhee
The querulous wren
The sweet ring of sparrows’ song?
Now you are hearing the voice of the birder
Leaning on every song
In the absence of good eyesight.
Acorn woodpecker, flicker
With strong beak and loud call,
Or the relentless caw of the black crow,
Boss of the neighborhood?
Will I be lucky enough
To have an owl’s hoot rouse me
In the early morning hour?
I feather my nest
With a down comforter
Books,
Bouquets of pungent sage,
Baskets of lichen.
How do I finish this short tale?
A day ending, I suppose.
With the dark coming on by five
A tale of rain arriving?
A gusty wind from the southeast
Testing itself.
In the early morning hours
Between midnight and dawn
The rain falls
I smell it first
And then sweet fragrance of hope
Could this be
The beginning of a season
Of abundant rains
Enough to end the drought?
COMING IN THE SPRING: The Best for Last: The Nature of Santa Barbara by Phila Rogers. Includes the blogs and a number of short pieces.
A Family Vacation at Big Bear Lake
After having lived most of my life in the Bay Area, California mountains meant only the Sierra Nevada. My earliest memories are of Lake Tahoe with the bands of blue, the color deepening the further you were from shore. I remember the translucency of the water, the whiteness of the beach sand and the way the sun shining through the water left a dazzling pattern on the sandy bottom. And the granite, always angular and glistening with feldspar.
Vacation in the mountains was a reprieve from home and the rank eucalyptus odors. Now it was sage and pine, and brilliant, hard edged cumulus instead of the dull sheets of stratus.
But it was time to put all that behind and turn my thoughts without aversion to the Southern California Mountains, another transverse mountain range like the Santa Ynez range. The deep power of the San Andreas fault had twisted the mountains sideways, contrary to the northwest trending of the other California ranges.
With some of the family now living in Southern California, a three and a half hour drive to Big Bear Lake in the San Bernardinos won the day over nine hours north to Lake Tahoe.
The San Bernardino Mountains rise abruptly on all sides out of its arid landscape. The curving road makes a quick ascent passing occasional coulter and knobcone pines, dried stalks of yuccas and chaparral. In a land of few lakes, only dams can create a body of water, gathered mostly from snow melt. Big Bear Lake, no exception, occupies its own shallow valley set in low mountains and open conifer forests. Unlike the Sierra, where millions of trees have succumbed to the long drought and insect attacks, Big Bear’s trees look healthy, perhaps being accustomed to dry years.
While noticing the distinct differences between the appearance of Sierra Nevada and the San Bernardinos, I remembered reading of their similarities. Both began as batholiths formed of cooling magma deep underground before being uplifted some three million years ago. Older rocks overlain the newer granites. But in the Sierra Nevada, the old rock eroded away with the heavier rains and the extensive glaciation. In the Santa Bernardinos, with glaciation only on the highest peaks and less rain, more of the old rock remains.
Because we were nine people, we rented a large, recently remodeled house which is currently on the market for three and a half million dollars. While the family took to kayaks and paddle boards, I settled in on the deck to figure out this place.
The dominate pine is the Jeffrey – a close relative of the ponderosa (yellow) pine, which along with the coulter pine, are all members of the yellow pine family distinguished by packets of three long needles which produce nice harmonies in the wind.
The fir family was represented by white fir growing, at the deck rail, with short, dense needles which point upward. Each species seems to have its own distinct odor. Press your nose into the cracks between the plates of bark on the yellow pine and you smell vanilla. Sniff the white fir and you get an essence of pine and citrus. Be like the native American Indians, brew a cup of tea with the needles and you have your daily requirement for vitamin C.
But what took my fancy was the pair of sugar pines above a neighbor’s roof. Aside from being both the largest and second tallest in the pinus family with uncommonly long pine cones, I love this pine. John Muir savored the exuded gum which he said was sweeter than maple-syrup. The branches are arranged on the straight trunk often symmetrically, but sometimes a branch will shun order and stretch out further than the rest. Cones hang near the tip of the branch. I remember watching them in a winter wind swaying as if they were extravagant ornaments. Once, while examining a cone a foot and a half long lying on the ground, I remember someone telling me that the scales expand and contract with the change of temperature and the prickles make a grove in the soil for the seed. I’ve never been able to find another citation for that charming “fact” since.
The forest, at least in the neighborhood of our house on north-facing shore is knitted together by an understory of a tall manzanita called Pringle Manzanita. The season for its pink urn-shaped flowers is long past and only a few dried berries remain.
Time to shake off the lethargy that comes with an occasional fleecy cloud drifting across the blue and then dissolving or the soft song of pines, and explore the rest of the lake. The dam is a modest one required only to hold back the snow melt and the marshy waters in the shallow basin. Once around the corner to the drier south-facing shore, sages and the sturdy Sierra juniper make an appearance.
At the visitor’s center, we take literature on the trees of the region and the description of a champion lodgepole pine further up the mountain which sounds almost reachable by a short trail.
It appears there would be no avoiding the walk once my daughter learned of it. Children, no matter how old themselves, are reluctant to entertain the ills (real or imagined) of their elders. I did bring my boots so maybe I can avoid a compound fracture when I turn my ankle on the inevitable loose rock.
Once we turned off the road that circles the lake, we were in the forest headed uphill. We pitched and heaved over the bumpy road. But once in this sub-alpine forest we felt like we were back in the forests above Lake Tahoe. Though I am considered the chief exclaimer in the family, we all exclaimed over this familiar beauty. No more yellowish rock. Here the granitic core of the mountain revealed itself. The understory became varied – sometimes tender green fields of bracken ferns, other times corn lilies.
We parked at the end of the road where a sign pointed downhill to the lodgepole pine and to the Bluff Lake Preserve. I recognized this kind of trail – decomposed granite made “interesting” by rocks and exposed roots. My grandson Stuart walked close behind me and my daughter ahead of me. I focused on what was underfoot allowing only sidelong glances at the creek next to the trail over hung with
wildflowers, the first such sight in these mountains. The trail leveled out as we approached the lodgepole pine grove. Lodgepole pines are uncommon in this southern forest. They hark back to a cooler era. My joy was somewhat tempered by remembering that I had to walk back out. I didn’t care. I hadn’t expected this gift in my 89th year.

