Step off the trail above the last farm on Antisana and the ground gives. Cold water rises around your boot out of a tight green mat of plants that has been holding last week's fog. That is a Quito páramo: the wet grassland and cushion wetland above the treeline that catches rain and cloud, holds it in deep black soil, and lets it go slowly enough to keep a river running through the months when nothing falls. The water around your sole is on its way to a kitchen in Quitumbe.
Quito's páramos sit on four headwaters — Antisana, Cayambe-Coca above Papallacta, the Pita headwaters under Cotopaxi and Sincholagua, and the Pichincha–Atacazo slopes the city is built against. EPMAPS, the utility, says about 85% of the city's water starts in them; FONAG, the water fund, says closer to 90%. They are probably counting different things. Either way, most of the tap is grass first.
This is the third post in a place series — after what Quito depends on and who depends on it, this one stays on the living thing. The rule underneath is your water is not water. Here it is at four thousand meters.
the sponge is two things you can touch
A páramo holds water in its dark volcanic soil, and the grass and the bog are what keep that soil wet, shaded and in place. The grass — dense tussocks that slow runoff and shade the soil between rains. The cushion wetland — tight mats of plants over saturated peat that take in drizzle and fog and let it out over weeks. Together they turn a cold, wet climate into a steady river instead of a flash flood followed by a dry season. Burn, drain, plough, or trample either one and the rain still falls. It just leaves faster and arrives dirtier.
Quito drinks from four of these sponges.
| the sponge | the mountain | what it fills |
|---|---|---|
| Antisana páramo, under the glacier | Antisana | La Mica reservoir → El Troje plant → the south |
| Papallacta and Chalpi páramos | Cayambe-Coca, on the Amazon side of the divide | Salve Faccha, Mogotes, Sucus → Bellavista and Paluguillo plants → the north, the eastern valleys, the airport |
| Alto Pita páramo | Cotopaxi and Sincholagua | the Pita river → Puengasí plant → the centre and Los Chillos, with no reservoir behind it |
| Pichincha–Atacazo slopes | the volcano above the old city | the western conduits → the northwest |
The four systems do not connect, so every neighbourhood is downstream of exactly one sponge. Not "Quito's water." Your grass, on your mountain.
the ice above the grass
Antisana shows the stakes most plainly. Below the glacier, the páramo runs down to La Mica, the reservoir that since 2000 has sent 1,500 litres a second toward the south. By one modeled study, glacier melt is roughly a fifth of the streamflow at the Antisana intakes, and the ice is going: one measured tongue lost 15% of its area and retreated 235 metres between 1995 and 2012. Grass cannot replace ice: when the glacier gives less, there is less water. What the páramo below it can do is hold what still falls and let it go slowly, so the dry months hurt less — and that job gets more important as the ice shrinks.
what came back when the cattle left
For decades before the conservation area the páramo above La Mica was pasture. Cattle and sheep compacted the cushion wetlands, grazed the tussocks down, and left the soil open to burning. When FONAG and EPMAPS took the Antisana conservation area in hand — 7,121 hectares, plus 428 at Contadero — the livestock came off.
FONAG and The Nature Conservancy tell what happened next in order. Deer came back to the grass. Pumas followed the deer. And the Andean condor, down to a national count of 94 to 102 birds in the 2015 census, came back over Antisana. The recovery is unfinished — a juvenile was found dead in the park buffer in December 2025 — and one mountain's return is not yet a national trend. Take the cattle off the sponge and the sponge, and its neighbors, come back.
The bogs are being repaired on purpose as well. Pugllohuma, a cushion wetland on the Antisana side, was drained more than a hundred years ago by a hacienda that wanted pasture; since 2017 FONAG has been blocking those drains so the peat can rewet. That is how you rebuild a sponge. The counter-example is just as specific: in the Cinto catchment on the western side, about 7,000 hectares of páramo went to farming and pasture in thirteen years. Not a collapse — a steady trade of grass for fields until the catchment shrinks.
the bear corridor is the catchment
Between Antisana and Cayambe-Coca sits Paluguillo — land The Nature Conservancy gave to FONAG in April 2016 and, in December 2018, the first place in Ecuador declared an Área de Protección Hídrica. The Paluguillo plant takes its water there. So do sixteen Andean bears caught on camera trap, one of which — Iyali, collared on 25 November 2022 — became the first bear ever tracked inside the Distrito Metropolitano.
