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My Dream House and the Pond

News Feed
Tuesday, March 12, 2024

I can’t talk about our house in the Bronx without telling you first about the pond out front. Given how much worse flooding can be elsewhere in New York City—even just two blocks to the east along the valley of Broadway, where the sewer is always at capacity—not to mention elsewhere in the world, I’m embarrassed to gripe about my personal pond. These days, such bodies of water are everywhere. Mine is not the only pond, but merely the pond I can’t avoid.The pond dilates and contracts according to water levels. After a string of dry days, it may shrink to a puddle. After a storm, it may stretch to the length of a freight car, spilling into the middle of the street. It’s bad for curb appeal. Its sources are environmental, structural, and complex. On the rare occasion the pond dissipates, it leaves behind a residue like black mayonnaise.The pond is almost always there. Our region is getting wetter as the climate changes. More rain, more storms, more often. The infrastructure of our city, at the edge of the rising sea, isn’t fit to handle so much water. Sudden, torrential downpours overwhelm our outdated drainage systems, especially at high tide; drench the subway system; and, in some low-lying places nearby, turn streets into sewers and basements into death traps.In summer, the pond breeds mosquitoes and collects litter: cigarette butts, scratched-off lotto tickets. In winter, I worry the pond will become a slipping hazard. This is what I say when dialing 311, the city’s helpline, in hopes of remediation. An elderly neighbor could slip on the ice and break a bone. The pond could collapse into a sinkhole.Tell it to the DOT, lady, says the Department of Environmental Protection. I do. Nope, says the Department of Transportation; because of the tree, this is a problem for Parks. I follow up. Weeks pass. The Department of Parks and Recreation directs me to the Department of Health. Months pass. What you need to do for ponding, says the DOH, is try the DEP. I write to my city-council member: I’m being given the runaround. Weeks pass without reply. Surely, this wouldn’t happen in the rich neighborhood up the hill. As a city worker myself, I know this dance well—this absurd, disjointed roundelay.[Olga Khazan: Why can’t I just rent a house? ]I ruminate over the pond. It has caused me not just embarrassment but shame. It has turned me scientific, made me into a water witch. I understand that the pond is beyond the scope of any one person, or any one agency, to handle, and that it’s perilous to ignore. The pond is a dark mirror; in it, our house appears upside down, distorted. It reflects deeper problems of stewardship and governance and the position of our house in relation to both. We are privileged to own a home. Yet we live on land that will drown, that is inundated already. The pond is a portal. Sometimes it smells, this vent hole of the netherworld. Beneath its surface, something lies concealed. Given the fact of the pond, why did we buy the house? Now that we dwell in the house, what to do about the pond?Technically, the pond isn’t on our property at all. Our home inspector had no reason to suspect it. It belongs to the city, along with the street where it spreads. This is what we were told on the rainy day we arrived for the final walk-through before closing on the house in the deadly spring of 2020: The pond was up to the city to fix, with taxpayer dollars.Plenty of folks were deserting New York then. I mean hundreds of thousands. That we were committed to staying in the city was both an act of necessity and a point of pride. For my husband and I, the house was a step up from the crowded three-room apartment in Washington Heights where we’d sheltered in place, away from the mad snarl of highways whose traffic had given our boys asthma: a place to stretch out, a sign of our upward mobility. The American dream. To a Black family without generational wealth, some of whose ancestors were property themselves, it signified even more: Shelter. Safety. Equity. Arrival. A future for our children.We fell in love with the house as soon as we saw it, a run-down detached brick home in a working-class neighborhood with a little garden in back and windows on all four sides. The house had solid bones. We rejoiced when our offer was accepted. Yet until the day of the final walk-through, we had never visited the house in the rain.That morning, the pond greeted us like the opposite of a welcome mat, giving shape to whatever latent misgivings we had about making this move. I felt hoodwinked. Buyer beware! I waded into the middle of that bad omen to gauge its depth. Murky water sloshed over the tops of my rain boots, drenching my socks. Good Lord. It was so much more significant than a puddle. I wondered what it was, how to name it, and why it was here. Was what I stood on actually land, or something less concrete? Could it have been a wetland, once? Why hadn’t the pond been disclosed? Because it didn’t have to be, said the tight-lipped seller’s agent representing the estate of the previous owner, an old man named Jeremiah Breen.That night, my husband and I lay awake in bed, discussing our options. Sirens sounded up from the street. People were dying of COVID all around us. Purportedly, the house sat outside the floodplain. But what if the pond got bigger with worsening weather? Would it pour into the basement? Was the house’s foundation as solid as we’d been told? We doubted that the city would handle the underlying issues—not while hobbled by the pandemic. Would flood insurance be enough? Would the house be around to bequeath to our children, or would it be underwater? Was it an asset or a millstone? How high would the waters rise? How soon? Did we even believe, deep down in our souls, of ownership of this kind? Why fake like we or anyone else could own the land?Such questions of capital consumed us deep into the night. The bottom line was this: If we pulled out of the deal, we’d lose our down payment, amounting to two years of college tuition for one of our kids. By dawn, we admitted our disillusionment. We’d already crossed the Rubicon, imbricated in the twisted system that brought about the pond. Or so we said because nevertheless, we still loved the house.We renegotiated the purchase price; we moved in.Later, I learned that many current maps for flood risk overlap with maps of historic housing discrimination. Geography determines a neighborhood’s risk and, this being America, so does race. Neighborhoods that suffered from redlining in the 1930s—when our house was built—face a far higher risk of flooding today. The pond suggested a submerged history beneath the daily surface of things.The house was not just a risk but a wreck. Its rusty tanks sweated out oil that looked like blood onto the basement floor. Most of its windowpanes were cracked; its floors, uneven; its doors, out of plumb. It lacked adequate insulation. Under the creaky old planks, we discovered a newspaper dating back to the Depression. The front page addressed the use of antiques in home decoration. It featured a photo of a card room with an 18th-century Queen Anne table being used for bridge. How far back could I imagine? The paper flaked into pieces like the wings of moths when I tried to turn the page.By the time Jeremiah Breen took possession of the house, bridge had fallen out of fashion. At the time the table was carved, this part of the Bronx was marsh. When I input our zip code into the online archive of the U.S. Geological Survey, I can see on a century-old map what this wetland looked like before it was developed into the grid of streets, shops, houses, schools, and apartment buildings that make up the neighborhood now. In 1900, the land is still veined by blue streams. A pin in the shape of a teardrop marks the spot of our present address, smack-dab in a bend of a waterway called Tibbetts Brook. The brook was named after a settler whose descendants were driven off the land for their royalist sympathies during the Revolutionary War. Before that, it had another name. The Munsee Lenape called it Mosholu. We live on the ghost of this rivulet, just one of the city’s dozens of lost streams.