We present magnetization measurements on oriented powder of ZnCu3(OH)6Cl2 along and perpendicular to the orienting field. We find a dramatic difference in the magnetization between the two directions. It is biggest at low measurement fields H or high temperatures. We show that the difference at high temperatures must emerge from Ising-like exchange anisotropy. This allows us to explain muon spin rotation data at T → 0 in terms of an exotic ferromagnetic ground state. PACS numbers: 75.50.Lk, 75.10.Nr The synthesis of the herbertsmithite [ZnCu 3 (OH) 6 Cl 2 ] [1] has led to a renewed interest in the frustrated spin-1/2 Heisenberg model on the kagomé lattice. This system has a highly degenerate ground state [2] and any small perturbation to the Hamiltonian can severely affect the ground state manifold. The perturbations can be: exchange anisotropy [3], bond anisotropy [4, 5], transverse field [6, 7], Dzyaloshinksy-Moriya Interaction (DMI) [8,9,10], or longer range interactions [11]. Therefore, numerous theoretical directions have been taken to predict the low-temperature behavior of the kagomé system, and some of them were particularly applied to magnetization and other measurements of the herbertsmithite [10] [12].