The Unions des Maisons de Champagne (UMC) divides its Montaigne de Reims subregion into four subzones:
- Grande Montagne Reims
- Massif de St. Thiery
- Monts de Berru
- Reims: Vesle & Ardre
Modification of a map secured from cambridgewineblogger .blogspot.com |
In his graphical representation of Montagne de Reims, Liem divides the villages into two buckets: West and North (to include all the villages located outside of the Grande Montagne subzone); and Grande Montagne. In his description of the wines and terroir, however, he does distinguish between Grande and Petite Montagne. Liem does not spill any ink on the villages falling into the maisons-champagnes.com Monts de Berru and Vesle & Ardre (beyond Petite Montagne) subzones.
Montagne de Reims is more of a wide plateau than a mountain as its horseshoe shape -- open to the west -- is only 293 m (940 feet) at its highest point. The plateau is mostly covered with thick forests with vineyards occupying the flanks and, depending on their position on the horseshoe, having exposures ranging between northwest and south. Grande Montagne occupies the northern, eastern, and southern slopes of the horseshoe while Petite Montagne, a lower slope, occupies a northwesterly offshoot.
Grand Cru sites are located on south and north exposures while Premier Cru sites can be found at all exposures. The Grand Cru sites are pictured on the map below and described in detail in the table following.
Source: wineroutesfrance.com |
Table 1. The Grand Crus of Grande Montagne.
Village
|
Description
|
Soil
|
Lieux-dits
|
Tours-sur-Marne
|
-
Most southerly of the Grande Montagne Villages
-
On north bank of the Marne
-
Newcomer (1955) to grapegrowing
-
Terroir produces combination of mountain (more
rigidly structured) and river wines
|
||
Bouzy
|
-
Ranks among the greatest terroirs of Champagne
-
Among warmest terroirs of this subzone
-
True mountain wine
|
-
Bedrock of hard chalk
-
Some parts of topsoil at 50 cm
-
A 3-m-deep layer of sedimentary soil runs
through center of village – ideal for Pinot Noir
|
|
Ambonnay
|
-
Among greatest terroirs of Champagne
-
Portion of vineyard faces SE (Tempers
ripeness, resulting in wines more delicate than Bouzy)
-
Three rolling hills provides wider variety of
sun exposure than experienced in Bouzy
|
-
Chalky terroir
-
Soil poor near Bouzy
-
Deeper alluvial soil at the base of the slope
in the eastern portion
-
Thinner closer to Trépail
-
More calcareous soil exposed in SE vineyards
9ideal for Chardonnay)
-
Deep topsoils below the village
|
-
Les Crayères – chalky vineyard on
east side of village
-
Les Bermonds
-
La Grande Ruelle
-
Le Bout de Clos
-
Le Parc – thick layers of tufa above the chalk
-
Clos d’Ambonnay – notably calcareous soils
(structure, complexity, salinity)
|
Verzennay
|
-
418 ha (1033 acres)
-
Pinot Noir darker than in south-facing
villages (distinctive gaminess and metallic, iron-like undertone
|
-
Well-drained soils
-
Some clay-heavy parcels, some chalk-heavy
parcels
-
Clay seems deeper
|
|
Sillery
|
-
Located on the flatter land below the slope
(other side of A4)
-
92 ha (227 acres)
-
Mild, NE-facing slopes in southern part of
village
|
-
La Loge
-
Les Blauer Germains
-
Les Champs de Romont (southern part of
village)
|
|
Mailly-Champagne
|
-
Westernmost Grand Cru in northern Montagne de
Reims
-
Classified Grand Cru in 1920
-
70 ha (123 acres)
-
Strong, 80-member Coop operates herein
-
35 lieux-dits
-
400 parcels of Pinot Noir (89%) and Chardonnay
-
Pinot Noir not as powerful and vinous as is
the case for south-facing slopes
-
Among the last subzones in Champagne to be
harvested (difficulty ripening)
|
Varied terroir with chalk subsoil
|
-
Les Baraqumes – cooler site producing
structured, spicy PN
-
Les Godats and Les Coutures – further downm
the slope; fatter and warmer
-
Les Cotes – Southern side of the chalky ridge
so more exposure than the preceding
|
The Premier Cru vineyards and the remaining subzones of the Montagne de Reims will, in a subsequent post, round out the discussion of the region.
©Wine -- Mise en abyme
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