The old giant was closely encircled by younger trees (as I am by my family). The tree overlooks a broad green meadow—a meadow which not so long ago had been a pond. In the Sierra, the Lodgepole pine is the first to show up as the pond becomes a meadow. As other trees move in, the meadow becomes part of the forest.
The noble tree is a part of a national registry of the largest known of its species in a particular geographic area. A nearby Jeffrey pine is several hundred years old, an “old growth” survivor in a forest that had been heavily logged
The champion lodgepole pine from its meadow and two oldtimers.
Looking back – WINTER AFTER ALL
When one of my friends fell on an icy path this morning and Gibraltar Dam flowed into its spillway, the first time since 2011, I decided that winter could not be ignored.

I hadn’t considered writing about Santa Barbara in the winter thinking that the season had been mostly passed by in these years of drought. Then yesterday, December 23, we had a storm that was worthy of qualifying as a winter storm in every way. The day began with a thin cloud cover which built during the morning to promising layers of clouds and brief gusts of wind, which by noon led to rain. After slacking off in a way that I had become used to during these dry years, the rain built again as if to defy my pessimism. By mid-afternoon the rain built to a real gully-washer. I was lucky enough to be in my car so I could enjoy splashing through flows of water at every intersection and best of all, seeing Mission Creek coursing down its creek bed after so many months of being bone dry.
From the sound of my bamboo wind chimes during the night, I knew the storm had passed to the east and the wind had shifted to the north as it does along the coast after a rain storm. The cold wind continues today pushing around remnant clouds, now empty of their contents.

I know storm must follow storm to make the creek a winter feature and the soil be soaked enough to start recharging the depleted water table. Lake Cachuma which lies in the valley between our mountains, the Santa Ynez, and the higher range to the east, is the reservoir which holds our water supply. At present, it’s almost no lake at all, having shrunk to less than 7% of its capacity. Vultures have taken to roosting on the rim of the dam.
December ended with the rainfall slightly above normal.

January was another matter altogether thanks to massive storms brought across the Pacific by an atmospheric river — a new word in my weather lexicon. An atmospheric river can be several thousand miles long to a few hundred miles wide. Drawing up moisture from near the Hawaiian Islands, the warm air can transport large amounts of rain. It’s what we once called the “Pineapple Express.’
The atmospheric rivers produced five days of good rains. At the end of January, rainfall for the month was 8.96 inches rather than a normal 2.86 inches. Even the lawns, most of which were allowed to go brown over the summer and fall, were green again.

The rains continued intermittently until Friday, February 17. The papers were advertising that the biggest storm of the season was on its way. Over the years, I have learned to be suspicious of such a build-up which often leads to disappointment. I believe in sneaker storms – the ones which arrive with little or no advance warning. That may be the old days before sophisticated weather-measuring equipment and computers, which can put together predictive models, eliminated much of the guesswork.

At 5 AM heavy rain was falling, serious, confident rain. By mid-morning the velocity of the rain continued to increase. Coarse and dense raindrops were being driven by gale winds from the south-east. By early afternoon, the rain had slackened enough to allow me to drive down to the Mission Creek just below us. Others had already gathered. Some of us stood on the bridge itself which was trembling with the force of the volume of water pouring a few feet beneath. On the opposite side of the bridge where the stream bed is narrowed by rock walls, boulders were being slammed together. The percussive, booming sounds resembled thunder. Some people, unnerved by the violence, hurried back to their cars. As a fan of such drama, I stayed put.

The storm finally moved on leaving 5-inches of rain downtown and heavier amounts on the mountain slopes. Mission Creek up Mission Canyon left its stream bed and temporarily carved out a new route. Further engorged by a cargo of mud, the stream poured over the old Indian Dam.
The gift for me was that Mission Creek became a real stream, a winter stream which flowed for weeks on end, not just for a day or two after a rain.

Now it’s early April and the creek has ceased to flow. It survived for few more days as isolated pools, until it disappeared altogether. I like to think that it continues to flow underground bringing moisture to the roots of the sycamores and to the other streamside plants.
Rattlesnake Creek, a tributary of Mission Creek in flood conditions.
Credit: Ray Ford
(Please note the material following the video is not part of this presentation.)












