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Lieu-dit · Pommard

Le Bas des Rouards

Le Bas des Rouards is a lieu-dit in Pommard, Côte de Beaune, Burgundy, whose largest tier is regional.

18.8 ha

delimited

308 m

elevation

10.0 h

sun at harvest

Open on the mapWith the boundary, the plots, the sun through the year and the bedrock.

In figures

LevelRegionalinao-aoc-viticoles-bulk (c. 4 September 2026)
VillagePommard
RegionCôte de Beaune, Burgundy
Delimited18.8 hainao-aoc-viticoles-bulk (c. 4 September 2026) · cadastre-etalab (4 September 2026)
Planted5.23 hacadastre-etalab (4 September 2026) · ign-bdtopo-vigne (5 September 2026) · ign-rpg-2024 (5 September 2026)
Parcels172
Grape varietypinot noir / chardonnay also permitted: pinot blanc, pinot grisinao-cahiers-des-charges (7 September 2026) · dgddi-superficies-produits (7 September 2026) · franceagrimer-observatoire-viticulture (7 September 2026)
Organic5%agence-bio-cartobio (c. 5 September 2026) · agence-bio-operateurs (5 September 2026)

Place in the village

Among the 31 named plots ranked regional in Pommard, from high to low:

sun at harvest 29
elevation 10
slope 5
on the slope 21

Position

308 m

elevation

17.2%

steep

W

west

mid-slope

concave fold

Elevation308 m 282 to 328 mign-rge-alti (5 September 2026)
Daytime temperature−0.30 °C by day, relative to the village centre at 266 m, ± 0.05 °Cmeteo-france-quotidiennes (6 September 2026) · meteo-france-postes (6 September 2026) · meteo-france-lsh (6 September 2026) · ign-rge-alti (5 September 2026)
Slope17.2% 9.8°ign-rge-alti (5 September 2026)
Aspectwest 275°ign-rge-alti (5 September 2026)
On the slope29% mid slope, in a concave hollow, 453 m drains onto itign-rge-alti (5 September 2026)

Bedrock

youngold
  • 11%Modern alluvium of the rivers 0.012–⁠0 million years
  • 39%Colluvium, mixed slope deposit about 0.1–⁠0 million years
  • 50%Argovien marl and marly limestone 159.5–⁠157.5 million years

Not a borehole: ordered by age, thickness by share of surface.

In the glass. In practice it is mainly associated with white wine: broader and fuller than on hard limestone, and often described as slower to open up, although that depends at least as much on yield and vinification. The link runs through soil depth and water supply, not directly from rock to taste.

White marls and marly limestones from the Middle Oxfordian, referred to in the older French literature and on the geological map as faciès argovien. They were laid down on a quiet, relatively deep carbonate seabed where lime mud mixed with clay carried in from the land, roughly 159.5 to 157.5 million years ago. In the ground they are pale, crumbly layers that stick in rain and break up into flakes in drought, alternating with thin, harder limestone beds.

For the vine. Marl holds water, and that is the key property here: in a dry summer there is reserve in the subsoil and the roots can penetrate to considerable depth as long as the layer is not compacted. The downside is that the ground stays cold and heavy in spring and is hard to work after rain, so these marls almost always need slope and good drainage to perform as vineyard soil. The active lime content is high, so chlorosis is a real risk and the choice of rootstock matters.

Characteristic of the slopes around Chagny, Rully and Bouzeron, and of the upper slopes of the Corton hill where Corton-Charlemagne stands.

BRGM geological map at 1:50,000. It tells vineyards apart, not plots within a vineyard. The link between rock and taste is indirect: soil depth, water and warmth do the work, and slope, vine age and the cellar do the rest. Units on that map: j5b, C, Fz.

brgm-bdcharm50 (c. 4 September 2026)

Sun and horizon

09:09

above the hill

19:08

behind the hill

10.0 h

sun at harvest

1.3 h

lost to the hill

Grey: sun up, but behind the hill or the vineyard's own slope.

Around harvest the sun rises here at 09:09 above the hill and disappears at 19:08 behind the hill: 10.0 hours of direct sun on a clear day. The ridge reaches 17.3° above the horizon to the east. The relief costs 1.0% of the irradiation from April to October, direct and diffuse together.

Irradiation−2.4% versus flat land 1,013 kWh/m² from April to October, 43% of it diffuseunder the average cloudiness of 2005 to 2023 (PVGIS-SARAH3, EU JRC); direct, diffuse and reflected light togetherign-rge-alti (5 September 2026) · ign-lidarhd-mnh (6 September 2026) · ign-bdforet-v2 (5 September 2026) · jrc-pvgis-sarah3 (10 September 2026)
Open sky97.2% of the sky the slope itself sees; the surrounding relief blocks the restign-rge-alti (5 September 2026) · ign-lidarhd-mnh (6 September 2026) · ign-bdforet-v2 (5 September 2026)
Three reference days and the caveat
risesetsunday
21 June07:4220:4813.1 h15.9 h
20 September09:0919:0810.0 h12.3 h
21 December10:2116:165.9 h8.5 h

Computed from the IGN elevation model at 5 m: horizon in 36 directions up to six kilometres, sun position per minute, angle of incidence on the mean slope. Clear sky, with the tree canopy from the IGN forest inventory as a raised horizon (15 m closed forest, 5 m heath, trees within 60 m ignored), 35% of the far field is forest (BD Forêt), no buildings.