[Hannah Ritchie: A slightly hotter world could still be a better one]The teardrop confirmed what I sensed about the true nature of my pond, which was so much more than a puddle, and not mine at all, but rather a part of a much larger body of water.Waterways like Tibbetts Brook were once the lifeblood of the city. As New York grew, in the 17th and 18th centuries, into the world’s supreme port, it counted on such freshwater streams for transportation, drinking water, fishing, and waterpower for grain mills and sawmills. The brook became polluted; eventually, railroad lines overtook waterways as transportation routes. Waterpower was replaced by steam. Steam was replaced by electric power. The banks of the streams became industrial wastelands, which became Black and brown neighborhoods. Plundered water bodies. Plundered peoples.The works of Eric Sanderson, a landscape ecologist, and Herbert Kraft, a scholar of the Lenape, help me imagine a preindustrial, pre-European version of my home place. The Wiechquaeseck community of Lenape lived in a settlement nearby, around Spuytin Duyvil Creek, fed by the waters of Mosholu. They lived mostly out of doors and owned no more than they could carry. Wealth was being in communion with one another, and in balance with the abundant natural world, “filled with an almost infinite variety of plants, animals, insects, clouds and stones, each of which possessed spirits no less important than those of human beings,” according to Kraft.All I have to do to see a remaining pocket of that natural world that was once my home is walk three blocks east to Van Cortlandt Park, where a narrow belt of lowland swamp forest still survives along a trail around open water. This small freshwater wetland is ecologically precious, home to many plant and animal species. It slows erosion, prevents flooding by retaining stormwater, filters and decomposes pollutants, and converts carbon dioxide into oxygen.Hunting the swamp are barred owls and red-tailed hawks. Water lilies, swamp loosestrife, and arrowhead each grow at different water depths, thickening the open water by midsummer. Mallards and wood ducks feed, nest, preen, and glide among dense strands of cattail, buttonbush, arrow arum, and blue flag. Eastern kingbirds and belted kingfishers screech from the treetops while painted turtles sun themselves on the lodges of muskrats. These, too, are my neighbors.The Van Cortlandt Swamp is fed by Tibbetts Brook, before the brook divides down into the concrete conduit, its tail buried. This little swamp is a patch of the 2,000 acres of freshwater wetland remaining in the city today, out of the 224,000 acres it boasted 200 years ago.“All water has a perfect memory and is forever trying to get back where it was,” Toni Morrison once wrote. From that point of view, the pond in front of our house is not a nuisance but rather the brook remembering itself. Mosholu. How might Thoreau have described my pond? The pond is a gift to the birds who stop there to bathe, and a place for wildlife to slake their thirst at night: possum, coyote, skunk. The pond is a lieu de mémoire, a reservoir. When the sun hits it at the right angle, the pond’s surface dances with jewels of light. When night comes, the pond throws back the orange glow of the streetlight. The pond is the paved-over wetland, reasserting its form.The Lenape believed that everything in nature has a spirit, and should be given thanks, and asked permission before taking from it. I doubt Jacobus Van Cortlandt, landowner, enslaver, and mayor of New York, asked permission when he had the Black people he owned dam up Tibbetts Brook in 1699 to install a sawmill and gristmill on his plantation. Some of the skeletons of those he enslaved were unearthed by construction workers laying down railroad tracks in the 1870s. The mill operated until 1889, when the city purchased the land for its park. At that point, the millpond became a small, decorative lake. Sometimes I walk to this lake, next to the African burial ground, to watch the damselflies and contemplate what lies beneath.At the lake’s south end, in 1912, the brook was piped into a storm drain and rechanneled into an underground tunnel that merged into a brick sewer below Broadway. This enabled the construction of streets and buildings south of the park, including our house, on top of backfill and city trash. What does it mean to live in a place where rivers are harnessed to carry our waste away, so we don’t have to think about it?According to the Department of Environmental Protection, 4 million to 5 million gallons of water flow into the Broadway sewer on a dry day from Tibbetts Brook and the millpond alone. That water runs through the sewer, where it mixes with raw household sewage, and then on to Wards Island Wastewater Treatment Plant. But when it rains, the amount of water can be five times that. At least 60 times a year, the treatment plant gets overwhelmed by rainwater and shuts down. Untreated sewage and rainwater are then discharged into the Harlem River, in violation of federal law.Now there are plans to “daylight” the subterranean stretch of Tibbetts Brook, bringing it back to the surface. This restoration will alleviate flooding by rerouting the buried section of the brook directly into the Harlem River, not exactly along its historic route, upon which our house sits. Instead, it will flow slightly to the east, along an old railway line that accidentally reverted to an urban wetland after the freight trains stopped running in the 1980s. This gully runs behind BJ’s Wholesale Club and the strip mall with the nail salon and the Flame hibachi and the Staples—already rewilding with tall marsh grasses and reeds.There is talk of undoing the past, of giving some of what was taken from nature back to nature. There is talk of a bike path along a greenway costing millions of dollars. If the project comes to pass by 2030 as planned, it will be New York City’s first daylighting story, and we will be in the watershed. Unburying the brook seems like a good thing. I hope, when it beautifies the landscape, that my neighbors can still afford to live here.We were still living out of boxes in early September 2021 when the National Weather Service declared New York City’s first flash-flood emergency. Our boys were by then 8 and 10. More than three inches of rain fell in just one hour, shattering a record set by a storm the week before. Was it even correct to call it a 500-year rainfall event when the past had become such a poor guide to the present? The remnants of Hurricane Ida turned the nearby Major Deegan Expressway back into a river, stranding cars, buses, and trucks in high water. That image, from our new neighborhood, became an international symbol of the city’s unpreparedness. Every single subway line in the city was stalled. A thousand straphangers were evacuated from 17 stuck trains. “We are BEYOND not ready for climate change,” a city-council member declared on Twitter.The pond in front of our house was whipped into waves by the wind. It was as sure a sign as any that we were living on borrowed time. But in the weeks that followed Ida, against our better judgment, we had Con Edison connect us to the gas line under the kettle in the street where the water gathers. We’d have preferred to heat the house with geothermal energy, but couldn’t find anybody yet trained to install it. At times, the house feels like a snare. I mean to say, if I remain embarrassed as a homeowner, it is not on account of the pond.Just as remarkable as the pond out front is the garden out back. Down on my knees with my hands in the soil, I weed and tend the beds. My mother has given me a Lenten rose. It is the first thing to bloom in spring. I marvel at the shoots coming up from the bulbs planted before me by Mary, wife of Jeremiah, whose name was not on the deed but was told to me by our neighbor Eve. Daffodils, peonies, hyacinths, and tulips.I live in Lenapehoking, the unceded territory of the Lenape people, past and present. Generations before we bought this land, it was stolen. I believe we have a responsibility to honor them by becoming better stewards of the land we inhabit. I want these words to be more than words; I want them to be deeds.I’m learning to grow food for our table, sensing that the truest sacrament is eating the earth’s body. I have planted lettuce, tomatoes, sweet peas, and beets. I collect water in a barrel under the gutter spout. I see that our land is a quilt; that our house is only a structure among structures among pollinating plants visited by bees.The pond is part of the place where we live. To prevent stagnation, I sometimes stir it with a stick. Through the front windows, I watch it swell when it rains. I observe the birds who stop there to bathe: warblers, tanagers, grosbeaks, sparrows. Some of them are endangered. A small reparation: I am teaching our children their names.This essay has been adapted from Emily Raboteau’s forthcoming book, Lessons for Survival: Mothering Against “The Apocalypse.”