Nobody arranged that as a bonus. The bear corridor and the water catchment are the same hillside; protect one and you have protected the other. The airport at Tababela drinks from the Paluguillo plant and has already put money through FONAG toward that land — who else should is the fifth post's question. The point here is narrower: the living thing has names. A corridor, a bear, a plant, and Pifo and Tumbaco at the end of the pipe.
the people already on the grass
Someone walks this páramo every day. FONAG employs more than two dozen guardapáramos, hired from the communities that border the conservation areas, to watch for cattle, fire, and new fences, and to know the ground the way no model does. One of them, Lady Ulcuango, told The Nature Conservancy that Polylepis — the paper-barked tree that grows in patches above the grass — is "a sacred plant" with "great capacity to retain water." The communities are in it as well; San Francisco de Cruz Loma, on the Pichincha side, joined FONAG's work in 2017. So the páramo above Quito is not unattended. FONAG has kept cattle off it, blocked drains in it, and paid people to walk it since 2000, out of the city's water bill. How that fund works, and who besides the ratepayer pays into it, is post five. The line that matters here is shorter. The grass has stewards. The gap is not attention.
both ways up the mountain
The sponge has its own dependencies, none abstract. Cattle off the cushion wetlands. Fire out of the tussock. Cold — The Nature Conservancy warns that half of Latin America's páramos could be gone by 2050 as the treeline climbs. On the Papallacta side, no repeat of the 2003 oil spill into Laguna de Papallacta (post four).
Running the other way: about 2.7 million people depend on the four sponges. Roughly 400,000 in six southern parishes depend on Antisana alone, as they learned in July 2025 when the one pipe from La Mica broke — post four tells it. The airport depends on Paluguillo; the brewers and bottlers on basin water; the hydro plants on the páramo releasing slowly; the condors and bears on it as home. On the eastern side, the Kichwa Comuna Oyacachi holds title to páramos that feed Salve Faccha, and the utility has paid the comuna for that water since 2001 — the city paying its upstream neighbour, at a table the neighbour set. That is the map both ways.
nobody here funds "the andes"
"Protect the Andes" earns a nod from anyone in Quito. It converts almost nobody, because there is nothing in it to touch. "Keep the cattle off the bog above La Mica" lands, because the person reading it lives in the south, drinks from La Mica, and learned in July 2025 exactly which sponge that is.
That is the rule in your water is not water: name one living thing, one person who already cares, one next step. Santa Fe, the later cousin, found the same shape in a ditch and its parciantes. In Quito the living thing is a páramo — Antisana's grass, Pugllohuma's peat, Paluguillo's corridor — and the person is the guardapáramo already on it. The next step is to put money where they are.
For a foundation, that is not a new idea. The Nature Conservancy co-founded the fund in 2000 and, sixteen years later, gave a whole hillside. Fundación Cóndor Andino runs the camera traps; WCS Ecuador counted the condors; Fundación Oso Andino follows the bears and mountain tapirs on the Papallacta side. What a foundation can add is more of the same thing, for longer: guardapáramo salaries, drain-blocking and fence lines on a named hillside, year after year, through the fund that already does the work. That is the specific gift. Not "conservation in Ecuador." This grass.
For a land steward — a land trust or a conservation-area manager — the lesson is to name the ground you hold in the same breath as the intake it fills. In Quito that pairing is already on the map: Antisana's páramo, La Mica, the south.
If you live here, you are already in. Your water bill has funded this grass since 2000. If you want to see who walks it, start with FONAG.
our own stage, plainly
If you want to fund this grass today, the door already exists: FONAG takes company and foundation money now, and that is the first place to send it. What ensurance could add later — only if FONAG wanted it — is a certificate for one named piece of this páramo: a standing public record that lets many smaller payors fund the same hillside continuously, with every transfer visible, all of it routed to FONAG's existing work. It would carry no title to the grass and make no claim about what the grass is worth. There is no Quito certificate today. The live parent is northern-andean-paramo.ecoregion. If you want that second pipe to exist, say so.
frequently asked questions
what is a quito páramo?
A Quito páramo is the wet, high Andean grassland above the treeline on Antisana, Cayambe-Coca, Pichincha–Atacazo, and the Pita headwaters. Tussock grass and cushion wetlands over deep black soil catch rain and fog and release them slowly into the rivers and reservoirs the city drinks from. EPMAPS attributes about 85% of Quito's water to páramo; FONAG says closer to 90%.
why does quito depend on páramo?
Because the páramo is the reservoir before the reservoirs. It holds water between rains and lets it out steadily into the Pita, the La Mica intake, the Papallacta reservoirs, and the western conduits. Grazed, burned, or drained, the same rain arrives faster, dirtier, and thinner in the dry season. On Antisana, the páramo's slow release matters more as the glacier shrinks; it cannot replace the ice, but it evens out what is left.
is a páramo a wetland?
Partly. A páramo is mostly grassland, but much of its water-holding power comes from the cushion wetlands and peat bogs inside it — FONAG's drain-blocking at Pugllohuma is wetland restoration inside a grassland. In the stocks-and-flows framework it reads as grasslands plus inland wetlands, producing water abundance, clean water, and risk resilience.
next steps
Four named sponges, each with grass, cushion wetlands, a mountain, and people already walking it. That is the thing to name. Not water. Antisana's páramo. Paluguillo's corridor. The bog above La Mica.
read the rule behind the ask — your water is not water →
see the live agent for the páramo Quito drinks from →