The irradiation loss does include clouds: the average of 2005 to 2023 (PVGIS-SARAH3, EU JRC), not any particular year.

ign-rge-alti (5 September 2026) · ign-lidarhd-mnh (6 September 2026) · ign-bdforet-v2 (5 September 2026)

Air and cold

26 m

above the lowest point

drains far away

cold air

a main drain

242.9 ha flows past

Cold air26 m high on the slope, cold air drains far awayign-rge-alti (5 September 2026)
Cold air passing through242.9 ha a main drain, mean over the polygon 3.68 haign-rge-alti (5 September 2026)

Planting

E-W

down the slope

1.01 m

between the rows

85%

vineyard in 1950

RowsE-W (92°) down the slope (3°), every 1.01 m, varies by plotmeasured over 3.7 of 5.2 ha plantedign-bdortho (5 September 2026)
Vineyard in 195085% abandoned since: 7.09 haassessed over 13.0 ha on the 1950-1965 aerial photographign-photos-historiques-1950-1965 (6 September 2026)

Climate over time

196019802000202012°14°16°

station LA ROCHEPOT, 417 m, 11.2 km away

growing season, April to October: 1951-1980: 14.1 °C, 1991-2020: 15.2 °C

Huglin index: 1951-1980: 1,528, 1991-2020: 1,726

last spring frost: 1951-1980: day 115, 1991-2020: day 108

raw daily series, not corrected for station breaks

The name

bas
low, the lower part of a named plot. Shape and position · Terroirium, Eigen telling over de namen in deze atlas (2026)

This is about the words, not about this plot: the same name can have arisen differently elsewhere.

Who owns land here

4.50 ha of 18.8 ha delimited is registered to a legal entity

  • GFA GOUTARD JOILLOT8%
  • COMMUNE DE POMMARD3%
  • DOMAINE DU CHANCELIER3%
  • SCEA DU DOMAINE GUY ET YVAN DUFOULEUR3%
  • JULEMOTI2%
  • 6 other legal entities6%
  • private individuals or unknown76%

Private individuals or unknown: 14.3 ha.

Share of the delimited hectares. Only legal entities are public in France; everything else stays unnamed. From the public register of legal entities (DGFiP), as of 1 January 2025. The owner is not always the one who works the vineyard: tenancy is common.

Nearby lieux-dits

In the same village, measured between label points. That does not say which ones border each other; the map shows that.

Where each figure comes from

Classification
The INAO delimitation per denomination, cut against the cadastral parcel. Only the INAO's own plans are legally binding; this map is informational.
Area
Computed on the sphere from longitude and latitude (turf.area), not in Lambert-93. For an appellation this is the union of the INAO polygons across commune boundaries, measured on the unclosed geometry; the fifteen metres used to close the outline for the map are not counted. For a climat it is the union of the cadastral lieu-dit polygons with that name.
Planted
Parcel area times vineyard cover, where cover comes from the IGN vegetation layer supplemented by the agricultural declaration. Checked against the customs harvest declarations: median deviation 5.1 per cent over a hundred appellations.
Elevation
Mean of the elevation-model cells whose centre falls inside the polygon, on a 5 m grid.
Slope
Per-cell slope from the elevation model using Horn's method, then averaged over the cells in the polygon.
Aspect
Vector mean of the per-cell aspect. A plain average would turn north-east and north-west into south.
Sun at harvest
Hours of direct sun on 20 September under a clear sky, with the horizon in 36 directions out to six kilometres and the height of woods and buildings on top of it. Canopy height is measured where LiDAR HD covers the area and estimated from BD Forêt where it does not; the panel states which of the two was used.
Grape variety by appellation
Per appellation and colour the permitted varieties from the approved cahier des charges; per appellation and tier the declared hectares of white and red from the customs harvest declaration (product codes). One colour permitted: the main variety of that colour. Two colours: from 85 percent of the hectares that colour applies, in between it is called mixed. Champagne: the dominant variety from the planted hectares per variety per commune from FranceAgriMer. Per polygon the dominant variety of its parts by area. Derived, not measured: the variety per plot exists only in the customs vineyard register, which is not public. In a two-colour appellation a single plot may carry the other variety. Customs withhold small appellations (statistical secrecy), in which case the split is missing.
Bedrock
The geological unit covering the largest share of the polygon, from the 1:50,000 geological map. At 1:50,000 the map separates one climat from another, but not what varies inside a climat.
Organic
Share of the area certified organic or in conversion, from the CartoBio plot register.