Would the house be around to bequeath to our children, or would it be underwater?

I can’t talk about our house in the Bronx without telling you first about the pond out front. Given how much worse flooding can be elsewhere in New York City—even just two blocks to the east along the valley of Broadway, where the sewer is always at capacity—not to mention elsewhere in the world, I’m embarrassed to gripe about my personal pond. These days, such bodies of water are everywhere. Mine is not the only pond, but merely the pond I can’t avoid.

The pond dilates and contracts according to water levels. After a string of dry days, it may shrink to a puddle. After a storm, it may stretch to the length of a freight car, spilling into the middle of the street. It’s bad for curb appeal. Its sources are environmental, structural, and complex. On the rare occasion the pond dissipates, it leaves behind a residue like black mayonnaise.

The pond is almost always there. Our region is getting wetter as the climate changes. More rain, more storms, more often. The infrastructure of our city, at the edge of the rising sea, isn’t fit to handle so much water. Sudden, torrential downpours overwhelm our outdated drainage systems, especially at high tide; drench the subway system; and, in some low-lying places nearby, turn streets into sewers and basements into death traps.

In summer, the pond breeds mosquitoes and collects litter: cigarette butts, scratched-off lotto tickets. In winter, I worry the pond will become a slipping hazard. This is what I say when dialing 311, the city’s helpline, in hopes of remediation. An elderly neighbor could slip on the ice and break a bone. The pond could collapse into a sinkhole.

Tell it to the DOT, lady, says the Department of Environmental Protection. I do. Nope, says the Department of Transportation; because of the tree, this is a problem for Parks. I follow up. Weeks pass. The Department of Parks and Recreation directs me to the Department of Health. Months pass. What you need to do for ponding, says the DOH, is try the DEP. I write to my city-council member: I’m being given the runaround. Weeks pass without reply. Surely, this wouldn’t happen in the rich neighborhood up the hill. As a city worker myself, I know this dance well—this absurd, disjointed roundelay.

[Olga Khazan: Why can’t I just rent a house? ]

I ruminate over the pond. It has caused me not just embarrassment but shame. It has turned me scientific, made me into a water witch. I understand that the pond is beyond the scope of any one person, or any one agency, to handle, and that it’s perilous to ignore. The pond is a dark mirror; in it, our house appears upside down, distorted. It reflects deeper problems of stewardship and governance and the position of our house in relation to both. We are privileged to own a home. Yet we live on land that will drown, that is inundated already. The pond is a portal. Sometimes it smells, this vent hole of the netherworld. Beneath its surface, something lies concealed. Given the fact of the pond, why did we buy the house? Now that we dwell in the house, what to do about the pond?

Technically, the pond isn’t on our property at all. Our home inspector had no reason to suspect it. It belongs to the city, along with the street where it spreads. This is what we were told on the rainy day we arrived for the final walk-through before closing on the house in the deadly spring of 2020: The pond was up to the city to fix, with taxpayer dollars.

Plenty of folks were deserting New York then. I mean hundreds of thousands. That we were committed to staying in the city was both an act of necessity and a point of pride. For my husband and I, the house was a step up from the crowded three-room apartment in Washington Heights where we’d sheltered in place, away from the mad snarl of highways whose traffic had given our boys asthma: a place to stretch out, a sign of our upward mobility. The American dream. To a Black family without generational wealth, some of whose ancestors were property themselves, it signified even more: Shelter. Safety. Equity. Arrival. A future for our children.

We fell in love with the house as soon as we saw it, a run-down detached brick home in a working-class neighborhood with a little garden in back and windows on all four sides. The house had solid bones. We rejoiced when our offer was accepted. Yet until the day of the final walk-through, we had never visited the house in the rain.

That morning, the pond greeted us like the opposite of a welcome mat, giving shape to whatever latent misgivings we had about making this move. I felt hoodwinked. Buyer beware! I waded into the middle of that bad omen to gauge its depth. Murky water sloshed over the tops of my rain boots, drenching my socks. Good Lord. It was so much more significant than a puddle. I wondered what it was, how to name it, and why it was here. Was what I stood on actually land, or something less concrete? Could it have been a wetland, once? Why hadn’t the pond been disclosed? Because it didn’t have to be, said the tight-lipped seller’s agent representing the estate of the previous owner, an old man named Jeremiah Breen.

That night, my husband and I lay awake in bed, discussing our options. Sirens sounded up from the street. People were dying of COVID all around us. Purportedly, the house sat outside the floodplain. But what if the pond got bigger with worsening weather? Would it pour into the basement? Was the house’s foundation as solid as we’d been told? We doubted that the city would handle the underlying issues—not while hobbled by the pandemic. Would flood insurance be enough? Would the house be around to bequeath to our children, or would it be underwater? Was it an asset or a millstone? How high would the waters rise? How soon? Did we even believe, deep down in our souls, of ownership of this kind? Why fake like we or anyone else could own the land?

Such questions of capital consumed us deep into the night. The bottom line was this: If we pulled out of the deal, we’d lose our down payment, amounting to two years of college tuition for one of our kids. By dawn, we admitted our disillusionment. We’d already crossed the Rubicon, imbricated in the twisted system that brought about the pond. Or so we said because nevertheless, we still loved the house.

We renegotiated the purchase price; we moved in.


Later, I learned that many current maps for flood risk overlap with maps of historic housing discrimination. Geography determines a neighborhood’s risk and, this being America, so does race. Neighborhoods that suffered from redlining in the 1930s—when our house was built—face a far higher risk of flooding today. The pond suggested a submerged history beneath the daily surface of things.

The house was not just a risk but a wreck. Its rusty tanks sweated out oil that looked like blood onto the basement floor. Most of its windowpanes were cracked; its floors, uneven; its doors, out of plumb. It lacked adequate insulation. Under the creaky old planks, we discovered a newspaper dating back to the Depression. The front page addressed the use of antiques in home decoration. It featured a photo of a card room with an 18th-century Queen Anne table being used for bridge. How far back could I imagine? The paper flaked into pieces like the wings of moths when I tried to turn the page.

By the time Jeremiah Breen took possession of the house, bridge had fallen out of fashion. At the time the table was carved, this part of the Bronx was marsh. When I input our zip code into the online archive of the U.S. Geological Survey, I can see on a century-old map what this wetland looked like before it was developed into the grid of streets, shops, houses, schools, and apartment buildings that make up the neighborhood now. In 1900, the land is still veined by blue streams. A pin in the shape of a teardrop marks the spot of our present address, smack-dab in a bend of a waterway called Tibbetts Brook. The brook was named after a settler whose descendants were driven off the land for their royalist sympathies during the Revolutionary War. Before that, it had another name. The Munsee Lenape called it Mosholu. We live on the ghost of this rivulet, just one of the city’s dozens of lost streams.

