- Taxon
- Gallery
- ≡ Hebe stenophylla (Steudel) Bayly & Garn.-Jones in Bayly et al., New Zealand J. Bot. 38: 173 (2000) var. stenophylla
- = Veronica parviflora var. angustifolia Hook.f., Bot. Mag. 98, t. 5965 (1872)
- ≡ Hebe parviflora var. angustifolia (Hook.f.) L.B.Moore in Allan, Fl. New Zealand 1, 912 (1961)
- = Veronica angustifolia var. abbreviata Petrie, Trans. & Proc. New Zealand Inst. 53: 371 (1921)
Stem pubescence glabrous or bifarious to uniform. Lamina linear to narrow-lanceolate or narrowly elliptic, 19–87 mm long, 2.5–9.5 mm wide, dull above; stomata sparse to dense; minute pits abundant, or confined to near margins; margins usually glabrous or sometimes minutely hairy towards apex. Inflorescence 26–95 mm long; pedicels glabrous. Corolla tube 3.0–4.9 mm long, glabrous within.
North Island: Auckland (a few sites near Hamilton, e.g., Narrows Bridge, Waikato River), Gisborne (a few scattered sites in the south), Taranaki (near Whanganui and in the Ruahine Range only), southern North Island (Hawke’s Bay, Kaweka Range, Kaimanawa Mountains, and Ruahine Range, Manawatu, Wairarapa coast.
South Island: Western Nelson, Sounds Nelson, Marlborough, Westland and Marlborough (north of a line from Cape Farewell to Cape Campbell).
A collection labelled Dillon River (Martin, WELT SP082014, not mapped here) might be from south of this range, or it could be from Dillon Creek, close to Blenheim.
Bluffs, terraces, hillsides, open rocky sites, stream banks, gorges, and roadsides. Recorded elevations range from 1 to 1280 m.
Flowers: December–April (occasionally to September); fruits: January–July, persisting all year.
2n = 40 (see Bayly & Kellow 2006, as Hebe stenophylla var. stenophylla).
Veronica stenophylla var. stenophylla includes a range of populations that differ morphologically in several characters, particularly habit, leaf shape and size, and distribution of leaf stomata. North Island plants on mudstone usually have lower stature, often narrower leaves and more abundant leaf stomata than plants on greywacke and other rocks. For details, see Bayly & Kellow (2006).