[Hannah Ritchie: A slightly hotter world could still be a better one]

The teardrop confirmed what I sensed about the true nature of my pond, which was so much more than a puddle, and not mine at all, but rather a part of a much larger body of water.

Waterways like Tibbetts Brook were once the lifeblood of the city. As New York grew, in the 17th and 18th centuries, into the world’s supreme port, it counted on such freshwater streams for transportation, drinking water, fishing, and waterpower for grain mills and sawmills. The brook became polluted; eventually, railroad lines overtook waterways as transportation routes. Waterpower was replaced by steam. Steam was replaced by electric power. The banks of the streams became industrial wastelands, which became Black and brown neighborhoods. Plundered water bodies. Plundered peoples.

The works of Eric Sanderson, a landscape ecologist, and Herbert Kraft, a scholar of the Lenape, help me imagine a preindustrial, pre-European version of my home place. The Wiechquaeseck community of Lenape lived in a settlement nearby, around Spuytin Duyvil Creek, fed by the waters of Mosholu. They lived mostly out of doors and owned no more than they could carry. Wealth was being in communion with one another, and in balance with the abundant natural world, “filled with an almost infinite variety of plants, animals, insects, clouds and stones, each of which possessed spirits no less important than those of human beings,” according to Kraft.

All I have to do to see a remaining pocket of that natural world that was once my home is walk three blocks east to Van Cortlandt Park, where a narrow belt of lowland swamp forest still survives along a trail around open water. This small freshwater wetland is ecologically precious, home to many plant and animal species. It slows erosion, prevents flooding by retaining stormwater, filters and decomposes pollutants, and converts carbon dioxide into oxygen.

Hunting the swamp are barred owls and red-tailed hawks. Water lilies, swamp loosestrife, and arrowhead each grow at different water depths, thickening the open water by midsummer. Mallards and wood ducks feed, nest, preen, and glide among dense strands of cattail, buttonbush, arrow arum, and blue flag. Eastern kingbirds and belted kingfishers screech from the treetops while painted turtles sun themselves on the lodges of muskrats. These, too, are my neighbors.

The Van Cortlandt Swamp is fed by Tibbetts Brook, before the brook divides down into the concrete conduit, its tail buried. This little swamp is a patch of the 2,000 acres of freshwater wetland remaining in the city today, out of the 224,000 acres it boasted 200 years ago.

“All water has a perfect memory and is forever trying to get back where it was,” Toni Morrison once wrote. From that point of view, the pond in front of our house is not a nuisance but rather the brook remembering itself. Mosholu. How might Thoreau have described my pond? The pond is a gift to the birds who stop there to bathe, and a place for wildlife to slake their thirst at night: possum, coyote, skunk. The pond is a lieu de mémoire, a reservoir. When the sun hits it at the right angle, the pond’s surface dances with jewels of light. When night comes, the pond throws back the orange glow of the streetlight. The pond is the paved-over wetland, reasserting its form.

The Lenape believed that everything in nature has a spirit, and should be given thanks, and asked permission before taking from it. I doubt Jacobus Van Cortlandt, landowner, enslaver, and mayor of New York, asked permission when he had the Black people he owned dam up Tibbetts Brook in 1699 to install a sawmill and gristmill on his plantation. Some of the skeletons of those he enslaved were unearthed by construction workers laying down railroad tracks in the 1870s. The mill operated until 1889, when the city purchased the land for its park. At that point, the millpond became a small, decorative lake. Sometimes I walk to this lake, next to the African burial ground, to watch the damselflies and contemplate what lies beneath.

At the lake’s south end, in 1912, the brook was piped into a storm drain and rechanneled into an underground tunnel that merged into a brick sewer below Broadway. This enabled the construction of streets and buildings south of the park, including our house, on top of backfill and city trash. What does it mean to live in a place where rivers are harnessed to carry our waste away, so we don’t have to think about it?

According to the Department of Environmental Protection, 4 million to 5 million gallons of water flow into the Broadway sewer on a dry day from Tibbetts Brook and the millpond alone. That water runs through the sewer, where it mixes with raw household sewage, and then on to Wards Island Wastewater Treatment Plant. But when it rains, the amount of water can be five times that. At least 60 times a year, the treatment plant gets overwhelmed by rainwater and shuts down. Untreated sewage and rainwater are then discharged into the Harlem River, in violation of federal law.

Now there are plans to “daylight” the subterranean stretch of Tibbetts Brook, bringing it back to the surface. This restoration will alleviate flooding by rerouting the buried section of the brook directly into the Harlem River, not exactly along its historic route, upon which our house sits. Instead, it will flow slightly to the east, along an old railway line that accidentally reverted to an urban wetland after the freight trains stopped running in the 1980s. This gully runs behind BJ’s Wholesale Club and the strip mall with the nail salon and the Flame hibachi and the Staples—already rewilding with tall marsh grasses and reeds.

There is talk of undoing the past, of giving some of what was taken from nature back to nature. There is talk of a bike path along a greenway costing millions of dollars. If the project comes to pass by 2030 as planned, it will be New York City’s first daylighting story, and we will be in the watershed. Unburying the brook seems like a good thing. I hope, when it beautifies the landscape, that my neighbors can still afford to live here.


We were still living out of boxes in early September 2021 when the National Weather Service declared New York City’s first flash-flood emergency. Our boys were by then 8 and 10. More than three inches of rain fell in just one hour, shattering a record set by a storm the week before. Was it even correct to call it a 500-year rainfall event when the past had become such a poor guide to the present? The remnants of Hurricane Ida turned the nearby Major Deegan Expressway back into a river, stranding cars, buses, and trucks in high water. That image, from our new neighborhood, became an international symbol of the city’s unpreparedness. Every single subway line in the city was stalled. A thousand straphangers were evacuated from 17 stuck trains. “We are BEYOND not ready for climate change,” a city-council member declared on Twitter.

The pond in front of our house was whipped into waves by the wind. It was as sure a sign as any that we were living on borrowed time. But in the weeks that followed Ida, against our better judgment, we had Con Edison connect us to the gas line under the kettle in the street where the water gathers. We’d have preferred to heat the house with geothermal energy, but couldn’t find anybody yet trained to install it. At times, the house feels like a snare. I mean to say, if I remain embarrassed as a homeowner, it is not on account of the pond.

Just as remarkable as the pond out front is the garden out back. Down on my knees with my hands in the soil, I weed and tend the beds. My mother has given me a Lenten rose. It is the first thing to bloom in spring. I marvel at the shoots coming up from the bulbs planted before me by Mary, wife of Jeremiah, whose name was not on the deed but was told to me by our neighbor Eve. Daffodils, peonies, hyacinths, and tulips.

I live in Lenapehoking, the unceded territory of the Lenape people, past and present. Generations before we bought this land, it was stolen. I believe we have a responsibility to honor them by becoming better stewards of the land we inhabit. I want these words to be more than words; I want them to be deeds.

I’m learning to grow food for our table, sensing that the truest sacrament is eating the earth’s body. I have planted lettuce, tomatoes, sweet peas, and beets. I collect water in a barrel under the gutter spout. I see that our land is a quilt; that our house is only a structure among structures among pollinating plants visited by bees.

The pond is part of the place where we live. To prevent stagnation, I sometimes stir it with a stick. Through the front windows, I watch it swell when it rains. I observe the birds who stop there to bathe: warblers, tanagers, grosbeaks, sparrows. Some of them are endangered. A small reparation: I am teaching our children their names.

This essay has been adapted from Emily Raboteau’s forthcoming book, Lessons for Survival: Mothering Against “The Apocalypse.”

Read the full story here.
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Toxic Pfas above proposed safety limits in almost all English waters tested

Exclusive: 110 of 117 bodies of water tested by Environment Agency would fail standards, with levels in fish 322 times the planned limitNearly all rivers, lakes and ponds in England tested for a range of Pfas, known as “forever chemicals”, exceed proposed new safety limits and 85% contain levels at least five times higher, analysis of official data reveals.Out of 117 water bodies tested by the Environment Agency for multiple types of Pfas, 110 would fail the safety standard, according to analysis by Wildlife and Countryside Link and the Rivers Trust. Continue reading...

Nearly all rivers, lakes and ponds in England tested for a range of Pfas, known as “forever chemicals”, exceed proposed new safety limits and 85% contain levels at least five times higher, analysis of official data reveals.Out of 117 water bodies tested by the Environment Agency for multiple types of Pfas, 110 would fail the safety standard, according to analysis by Wildlife and Countryside Link and the Rivers Trust.They also found levels of Pfos – a banned carcinogenic Pfas – in fish were on average 322 times higher than planned limits for wildlife. If just one portion of such freshwater fish was eaten each month this would exceed the safe threshold of Pfos for people to consume over a year, according to the NGOs.Pfas, or per- and polyfluoroalkyl substances, are a group of thousands of human-made chemicals used in industrial processes and products such as non-stick pans, clothing and firefighting foams. They do not break down in the environment and some are linked to diseases, including cancers and hormone disruption.Pfas pollution is widespread, prompting the EU to propose a new water quality standard that limits the combined toxicity of 24 Pfas to 4.4 nanograms per litre of water, calculated as PFOA-equivalents – a method that weights each substance according to its toxicity relative to PFOA, a particularly hazardous and well-studied carcinogen that is now banned.The EU is also planning to regulate about 10,000 Pfas as one class as there are too many to assess on a case-by-case basis and because none break down in the environment, but the UK has no plans to follow suit.Last week, environment groups, led by the Marine Conservation Society, wrote to ministers, urging a ban on all Pfas in consumer products and a timeline for phasing them out in all other uses. Now, public health and nature groups have joined forces to propose urgent measures to rein in pollution.“Scientists continue to identify Pfas as one of the biggest threats of our time, yet the UK is falling behind other countries in restricting them,” said Hannah Evans of the environmental charity Fidra. “Every day of inaction locks in decades of pollution and environmental harm … we’re asking the UK government to turn off the tap of these persistent forever chemicals.”They say the UK should align with the EU’s group-based Pfas restrictions and ban the substances in food packaging, clothing, cosmetics, toys and firefighting foams, following examples from Denmark, France and the EU. They want better monitoring, tougher water and soil standards and to make polluters cover the cost of Pfas clean-up.Emma Adler, the director of impact at Wildlife and Countryside Link, said: “Pfas are linked to an explosion of impacts for wildlife and public health, from cancers to immune issues. These new figures underline just how widespread Pfas pollution is and that Pfas regulation must be a much clearer priority in government missions to clean up UK rivers and improve the nation’s health.”Thalie Martini, the chief executive officer at Breast Cancer UK, said: “Evidence points to the potential for some Pfas to be related to health issues, including increasing breast cancer risk … millions of families affected by this disease will want the government to do everything they can to deliver tougher Pfas rules to protect our health.”Last year, 59 Pfas experts urged the government to follow the science and regulate all Pfas as a single class, warning their extreme persistence – regardless of toxicity – posed a serious environmental threat.skip past newsletter promotionThe planet's most important stories. Get all the week's environment news - the good, the bad and the essentialPrivacy Notice: Newsletters may contain info about charities, online ads, and content funded by outside parties. For more information see our Privacy Policy. We use Google reCaptcha to protect our website and the Google Privacy Policy and Terms of Service apply.after newsletter promotion“Countries like France and Denmark, the EU as a whole and many US states have taken strong action against Pfas pollution,” said Dr Francesca Ginley from the Marine Conservation Society. “The time is now for the UK to take a stand and show the leadership we need on Pfas pollution from source to sea.”Dr Shubhi Sharma of the charity Chem Trust said: “Too often with hazardous chemicals the world has ignored early warnings of harm and learned lessons far too late. Costs to tackle Pfas in the environment and address health impacts have a multi-billion pound economic price tag … the government must not delay.”An Environment Agency spokesperson said the science on Pfas was moving quickly and that it was running a multi-year programme to improve understanding of Pfas pollution sources in England. They added: “We are screening sites to identify potential sources of Pfas pollution and prioritise further investigations, whilst assessing how additional control measures could reduce the risks of Pfas in the environment.”A spokesperson for the Department for Environment, Food and Rural Affairs said: “The government is committed to protecting human health and the environment from the risks posed by Pfas. That’s why we are working at pace together with regulators to assess levels of Pfas in the environment, their sources and potential risks to inform our approach to policy and regulation.”

Breaking Down the Force of Water in the Texas Floods

Flash floods last week in Texas caused the Guadalupe River to rise dramatically, reaching three stories high in just two hours

Over just two hours, the Guadalupe River at Comfort, Texas, rose from hip-height to three stories tall, sending water weighing as much as the Empire State building downstream roughly every minute it remained at its crest.Comfort offers a good lens to consider the terrible force of a flash flood’s wall of water because it’s downstream of where the river’s rain-engorged branches met. The crest was among the highest ever recorded at the spot — flash flooding that appears so fast it can “warp our brains,” said James Doss-Gollin, assistant professor of civil and environmental engineering at Rice University.The Texas flood smashed through buildings, carried away cars and ripped sturdy trees out by the roots, dropping the debris in twisted piles when the water finally ebbed. It killed more than 100 people, prompted scores of rescues and left dozens of others missing. The deaths were concentrated upriver in Kerr County, an area that includes Camp Mystic, the devastated girls' camp, where the water hit early and with little notice.Water is capable of such destruction because it is heavy and can move fast. Just one cubic foot of water — imagine a box a bit larger than the size of a basketball — weighs about 62 pounds (28 kilograms). When the river rose to its peak at Comfort, 177,000 cubic feet — or 11 million pounds (5 million kilograms) of water — flowed by every second.“When you have that little lead time ... that means you can’t wait until the water level starts to rise,” Doss-Gollin said. “You need to take proactive measures to get people to safety.” Water as heavy as a jumbo jet A small amount of water — less than many might think — can sweep away people, cars and homes. Six inches (15.2 centimeters) is enough to knock people off their feet. A couple of feet of fast-moving water can take away an SUV or truck, and even less can move cars.“Suppose you are in a normal car, a normal sedan, and a semitrailer comes and pushes you at the back of the car. That’s the kind of force you’re talking about,” said Venkataraman Lakshmi, a University of Virginia professor and president of the hydrology section of the American Geophysical Union.And at Comfort, it took just over 15 minutes for so much water to arrive that not only could it float away a large pickup truck, but structures were in danger — water as heavy as a jumbo jet moved by every second.At that point, “We are past vehicles, homes and things can start being affected,” said Daniel Henz, flood warning program manager at the flood control district of Maricopa County, Arizona, an area that gets dangerous scary flash floods.The water not only pushes objects but floats them, and that can actually be scarier. The feeling of being pushed is felt immediately, letting a person know they are in danger. Upward force may not be felt until it is overwhelming, according to Upmanu Lall, a water expert at Arizona State University and Columbia University.“The buoyancy happens — it’s like a yes, no situation. If the water reaches a certain depth and it has some velocity, you’re going to get knocked off (your feet) and floating simultaneously,” he said. The mechanics of a flash flood The landscape created the conditions for what some witnesses described as a fast-moving wall of water. Lots of limestone covered by a thin layer of soil in hilly country meant that when rain fell, it ran quickly downhill with little of it absorbed by the ground, according to S. Jeffress Williams, senior scientist emeritus with the U.S. Geological Survey.A flash flood generally starts with an initial lead wave and then builds as rain rushes over the landscape and into the river basin. It may rise quickly, but the water still takes some time to converge. The water crumpled cars into piles, twisted steel and knocked trees down as if they were strands of grass. Images captured the chaos and randomness of the water’s violence.And then, not as fast as it rose, but still quickly, the river receded.Five hours after its crest at Comfort, it had already dropped 10 feet (3 meters), revealing its damage in retreat. A couple of days after it started to rise, a person could stand with their head above the river again.“Everything just can happen, very, very quickly,” Henz said.Associated Press writer Seth Borenstein in Washington contributed.The Associated Press receives support from the Walton Family Foundation for coverage of water and environmental policy. The AP is solely responsible for all content. For all of AP’s environmental coverage, visit https://apnews.com/hub/climate-and-environmentCopyright 2025 The Associated Press. All rights reserved. This material may not be published, broadcast, rewritten or redistributed.Photos You Should See - June 2025

South West Water allowed to invest £24m rather than pay £19m fine

Campaigners say Ofwat ‘subservient to industry and its rampaging pursuit of profit’ after illegal sewage dischargesSouth West Water has agreed to pay a £24m penalty for illegal sewage discharges into the environment from its treatment works.The regulator for the water and wastewater sector in England and Wales, Ofwat, says the company, which has 1.8 million customers in Cornwall, Devon, the Isles of Scilly and parts of Dorset and Somerset, is being penalised for dumping sewage in breach of its legal permit conditions. Continue reading...

South West Water has agreed to pay a £24m penalty for illegal sewage discharges into the environment from its treatment works.The regulator for the water and wastewater sector in England and Wales, Ofwat, says the company, which has 1.8 million customers in Cornwall, Devon, the Isles of Scilly and parts of Dorset and Somerset, is being sanctioned for dumping sewage in breach of its legal permit conditions.But there was anger over revelations on Thursday that the regulator had not imposed a direct fine on the company.South West Water put forward the suggestion that it would invest £20m to reduce sewage discharges at key storm overflows, spend £2m to tackle sewer misuse and misconnections, and another £2m to support local environment groups. This was accepted by Ofwat rather than imposing a fine of £19m.But Rob Abrams, the campaigns manager at Surfers Against Sewage, said allowing water companies to choose their own penalty was farcical.He said the situation “illustrates a water industry model that’s broken beyond repair, with government and regulators subservient to industry and its rampaging pursuit of profit, at any cost”.Ofwat said it had chosen this route rather than imposing a fine because it was satisfied that the company would carry out the work required to bring its infrastructure back into legal operation.“We have … concluded that it would be appropriate to accept the undertakings in lieu of the financial penalty we would otherwise impose in this case (£19m, 6.5% of its relevant turnover),” Ofwat said.The regulator carried out a two-year investigation into the company that found it had failed to upgrade its treatment works to prevent sewage discharges into the environment, failed to properly deal with the content of its sewers and failed to put in the resources to monitor its treatment works properly.The penalty is the latest in an ongoing investigation by Ofwat into several water companies into widespread illegal sewage dumping across the network from thousands of treatment plants.Penalties totalling more than £160m have already been imposed against Yorkshire Water, Thames Water and Northumbrian Water for widespread illegal sewage dumping from their treatment works.Lynn Parker, the senior director for enforcement at Ofwat, said the regulator had secured the £24m package and a commitment to put things right from the company.skip past newsletter promotionSign up to Business TodayGet set for the working day – we'll point you to all the business news and analysis you need every morningPrivacy Notice: Newsletters may contain info about charities, online ads, and content funded by outside parties. For more information see our Privacy Policy. We use Google reCaptcha to protect our website and the Google Privacy Policy and Terms of Service apply.after newsletter promotionBut Abrams said it amounted to a cynical PR exercise and an abdication of responsibility by Ofwat.“There is no transparency about how the money will be spent or whether it’s even enough,” he said.“Of the £4m pledged for environmental initiatives and local groups, we’ve been given no clarity on who will benefit or why.”The public and other stakeholders can make representations about the size of the penalty before it is finalised.

Oregon groundwater protection bill passes despite criticism that it’s too weak

Gov. Tina Kotek backed the bill to modernize Oregon’s failed groundwater pollution laws.

Legislators have just passed a groundwater protection bill that many nonprofit groups working on groundwater contamination said was too watered down to make a real difference. Gov. Tina Kotek backed the bill to modernize Oregon’s failed groundwater pollution laws. Kotek has been active in trying to speed up response to the three-decades-old groundwater contamination crisis in the Lower Umatilla Basin, where many residents with nitrate-contaminated domestic wells must rely on bottled drinking water. Until 2022, many people in the region had no idea they had been drinking contaminated water for years. Some still don’t know it because the state has yet to test all the affected wells. A state analysis also has shown that nitrate pollution in the area has worsened significantly over the past decade. Though the state has been testing wells and conducting public awareness campaigns, critics have accused the Oregon Department of Environmental Quality, Department of Agriculture and Water Resources Department of not doing enough to crack down on the pollution sources. Much of the nitrate contamination comes from fertilizer used by large farms, animal manure from local industrial dairies and feedlots and wastewater from food processing plants that are constantly applied to farm fields. Early versions of the bill laid out specific actions that state agencies would have to take once groundwater pollution had reached the level of a serious public health threat. But many of those actions were stripped out of the bill, leading environmental and social justice nonprofits to pull their support because they deemed the bill too weak to make a difference. Oregon Rural Action, the eastern Oregon nonprofit that has been instrumental in testing domestic wells and pushing the state to do more testing and to limit nitrate pollution, said industry groups representing polluters put pressure on the governor’s office, leading to major changes in the bill’s language. “The version passed on Friday no longer includes the tools, resources, and Legislative directives needed for agencies to exercise their authority to protect Oregon’s groundwater and enforce the law,”the group’s executive director, Kristin Anderson Ostrom, said in a statement. The governor’s office declined to comment.Kotek in January issued an emergency order allowing the Port of Morrow to again violate its water pollution permit and over-apply nitrogen contaminated water onto farmland. The port, which handles billions of gallons of nitrogen-rich water every year, said that it would have to pause operations and lay off workers if not for the emergency permit. In addition to the Lower Umatilla Basin, Oregon has designated two other areas – in northern Malheur County and the southern Willamette Valley – where elevated nitrate concentrations in groundwater pose a human health risk. Each one has an action plan to reduce nitrate concentrations in groundwater. Research has linked high nitrate consumption over long periods to stomach, bladder and intestinal cancers, miscarriages and thyroid issues. It is especially dangerous to infants who can quickly develop “blue baby syndrome,” a fatal illness.— Gosia Wozniacka covers environmental justice, climate change, the clean energy transition and other environmental issues. Reach her at gwozniacka@oregonian.com or 971-421-3154.

A rare glimpse inside the mountain tunnel that carries water to Southern California

In the 1930s, workers bored a 13-mile tunnel beneath Mt. San Jacinto. Here's a look inside the engineering feat that carries Colorado River water to Southern California.

Thousands of feet below the snowy summit of Mt. San Jacinto, a formidable feat of engineering and grit makes life as we know it in Southern California possible. The 13-mile-long San Jacinto Tunnel was bored through the mountain in the 1930s by a crew of about 1,200 men who worked day and night for six years, blasting rock and digging with machinery. Completed in 1939, the tunnel was a cornerstone in the construction of the 242-mile Colorado River Aqueduct. It enabled the delivery of as much as 1 billion gallons of water per day.The tunnel is usually off-limits when it is filled and coursing with a massive stream of Colorado River water. But recently, while it was shut down for annual maintenance, the Metropolitan Water District of Southern California opened the west end of the passage to give The Times and others a rare look inside. “It’s an engineering marvel,” said John Bednarski, an assistant general manager of MWD. “It’s pretty awe-inspiring.” The 16-foot-diameter San Jacinto Tunnel runs 13 miles through the mountain. While shut down for maintenance, the tunnel has a constant stream of water entering from the mountain. A group visits the west end of the San Jacinto Tunnel, where the mouth of the water tunnel enters a chamber. He wore a hard hat as he led a group to the gaping, horseshoe-shaped mouth of the tunnel. The passage’s concrete arch faded in the distance to pitch black.The tunnel wasn’t entirely empty. The sound of rushing water echoed from the walls as an ankle-deep stream flowed from the portal and cascaded into a churning pool beneath metal gates. Many in the tour group wore rubber boots as they stood on moist concrete in a chamber faintly lit by filtered sunlight, peering into the dark tunnel. This constant flow comes as groundwater seeps and gushes from springs that run through the heart of the mountain. In places deep in the tunnel, water shoots so forcefully from the floor or the wall that workers have affectionately named these soaking obstacles “the fire hose” and “the car wash.”Standing by the flowing stream, Bednarski called it “leakage water from the mountain itself.”Mt. San Jacinto rises 10,834 feet above sea level, making it the second-highest peak in Southern California after 11,503-foot Mt. San Gorgonio.As the tunnel passes beneath San Jacinto’s flank, as much as 2,500 feet of solid rock lies overhead, pierced only by two vertical ventilation shafts. Snow covers Mt. San Jacinto, as seen from Whitewater, in March. At the base of the mountain, the 13-mile San Jacinto Tunnel starts its journey. The tunnel transports Colorado River water to Southern California’s cities. During maintenance, workers roll through on a tractor equipped with a frame bearing metal bristles that scrape the tunnel walls, cleaning off algae and any growth of invasive mussels. Workers also inspect the tunnel by passing through on an open trailer, scanning for any cracks that require repairs.“It’s like a Disneyland ride,” said Bryan Raymond, an MWD conveyance team manager. “You’re sitting on this trailer, and there’s a bunch of other people on it too, and you’re just cruising through looking at the walls.” Aside from the spraying and trickling water, employee Michael Volpone said he has also heard faint creaking.“If you sit still and listen, you can kind of hear the earth move,” he said. “It’s a little eerie.”Standing at the mouth of the tunnel, the constant babble of cascading water dominates the senses. The air is moist but not musty. Put a hand to the clear flowing water, and it feels warm enough for a swim. On the concrete walls are stained lines that extend into the darkness, marking where the water often reaches when the aqueduct is running full. Many who have worked on the aqueduct say they are impressed by the system’s design and how engineers and workers built such a monumental system with the basic tools and technology available during the Great Depression.Pipelines and tunnelsThe search for a route to bring Colorado River water across the desert to Los Angeles began with the signing of a 1922 agreement that divided water among seven states. After the passage of a $2-million bond measure by Los Angeles voters in 1925, hundreds of surveyors fanned out across the largely roadless Mojave and Sonoran deserts to take measurements and study potential routes.The surveyors traveled mostly on horseback and on foot as they mapped the rugged terrain, enduring grueling days in desert camps where the heat sometimes topped 120 degrees.Planners studied and debated more than 100 potential paths before settling on one in 1931. The route began near Parker, Ariz., and took a curving path through desert valleys, around obstacles and, where there was no better option, through mountains.In one official report, a manager wrote that “to bore straight through the mountains is very expensive and to pump over them is likewise costly.” He said the planners carefully weighed these factors as they decided on a solution that would deliver water at the lowest cost. VIDEO | 02:45 A visit to the giant tunnel that brings Colorado River water to Southern California Share via Those in charge of the Metropolitan Water District, which had been created in 1928 to lead the effort, were focused on delivering water to 13 participating cities, including Los Angeles, Burbank and Anaheim. William Mulholland, Los Angeles’ chief water engineer, had led an early scouting party to map possible routes from the Colorado River to Southern California’s cities in 1923, a decade after he celebrated the completion of the 233-mile aqueduct from the Owens Valley to Los Angeles with the triumphant words, “There it is. Take it.”The aqueduct’s design matched the audaciousness of the giant dams the federal government was starting to build along the Colorado — Hoover Dam (originally called Boulder Dam) and Parker Dam, which formed the reservoir where the aqueduct would begin its journey.Five pumping plants would be built to lift water more than 1,600 feet along the route across the desert. Between those points, water would run by gravity through open canals, buried pipelines and 29 separate tunnels stretching 92 miles — the longest of which was a series of nine tunnels running 33.7 miles through hills bordering the Coachella Valley.To make it possible, voters in the district’s 13 cities overwhelmingly approved a $220-million bond in 1931, the equivalent of a $4.5-billion investment today, which enabled the hiring of 35,000 workers. Crews set up camps, excavated canals and began to blast open shafts through the desert’s rocky spines to make way for water.In 1933, workers started tearing into the San Jacinto Mountains at several locations, from the east and the west, as well as excavating shafts from above. Black-and-white photographs and films showed miners in hard hats and soiled uniforms as they stood smoking cigarettes, climbing into open rail cars and running machinery that scooped and loaded piles of rocks.Crews on another hulking piece of equipment, called a jumbo, used compressed-air drills to bore dozens of holes, which were packed with blasting power and detonated to pierce the rock. (Courtesy of Metropolitan Water District of Southern California) The work progressed slowly, growing complicated when the miners struck underground streams, which sent water gushing in.According to a 1991 history of the MWD titled “A Water Odyssey,” one flood in 1934 disabled two of three pumps that had been brought in to clear the tunnel. In another sudden flood, an engineer recalled that “the water came in with a big, mad rush and filled the shaft to the top. Miners scrambled up the 800-foot ladder to the surface, and the last man out made it with water swirling around his waist.”Death and delaysAccording to the MWD’s records, 13 workers died during the tunnel’s construction, including men who were struck by falling rocks, run over by equipment or electrocuted with a wire on one of the mining trolleys that rolled on railroad tracks. The Metropolitan Water District had originally hired Wenzel & Henoch Construction Co. to build the tunnel. But after less than two years, only about two miles of the tunnel had been excavated, and the contractor was fired by MWD general manager Frank Elwin “F.E.” Weymouth, who assigned the district’s engineers and workers to complete the project.Construction was delayed again in 1937 when workers went on strike for six weeks. But in 1939, the last wall of rock tumbled down, uniting the east and west tunnels, and the tunnel was finished. John Bednarski, assistant general manager of the Metropolitan Water District of Southern California, stands in a water tunnel near the end point of the larger San Jacinto Tunnel, which carries Colorado River water. The total cost was $23.5 million. But there also were other costs. As the construction work drained water, many nearby springs used by the Native Soboba people stopped flowing. The drying of springs and creeks left the tribe’s members without water and starved their farms, which led to decades of litigation by the Soboba Band of Luiseño Indians and eventually a legal settlement in 2008 that resolved the tribe’s water rights claims.The ‘magic touch’ of waterBy the time the tunnel was completed, the Metropolitan Water District had released a 20-minute film that was shown in movie theaters and schools celebrating its conquest of the Colorado River and the desert. It called Mt. San Jacinto the “tallest and most forbidding barrier.”In a rich baritone, the narrator declared Southern California “a new empire made possible by the magic touch of water.” “Water required to support this growth and wealth could not be obtained from the local rainfall in this land of sunshine,” the narrator said as the camera showed newly built homes and streets filled with cars and buses. “The people therefore realized that a new and dependable water supply must be provided, and this new water supply has been found on the lofty western slopes of the Rocky Mountains, a wonderland of beauty, clad by nature in a white mantle of snow.”Water began to flow through the aqueduct in 1939 as the pumping plants were tested. At the Julian Hinds Pumping Plant, near the aqueduct’s halfway point, water was lifted 441 feet, surging through three pipelines up a desert mountain. March 2012 image of the 10-foot-diameter delivery lines carrying water 441 feet uphill from the Julian Hinds Pumping Plant. (Los Angeles Times) From there, the water flowed by gravity, moving at 3-6 mph as it traveled through pipelines, siphons and tunnels. It entered the San Jacinto Tunnel in Cabazon, passed under the mountain and emerged near the city of San Jacinto, then continued in pipelines to Lake Mathews reservoir in Riverside County. In 1941, Colorado River water started flowing to Pasadena, Beverly Hills, Compton and other cities. Within six years, another pipeline was built to transport water from the aqueduct south to San Diego.The influx of water fueled Southern California’s rapid growth during and after World War II.Over decades, the dams and increased diversions also took an environmental toll, drying up much of the once-vast wetlands in Mexico’s Colorado River Delta. John Bednarski, assistant general manager of the Metropolitan Water District, walks in a water tunnel near the end point of the larger San Jacinto Tunnel. An impressive designToday, 19 million people depend on water delivered by the MWD, which also imports supplies from Northern California through the aqueducts and pipelines of the State Water Project.In recent decades, the agency has continued boring tunnels where needed to move water. A $1.2-billion, 44-mile-long conveyance system called the Inland Feeder, completed in 2009, involved boring eight miles of tunnels through the San Bernardino Mountains and another 7.9-mile tunnel under the Badlands in Riverside County.The system enabled the district to increase its capacity and store more water during wet years in Diamond Valley Lake, Southern California’s largest reservoir, which can hold about 260 billion gallons of water. “Sometimes tunneling is actually the most effective way to get from point A to point B,” said Deven Upadhyay, the MWD’s general manager.Speaking hypothetically, Upadhyay said, if engineers had another shot at designing and building the aqueduct now using modern technology, it’s hard to say if they would end up choosing the same route through Mt. San Jacinto or a different route around it. But the focus on minimizing cost might yield a similar route, he said.“Even to this day, it’s a pretty impressive design,” Upadhyay said.When people drive past on the I-10 in Cabazon, few realize that a key piece of infrastructure lies hidden where the desert meets the base of the mountain. At the tunnel’s exit point near San Jacinto, the only visible signs of the infrastructure are several concrete structures resembling bunkers. When the aqueduct is running, those who enter the facility will hear the rumble of rushing water. The tunnel’s west end was opened to a group of visitors in March, when the district’s managers held an event to name the tunnel in honor of Randy Record, who served on the MWD board for two decades and was chair from 2014 to 2018. Speaking to an audience, Upadhyay reflected on the struggles the region now faces as the Colorado River is sapped by drought and global warming, and he drew a parallel to the challenges the tunnel’s builders overcame in the 1930s. “They found a path,” Upadhyay said. “This incredible engineering feat. And it required strength, courage and really an innovative spirit.” “When we now think about the challenges that we face today, dealing with wild swings in climate and the potential reductions that we might face, sharing dwindling supplies on our river systems with the growing Southwest, it’s going to require the same thing — strength, courage and a spirit of innovation,” he said. A steep steel staircase gives access to a water tunnel near the end point of the larger San Jacinto Tunnel, which carries Colorado River water to Southern California.

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